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In this paper, we propose a novel Total Electron Content (TEC) map prediction model, named ED‐AttConvLSTM, using a Convolutional Long Short‐Term Memory (ConvLSTM) network and attention mechanism based on encoder‐decoder structure. The inclusion of the attention mechanism enhances the efficient utilization of spatiotemporal features extracted by the ConvLSTM, emphasizing the significance of crucial spatiotemporal features in the prediction process and, as a result, leading to an enhancement in predictive performance. We conducted experiments in East Asia (10°N–45°N, 90°E−130°E). The ED‐AttConvLSTM was trained and evaluated using the International GNSS Service TEC maps over a period of six years from 2013 to 2015 (high solar activity years) and 2017 to 2019 (low solar activity years). We compared our ED‐AttConvLSTM with IRI‐2016, COPG, LSTM, GRU, ED‐ConvLSTM and ED‐ConvGRU. The results indicate that our model surpasses the comparison models in forecasting both high and low solar activity years, across most months and UT moments in a day. Moreover, our model exhibits notably superior prediction performance during the most severe phases of a magnetic storm when compared to the comparison models. Subsequently, we then also discuss how the prediction performance of our model is affected by latitude. Finally, we discuss the diminishing performance of our model in multi‐day predictions, demonstrating that its reliability for forecasts ranging from one to 4 days in advance. Beyond the fifth day, there is a pronounced decline in the model's performance. Plain Language Summary: High precision prediction of Total Electron Content (TEC) is of great significance for improving the accuracy of global satellite navigation systems. In this paper, we introduced the attention mechanism into the ionospheric TEC map prediction model to adaptively weight the ionospheric TEC spatiotemporal features, highlighting the contribution of important spatiotemporal features in TEC map prediction. Results showed that the prediction performance of our model is improved compared with the other six models. Key Points: Introducing ED‐AttConvLSTM, a novel Total Electron Content (TEC) map prediction model utilizing Convolutional Long Short‐Term Memory and an attention mechanism in an encoder‐decoder frameworkThe incorporation of attention mechanisms markedly decreased root mean square error in TEC map predictions for 2015 and 2019Our model excels over 6 state‐of‐the‐art models, affirming its robustness and reliability for TEC map prediction [ABSTRACT FROM AUTHOR]

The sporadic E‐layer (Es) exhibits unique opportunity for exploring the coupling from lower to upper atmosphere. It was found that the East Asia is with the highest intensity and occurrence probability of Es. By using the long‐term data of 21 ionosonde stations in China and Japan over the past 60 yrs, this paper explores the probable control on the Es layer from the lower layers. It is found that the intensity of the Es layer is strongly correlated with the surface atmospheric temperature, terrain, and land‐sea boundary. The correlation coefficient of the intensity of Es with surface temperature is as high as 0.8204, while that with the terrain and land‐sea boundary is up to 0.6668. Based on the coupling between the lower and upper atmosphere, this paper reveals the probable controls from lower layers on the intensity of the Es in East Asia. Plain Language Summary: As an occasional ionized layer of the ionosphere, the sporadic E‐layer (Es) exhibits unique opportunity for exploring the coupling from lower to upper atmosphere. Despite extensive research on both behavior and mechanism of the Es, none have adequately explained the strong inhomogeneous of its global morphology. It is found in fact that the East Asia is with the highest intensity and occurrence probability of Es. By using the long‐term data of 21 ionosondes in China and Japan over the past 60 yrs, this letter explores the formation mechanism of the strongest Es regions in the world. It is found that the intensity of the Es layer is strongly correlated with the surface atmospheric temperature, terrain, and land‐sea boundary. The correlation coefficient between the intensity of Es and surface temperature is highest, while that with the terrain and land‐sea boundary is also high. By analyzing the data as long as six decades, this letter reveals the probable controls from lower layers on the intensity of the Es in East Asia. Key Points: By analyzing the six‐decade data of 21 ionosondes in East Asia, it reveals probable controls on the strongest Es layer from lower layersFor the first time, it is found that the intensity of Es layer is highly correlated with the surface atmospheric temperatureAn interesting coupling from lower to upper atmosphere may be found by taking advantage of observations longer than half of a century [ABSTRACT FROM AUTHOR]

The globally expanding doctoral education and the diminishing availability of academic job opportunities have prompted an increasing proportion of PhD graduates to seek employment beyond academia, drawing a growing scholarly interest. However, the existing literature on doctoral career pathways tends to be fragmented and dispersed, given the idiosyncratic individual and educational characteristics of doctorates grappling with the complex structural factors. To depict a comprehensive picture of the diversifying employment trajectories of doctorates across various geographical, disciplinary and sectoral contexts, this study conducts a systematic review, scouring 831 pertinent journal articles from the Web of Science. Following a set of inclusion criteria, 31 papers were ultimately selected to identify the key factors shaping employment trajectories of PhD graduates at structural (national supply and demand), institutional (employers' perceptions) and individual (doctorates' characteristics) levels. Drawing on the boundaryless and value‐based career theories, the authors develop a four‐dimension analytical framework, within which the findings of the 31 papers in East Asian and Western contexts are analysed. Overall, stakeholders in Western systems generally recognise the trend of PhD graduates securing non‐academic employment, whereas East Asian nations appear less receptive to this agenda. Meanwhile, due to their strong emphasis on research skills utilisation and employment stability, PhD graduates in certain economies find it challenging to pursue satisfying and successful careers, warranting increased attention. Building on the findings, we propose a four‐quadrat model in an effort to provide a tool for evaluating the capacity to absorb doctoral workforces of specific systems by categorising the doctoral professions. Highlighting shared patterns observed across various higher education systems and distinct trends prevalent in specific economies, this paper addresses key topics in doctoral education and doctorate employment literature such as labour market conditions, employment outcomes, job satisfaction, skills (mis)matches and sustainable careers. [ABSTRACT FROM AUTHOR]

Supply chain decoupling in the US–China confrontation has generated serious uncertainties for private businesses. This paper focuses on machinery international production networks in East Asia and tries to find quantitative evidence on supply chain decoupling by using international trade statistics, particularly from the viewpoint of middle powers such as Japan. While data on the sectoral level of trade do not show any clear evidence of supply chain decoupling, some specific US export controls indeed affect international transactions when examined at a finely disaggregated level. We econometrically measure the effect of some of the US policies on Japanese exports to China. The recent strengthening of US export controls related to supercomputers and advanced integrated circuits is likely to generate further effects. Nevertheless, the supply chain decoupling seems to end up as a partial one, and a large portion of International Production Networks (IPNs) may remain active. In conclusion, the paper briefly discusses the policy implications of the analysis. [ABSTRACT FROM AUTHOR]

Most Asian countries are regarded as Confucian countries although each has its own historical and cultural background. Little is known about how people in different Asian countries perceive their family boundaries. This study is an attempt to compare the perception of the family in China, Japan, and Korea. We examined the family perception and found substantial differences among the three. Chinese people showed the widest and paternally extended perception of family. Data from people in Korea nearly matched data from China, but family perception developed bilaterally. People in Japan, however, perceived only blood‐tied, intimate relations as family members. In addition, the perception of the family was not substantially different between the genders in Japan and China, but in South Korea, men perceived family boundaries more widely than women, implying that women have a greater family burden than men in Korea. Considering the heterogeneity in family perceptions in these countries, this paper tries to explain how social institutions interact with individuals and impact the perception of family. Finally, this paper concludes that it is inappropriate to tie the three East Asian countries as 'Confucian civilizations' in terms of family perception. [ABSTRACT FROM AUTHOR]

Background: Our bodies are a collection of nutrients. For healthy body production and activities, good nutrients must be balanced and supplied steadily. However, as modern people eat more irregular meals and fast food, they are running out of nutrients needed by the human body. As a result, research was conducted on the effect of eggs with good cost‐effectiveness on the human body and hair. Purpose: The purpose of this paper is to review the literature investigated to convey knowledge of the positive nutrients of modern people's nutrition and eggs. Methods: These data were reviewed to identify agreement between each section and the unique guiding area. Regarding the survey criteria, it was finally decided that 31 papers were suitable for evaluating the purpose of research as follows. PRISMA flowcharts allow you to determine the number of records identified, included, and excluded. Results: Eggs are considered the most cost‐effective foods that deliver protein, biotin, choline, and vitamin A to the world, and eggs that can be easily consumed are known as nutritional foods because they contain protein, lipids, minerals, and embryonic development growth factors. It is widely consumed as a food that can be eaten by anyone, including the elderly and children. Conclusions: In this study, eggs can be used as important data for modern people by delivering nutrients to the human body and hair of modern people and understanding positive nutrients. [ABSTRACT FROM AUTHOR]

Societal Impact Statement Summary The discovery of a new genus within the family Thismiaceae, known as fairy lanterns, marks a significant scientific milestone in Japan, a country renowned for its botanical research. The unearthing of a new genus, especially in a well‐documented flora like Japan, is both rare and monumental. Unlike other fairy lanterns that bloom under leaf litter and can be easily overlooked, the new genus and species, Relictithismia kimotsukiensis, often does not even emerge above the surface of the soil when flowering. This captivating characteristic not only enriches our knowledge of botanical diversity but also emphasizes the importance of preserving natural habitats that harbor such rare species.The family Thismiaceae, known as “fairy lanterns”, is distinguished by its urn‐ or bell‐shaped, glasswork‐like flowers with basally fused tepals and its dependence on specific fungi for carbon. A new genus and species, Relictithismia kimotsukiensis, has been discovered in southern Japan. This species is notable for its unique anther‐stigma contact, hitherto unreported in the other Thismiaceae. Unlike typical fairy lanterns that bloom just above the leaf litter, Relictithismia often flowers beneath it. The underground habit is potentially associated with self‐pollination. The discovery of Relictithismia enhances our understanding of evolutionary pathways within the Thismiaceae, as it possesses characteristics previously thought to be unique to Thismia (the annulus with drooping stamens) as well as traits found in other genera (free stamens without expanded connectives). This paper reviews the morphology, ecology, and evolutionary history of Relictithismia, offering insights into the peculiarities of these enigmatic plants. [ABSTRACT FROM AUTHOR]

A strong cooling event refers to a sharp change in the average temperature over a short period. The rapid change of temperature has important effect on human health and is highly concerned recent years. Based on the observed temperature data set from stations in Southwest China (SWC) from 1979 to 2017, this paper analyses the characteristics of the strong cooling event (SCE). The result shows that SCE occurs with the highest frequency during the time from February to May. Among them, the frequency of SCE in February exhibits an abrupt change before and after 2005 with a significant increase. Further study reveals that the change of SCE frequency in February is associated with the large‐scale background circulation patterns. After 2005, there is a cyclonic circulation anomaly in Northeast Asia and an anticyclonic circulation anomaly in the Tibet Plateau (TP). This pattern provides a favourable condition for the southward movement of cold air mass, thereby increasing the frequency of SCE in SWC. Furthermore, it is revealed that there is a strong correlation between the variation of SCE frequency in February and sea surface temperatures (SST) in the Northwest Pacific in January before 2005. The cold SST anomaly could favour the occurrence of extreme TD events in SWC through vertical circulation. After 2005, the correlation between SCE and Northwest Pacific SST is not significant. The sea ice in the northern Barents Sea and Kara Sea becomes the dominant impact factor. The abnormally low sea ice concentration is conducive to strengthen the meridional circulation over East Asia, leading to an increasing frequency of SCE in SWC. [ABSTRACT FROM AUTHOR]

This paper aims to contribute to global social theory by contextualizing modernity/coloniality in East Asia. It begins with a reconstruction and evaluation of three sociological accounts of East Asian modernity, namely Kazuko Tsurumi's theory of endogenous development, Sun Liping's theory of communist civilization, and Chang Kyung Sup's theory of compressed modernity. Despite their insights, these theorists fail to transcend the Eurocentrism and methodological nationalism implicit in the paradigm of latecomer modernization. These problems can be better addressed by anti‐colonial perspectives, including Tani Barlow's colonial modernity, Chen Kuan‐Hsing's inter‐Asia, Xie Lizhong's post‐Western sociology, and Wang Mingming's civilizational anthropology. Yet European hegemony continues to define the spatiotemporal frame of these perspectives. To overcome the lingering problem of Eurocentrism, Laura Doyle's notion of inter‐imperiality is employed to highlight the power‐laden interaction and interdependence among imperial powers in the global and regional history of East Asia. This alternative approach, I argue, can shed new light on East Asian modernity and delineate its dialectical formation. [ABSTRACT FROM AUTHOR]

A new incoherent scatter radar (ISR) has recently been dedicated at Sanya (SYISR), China (geographic 18.34°N and 109.62°E) to detect the low‐latitude ionospheric plasma by conducting continuous operation and electronic beam steering on a pulse‐to‐pulse basis. This paper provides an overview of the processing procedure of SYISR ion line data and presents some preliminary observational results under various transmitting signal schemes and different working modes, such as the zenith‐directed mode and meridional and zonal scanning modes, with comparison to the international reference ionosphere model (IRI‐2016), ionosonde and Ionospheric Connections Explorer (ICON) satellite measurements. The diurnal and altitude versus latitude variation characteristics of electron density (Ne), electron temperature (Te), and ion temperature (Ti) are in accordance with those of other ISR measurements in mid‐low latitudes, and IRI shows some discrepancies with SYISR observations, including the sunrise and sunset enhancement in SYISR_Ti and the overestimated IRI_Te. The comparison between the daytime SYISR_Ti and ICON_Ti shows good consistency based on 31 observational samples. The measurement of line‐of‐sight velocity (Vi) for long pulse can reveal the properties of the medium scale traveling ionospheric disturbances manifesting the radar's potential to study the mesoscale ionospheric variation in the Sanya area. The derived vector velocities with a better measurement accuracy during the day are generally in line with ionospheric plasma physics. The results show that SYISR can obtain continuous ionospheric parameters through multi‐beam scanning measurements at ∼700 km horizontal scale, which provides important information for studying the atmosphere‐ionosphere‐magnetosphere coupling and ionospheric scintillation at low latitudes in East Asia. Plain Language Summary: China's first phased‐array incoherent scatter radar was completed in 2021 in Sanya, which is called SYISR. SYISR aims to investigate fundamental scientific problems in the ionosphere, including atmosphere‐ionosphere‐magnetosphere coupling, regional ionospheric properties and ionospheric irregularities in southern China. SYISR can directly measure electron density, electron and ion temperature, and drift velocity of the ionospheric plasma and can be used to indirectly obtain the temperature of the neutral atmosphere, wind field and irregularity information. This paper describes in detail the data processing from the IQ signal to the derived ionospheric parameters for SYISR. Ionospheric experiments in various scanning modes have been performed, mainly including a single beam in zenith‐directed mode and multiple beams in meridian and zonal scanning modes, and the obtained results are evaluated. These experimental results are evaluated through comparison with the IRI‐2016 model, digital ionosonde and Ionospheric Connections Explorer satellite. The comparison results indicate that SYISR is able to provide reliable, unique, and important ionospheric information for the study of ionospheric science at low latitudes in East Asia. Key Points: Sanya incoherent scatter radar (SYISR) is a new phased array system dedicated to the ionospheric observations at low latitudes in Asia sectorSYISR is operational, providing high‐quality ionospheric measurements in multiple radar scanning modes and radio pulse schemes modesData processing procedures and initial ion‐line results using typical experiment modes are reported [ABSTRACT FROM AUTHOR]

Measuring the plasma motion vector field accurately is beneficial to understanding the physical processes in the ionosphere. As a newly built advanced modular phase array Incoherent Scatter Radar in Sanya (SYISR), SYISR can measure the line‐of‐sight (LOS) velocity of ion drift in multiple directions, potentially yielding the spatial distribution of ionospheric plasma drift at low latitudes in East Asia. Compared to the traditional ISR, it can operate continuously for a long‐time and perform with fast and flexible scanning. This paper evaluates different beam configurations and inversion methods for vector ion velocity detection by comparing the vector ion velocities input in the forward modeling and derived by inversion. For the mono‐static SYISR, the all‐sky scan mode is suitable for observing the distribution of vector ion velocity with height, and the fine scan mode is suitable for observing the spatial distribution of two components of vector ion drift perpendicular to the magnetic field in the northern region of SYISR's non‐grating lobe. For the future tri‐static SYISR, it could simultaneously observe the spatial distribution of all three components of the vector ion velocity. Besides, the inversion method based on Bayesian estimation shows good accuracy and stability in deriving the vector ion velocity, especially when the LOS ion velocity has a large error. These results will benefit the design and optimization of the actual experiments for the vector ion velocity measurement and inversion using the SYISR system. Key Points: A procedure is constructed to guide and evaluate the detection of the vector ion velocity by the Incoherent Scatter Radar in Sanya (SYISR) systemThe ion velocity inversion method based on Bayesian estimation shows good accuracy and stability in deriving the vector ion velocityMono‐static and tri‐static SYISR can be used to detect the height profile of vector ion velocity and spatial distribution, respectively [ABSTRACT FROM AUTHOR]

Inspired by Japanese faith groups, organic food production has witnessed surprising growth in East Asian countries, such as Japan, Taiwan, and South Korea, over the past two decades. The rapid expansion of East Asian trans‐national organic food production networks is closely linked with religious practices and beliefs, such as ahimsa (non‐killing). The complexities of transnational organic production networks in East Asia cannot be adequately captured by the existing literature on "conventionalisation of organic agriculture," which repeatedly debates the extent to which capitalism intrudes on the social and biophysical dimensions of farming. I argue that this simplified and binary debate tends to treat the organic market as an unquestioned, stabilised, and universalised artefact. Less attention has been paid to questions such as, how do alternative food markets come into being, stabilise or get crushed? Inspired by the social studies of economisation and marketisation (SSEM) approach, this paper urges scholars to move beyond the conventionalisation debate and draws attention to the organic food market‐making practices. Taking inspiration from SSEM thinking, I propose that more emphasis needs to be placed on the performation struggles, which refers to the confrontations between different economic programmes and actors. By drawing attention to the organic market performation struggles in Japan and Taiwan, this paper argues that organic food market‐making is a global heterogeneous assemblage, in which all human and non‐human actants across multi‐scalar geographies, such as trans‐local religious/scientific knowledge, believers, and so on, can contribute to the making and remaking of markets. With reference to qualitative interviews with organic distributors and practitioners, this paper deepens the knowledge of the geographies of marketisation in a global‐relational context. The rapid expansion of East Asian transnational organic food production networks is closely linked with religious practices and beliefs, such as ahimsa (non‐killing). The complexities of transnational organic production networks in East Asia cannot be adequately captured by the existing literature on "conventionalisation of organic agriculture," which repeatedly debates the extent to which capitalism intrudes on the social and biophysical dimensions of farming. Inspired by the social studies of economisation and marketisation (SSEM) approach, this paper urges scholars to move beyond the conventionalisation debate and draws attention to the organic food market‐making practices. [ABSTRACT FROM AUTHOR]

Over the past one and a half centuries, urbanization has coincided with industrialization and globalization. The business as usual mode of urban development has proven unsustainable, and the consensus of developing new paradigms toward more sustainable trajectories has been reached. This paper reviews and identifies the most prominent forms of sustainable urban development, encompassing theories of urban frameworks, major definitions and concepts and historical developments in the East Asian context. Three major trends are assessed, including garden cities (and eco‐cities), low‐carbon cities and smart cities, which identify each main phase of sustainable urbanization in the East Asian context. [ABSTRACT FROM AUTHOR]

This paper analyzes the shift in career strategies among Japanese women due to the globalization of Japan's economy since the 1980s. It highlights how economic changes led to a gender‐based division of labor, propelling women to seek opportunities abroad. The research draws on interviews with 81 women who moved to financial centers in East Asia, mainly in Hong Kong and Shanghai, examining their experiences in the workforce, the impact of human resource agencies in their migration, and the challenges and opportunities they encountered. The study reveals a complex landscape where Japanese women navigate gendered expectations and discrimination both in Japan and abroad in pursuit of career advancement. The conclusion emphasizes three points. First, women found opportunities abroad to do what they wanted, even if it was not what they initially expected before leaving Japan. Second, although supportive and subordinate to male managers, their work was indispensable to the management of Japanese companies abroad. Their contribution has long been underestimated but needs to be considered. Third, the experience abroad gave them direct interaction with various clients and colleagues and a view of rapid societal change in Hong Kong and China, contributing to choosing their diverse career trajectories and life plans. [ABSTRACT FROM AUTHOR]

The South China Sea summer monsoon (SCSSM) onset and withdrawal have critical impacts on the climate of East Asia. However, using different reanalysis data may lead to the uncertainty of the SCSSM. This study uses reanalysis datasets including JRA‐55, ERA5, NCEP‐NCAR NCEP‐1 and NCEP‐DOE NCEP‐2 to calculate onset and withdrawal dates and index of SCSSM from 1991 to 2020, analyses the uncertainty and figures out the possible reasons. Results reveal that the four reanalysis datasets have obvious uncertainty in calculating the withdrawal date of SCSSM, with the deviation being up to 3.4 pentads. Further analysis shows that large differences in thermal conditions and lead to the uncertainties. From the perspective of precipitation, Greater uncertainty exists in the relationship between monsoon retreat and September–October precipitation, NCEP1 and NCEP2 datasets show weak correlation in southern China and Indonesia. Moreover, the uncertainty can be also found in the correlations of SCSSM with global sea surface temperature (SST) anomalies. JRA‐55 and ERA5 show a strong correlation of with SST in several areas, and exhibit a distinct Pacific decadal oscillation (PDO) mode with monsoon onset, while NCEP‐1 and NCEP‐2 have a weaker correlation with SST anomalies than JRA‐55 or ERA5. Comparing multiple factors comprehensively, this paper concludes that JRA‐55 may be more representative in the monsoon study, followed by ERA data. In short, depending on the specific research questions, researchers can choose appropriate data sources to study the SCSSM based on the different aspects and the uncertainty also deserve our special attention when selecting the reanalysis datasets. [ABSTRACT FROM AUTHOR]

Glazed tiles were prestigious building materials reserved for embellishing the roofs of royal architectures of ancient states in East Asia. This paper, by studying glazed tiles from the palace precincts of Shangjingcheng, Xigucheng, and Baliancheng, three capital cities of the Bohai state (698–926 ad), aims to expose the vibrant technological and economic interactions among ancient states of East Asia untold in historical chronicles. Although it is well recorded that Bohai maintained intimate political, cultural, and commercial engagements with the Tang empire and the Yamato state, it is obscure what kinds of technology and commodities were involved in these activities. It appears that the bodies of these tiles were produced of local iron‐rich clays, and the glazes were made of compounds of the same clays and lead materials. The glazing technique may have been transmitted from the Tang empire yet modified in response to local circumstances. Lead materials were acquired from various sources, partly from the one for the Huangye sancai wares in the Tang empire, and partly from the one for Nara sancai wares of the Yamato state in Japan. Archaeology is therefore capable of enriching our knowledge of the human past, even in the historical period. [ABSTRACT FROM AUTHOR]

The observed variations in intense geomagnetic flux lobes have a significant impact on regional geomagnetic fields, and produce unique geomagnetic characteristics. To investigate the time‐dependent effect of the Siberian flux lobe on the geomagnetic field in East Asia, we reconstructed a stacked full‐vector paleomagnetic secular variation record (since 2000 BCE) from three sediment cores collected in the Bohai Sea, China. Age models of the studied cores were established through a combination of radiocarbon 14C dating and inter‐profile correlation of mass‐normalized magnetic susceptibility. Rock magnetic results indicate that fine‐grained magnetite is the primary remanent carrier. We found that the paleomagnetic field records in the Bohai Sea correspond more closely with those from the middle latitudes, rather than the low latitudes. This was primarily attributed to the variation of the Siberian flux lobe. This study provides a better understanding of the contrasting patterns of regional geomagnetic fields in East Asia, and emphasizes the significant role played by the Siberian flux intensity lobe in shaping their formation. Plain Language Summary: The Earth's magnetic field is in a constant state of flux, both temporally and spatially, and plays a crucial role in protecting our planet from solar wind and cosmic rays. The long‐term variation of the Earth's magnetic field is closely linked with the magnetic flux patch situated at the core‐mantle boundary. However, our understanding of the evolution of magnetic flux patches has been limited by the use of short‐term instrumental data and discrete archeomagnetic data. In this paper, we reconstruct a ∼4,000‐year high‐resolution full‐vector paleomagnetic record from sediments in the Bohai Sea, China. Our findings reveal a clear contrast in the paleomagnetic variations between the middle and low latitudes of East Asia. We proposed that the Siberian flux intensity lobe likely played an important role in the observed paleomagnetic behavior discrepancy between the low‐ and mid‐latitudes of East Asia. Key Points: A multi‐decadal resolution paleomagnetic record spanning approximately 4,000 years has been derived from sediments in the Bohai Sea, ChinaThe paleomagnetic behavior differs between middle and low latitudes across East Asia, indicating the variation of the Siberian flux lobeThe disparity in inclination between the Chinese and Levantine spikes implies that these spikes arise from separate magnetic flux patches [ABSTRACT FROM AUTHOR]

Declining levels of trust in the media in Western democracies have drawn the attention of political scientists, but much less attention has been paid to East Asia. This paper sets out to examine the logic behind media trust in three different types of regimes in East and Southeast Asia: countries with, partial, and no press freedom, respectively. Our findings show that while respondents' trust in government and support for socioideological control of the government have consistent and significant associations with their media trust across all 12 countries, Internet usage, online political participation, support for media censorship, and patriotic belief have different associations with the variable being studied as the degree of press freedom varies. The findings indicate that citizens are well aware of the role mass media plays in the political system and thus their trust in the media reflects the expectation‐perception gap of the government‐media relationship accordingly. [ABSTRACT FROM AUTHOR]

In this paper, the spatio-temporal variation characteristics of the daily maximum boundary layer height (BLH) and precipitation (Prec) from 1900 to 2010 are analysed by using ERA-20C reanalysis data with mathematical statistical methods. However, since time-scale variation of boundary layer processes is very short and precipitation is also a discontinuous variable, to further understand the influence of BLH on precipitation, appropriate individual cases need to be selected for more in-depth analysis. These three sub-regions are extreme arid (annual average Prec < 25mm), arid (25mm < annual average Prec <250mm), and semi-arid (250mm < annual average Prec < 500mm), as shown by the white contours in Figure 1. The white contours represent the average annual precipitation from 1900 to 2010, and the shaded colours represents the daily trend rates. gl 1 TableThe climate tendency rate and correlation coefficient (r) between the daily maximum boundary layer height and precipitation in the three sub-regions. [Extracted from the article]

We present the largest freely available EcoPlate dataset for Japan, comprising data collected from a network of 33 natural forest sites (77 plots) in regions of East Asia ranging from cool temperate to subtropical. EcoPlate is a 96‐well microplate that contains three repeated sets of 31 response wells with different sole carbon substrates. The utilization of each carbon substrate by the microbial community is quantified by the color density of the well during incubation. EcoPlate can provide a multifunctional index of a soil microbial community. Soil properties (water content, carbon [C] and nitrogen [N] contents, the C/N ratio, and pH) that are essential for interpreting the EcoPlate results were also measured. The network is part of the Forest and Grassland Survey of the Monitoring Sites 1000 Project established by the Ministry of the Environment. Using a standardized protocol, soil was sampled between September and December 2020. A preliminary principal component analysis was performed on the temporal integration of color density using 31 substrates. For the temporal integration, we calculated the cumulative amount of color development by integrating the color density development curve. PC1 contributed 55.6% and is thought to represent the magnitude of the overall absorbance of all substrates. The model of environmental factors including elevation and the model of soil properties, including water content and pH, were selected as the best‐fit models for variation in PC1. EcoPlate data enable the meta‐analysis of comparative studies among forest types and testing community ecology and ecosystem function hypotheses at broad spatial scales. The complete data set for this abstract published in the Data Paper section of the journal is available in electronic format in MetaCat in JaLTER at http://db.cger.nies.go.jp/JaLTER/metacat/metacat/ERDP‐2022‐01.1/jalter‐en. [ABSTRACT FROM AUTHOR]

The China‐France Oceanography Satellite (CFOSAT) launched in 2018 is equipped with the Chinese Scatterometer (CSCAT), which is designed to measure high‐precision sea surface wind fields in the global ocean. This study aims to validate the CFOSAT wind fields with moored buoy‐measured ground truth data from August 2019 to July 2021. The test area was chosen as the Taiwan Strait, which is an important navigation channel and rich fishery grounds in the East Asia. It is also a high wind speed area particularly during typhoons and cold air passages. Thus, the accurate wind forecasts are crucially needed to avoid capsizing and casualties. The validation results give the correlation coefficient (R2) of 0.92, the root mean square error (RMSE) of 1.75 m s−1, and the absolute deviation (AD) of 1.10 m s−1 for the wind speeds, and R2 of 0.96, the RMSE of 21.87°, and the AD of 1.17° for the wind directions. During cold air passages, the AD of wind speeds decreases to 1.03 m s−1, which is smaller than 1.17 m s−1 during typhoons. Using the CFOSAT wind as historical observation data for refining of forecast work was tested by model output statistics revised method. The test results show that the refined forecast results of wind fields are improved up to 4%–17%. Thus, the validation and test results obtained in this study indicate that updating satellite winds would have great contributions to refined forecasting of local sea surface winds. Plain Language Summary: The China‐France Oceanography Satellite (CFOSAT) is a China‐France joint mission launched in 2018, which aims to update satellite remote sensing technologies of the sea surface winds and waves. This paper reports the validation results of the CFOSAT winds with moored buoy measurements. The test area is chosen as the Taiwan Strait, which is an important navigation channel in the East Asia and a rich fishery ground. Total 467 satellite‐buoy spatiotemporal matching data pairs were collected during 8 typhoons and 8 cold air passage processes over the Taiwan Strait. Statistical calibration analyses give the correlation coefficients as high as 0.92 for the wind speeds and 0.96 for the wind directions, implying that the CFOSAT wind data are of high quality and satisfy the requirements for the operational applications. Furthermore, test results to use the CFOSAT winds for operational ocean forecasts in the Taiwan Strait and adjacent waters show that the accuracies of forecasting work are raised up to 4%–17% during the typhoon and cold air passage processes. Thus, the validation and test results provided by this study indicate that it is expectable that updating satellite winds would have great contributions to refined forecasting of local sea surface winds. Key Points: China‐France Oceanography Satellite (CFOSAT) scatterometer wind data are validated by buoy measurements deployed in the Taiwan StraitCalibration analyses of 467 spatiotemporal matching data pairs give correlation coefficients of 0.92 for wind speed and 0.96 for directionApplications of CFOSAT winds improve refined operational forecasts up to 4%–17% under the extreme weather conditions [ABSTRACT FROM AUTHOR]

The East Asian winter monsoon (EAWM) is one of the most important climate systems during boreal winter. It has a large meridional extent and provides a vital bridge between the mid‐to‐high latitudes and the tropics. This paper reviews the latest research on the climate variability of the EAWM, with particular emphasis on the associated processes of extratropical–tropical interaction. Some new results have been achieved in understanding the variation of the EAWM on interdecadal, interannual, and intraseasonal time scales, such as the interdecadal strengthening in the early 21st century, the unstable impact of El Niño–South Oscillation (ENSO) on the EAWM, and the intraseasonal strong cold events in East Asia. In addition, understanding of the extratropical–tropical interactions related to the EAWM has improved in several aspects, including the impacts of the EAWM on ENSO‐related climate effects, and the variation of regional Hadley circulation over the western Pacific and its climate impacts in the Asia–Australia region. Moreover, recent work has systematically evaluated the capacity of climate models to simulate the EAWM, including its climatology, interannual to interdecadal variations, and its relationship with ENSO. Finally, some scientific issues regarding our understanding of the EAWM are proposed for future investigation. [ABSTRACT FROM AUTHOR]

Various studies have highlighted the importance of ethnic differences. The consideration of ethnic differences in the field of individualized pharmacotherapy is imperative. Therefore, various organizations and networks across countries should aim to conduct multicountry and multiregional clinical trials (MRCTs). If there is solid evidence available to evaluate the existence of ethnic differences between the same regional areas, it will lead to an increase in the efficiency of drug development. The purpose of this paper was to compare the approval dosing regimen among four Asian countries (Korea, Japan, China, and Taiwan) and elucidate the readiness and current status of the implementation of the International Conference on Harmonization (ICH) E17 guidelines on MRCTs. Reducing unnecessary clinical trials via multinational clinical trials in East Asian countries is also suggested. The approved dosing regimens for some drugs in the four Asian countries were similar; however, some differences might be caused by differences in legislation, even though there were no ethnic differences. This indicates that there are several roles to be expected of the Asia Clinical Pharmacology study network for exploratory MRCTs, which would lead to the accumulation of evidence for MRCTs, ultimately accelerating the efficiency of drug development in East Asian countries. The exposure of the new treatment to the necessary patients through collaborative research coordination and simultaneous multinational subject recruitment would serve its role in providing East Asia with specific personalized medicine with a high treatment success rate. [ABSTRACT FROM AUTHOR]

Planktonic animals drifting or floating in the sea have small body sizes and weights from hundreds to thousands of milligrams, and are primarily the food for other zooplankton and macrofauna: fish, cephalopods, seabirds and marine mammals, and also the larval pool of many benthic invertebrates. This paper describes a unique dataset of zooplankton collected from 1984 to 2013 in the North Pacific (the Bering Sea, Sea of Okhotsk, Sea of Japan and adjacent Pacific Ocean waters), one of the most productive and economically important regions of the world's oceans using a Juday net made of kapron sieve No. 49 (0.168 mm mesh) with a 0.1 m2 opening. The information in this dataset has already been used to quantify the inventory of marine biological resources and assess the waters of the Russian Far Eastern seas and adjacent Pacific Ocean. In 2016, five tabular reference books were printed in Russian in limited numbers containing the species composition, occurrence (number and percentage of samples), abundance and biomass (in individuals per cubic meter, milligrams per cubic meter) of zooplankton in the surveyed area. The data are grouped by species, developmental stages, size fractions (animal length of 0.6-1.2 mm "fine/small," 1.2-3.2 mm "medium" and >3.2 mm "large"), standard regions (their total area is more than 6 million km2), vertical layers of water, light and dark time of the day, four seasons of the year and multiyear periods, in which there were considerable changes in the biota of the region caused by global climate and oceanographic factors. This information has recently been verified, corrected, translated into English, transformed from text to digital format, and supplemented by GIS with maps of the standard regions by which data were aggregated using morphometric parameters (volume of water in cubic kilometers in the region, in its epipelagic 0-200 m, and upper epipelagic 0-50 m water layers, occupied area in square kilometers, longitude and latitude of their centroids in decimal degrees) to increase their availability to the scientific community worldwide. The data enable the evaluation of the total plankton stock of the Russian Far Eastern seas in the North Pacific (in trillions of specimens and thousands of tons), recalculate the volumetric characteristics of density into areal characteristics (in billions of specimens per square kilometer or tons per square kilometer), and, using previously published tables on calorific value and chemical composition of zooplankton, obtain their energy characteristics. Such data are crucial for the proper management of marine resources, aquaculture development, nature conservation, and the assessment of the anthropogenic impact on nature. The presented metadata provide a detailed description of how this unique dataset was created, sources and volume of gathered information, its benefits and drawbacks, some results on the quantitative inventory of marine biological resources and assessment of waters in the North Pacific, and future prospects for the use of this type of dataset in applied and fundamental research. There are no copyright restrictions on the data; please cite this data paper when the data are used in publications. [ABSTRACT FROM AUTHOR]

This study investigates how El Niño‐Southern Oscillation (ENSO) modulates winter cold anomalies over central Eurasia (CE) using reanalysis data during 1950–2019. It is found that ENSO can significantly influence winter air temperature over CE mainly through modulating the strength and location of the cyclonic anomaly of Ural blocking (UB) or long‐lived UB events. A strong (weak) cyclonic anomaly of UB on the southeastern (eastern) side of the Ural Mountains tends to occur over midlatitude (high‐latitude) Eurasia during La Niña (El Niño) winters. Such anomalous circulation leads to a strong (weak) cold anomaly over CE, especially over East Asia, due to enhanced (weakened) cold air advection toward the CE during La Niña (El Niño). The UB‐related cyclonic anomaly in the midlatitude (high latitude) side of Eurasia is shown to be related to weakened (enhanced) eastward extension of strong westerly winds over midlatitude Eurasia during La Niña (El Niño) winters. Plain Language Summary: Observations show that in recent decades a strong cold anomaly appears over Eurasia, especially over central Eurasia (CE). This cold anomaly shows notable variations on interannual, decadal and interdecadal timescales. However, what factors lead to its interannual variations is not well understood. Here we show that El Niño‐Southern Oscillation (ENSO) events can influence Eurasian winter air temperature by modulating the strength and location of the cyclonic anomaly of Ural blocking (UB) or the frequency of long‐lived UB events. A La Niña (El Niño) favors a strong (weak) cyclonic anomaly circulation located in the southeastern (eastern) side of the Ural Mountains in the midlatitudes (high latitudes), which leads to a strong (weak) cold anomaly over CE especially in the low latitude Eurasia (i.e., East Asia) through enhanced (weakened) cold air advection. These new results help us understand the physical cause of the interannual variability of the Eurasian cold anomaly modulated by ENSO. Key Points: This paper examines the causal relationship between the Ural blocking (UB) and Eurasian cold anomaly during the La Niña phase in winterEl Niño‐Southern Oscillation plays an important role in the interannual variability of winter cold anomaly over the EurasiaThe UB leads to stronger cold anomaly over the Eurasian during the La Niña than El Niño [ABSTRACT FROM AUTHOR]

Zooarchaeological research on the early Bronze Age in the Central Plain of North China has been focused mainly on two periods: the Erlitou culture (ca. 1900–1500 BC) and the late Shang Dynasty (ca. 1250–1046 BC). In this paper, our research on the animal bone assemblage from the Wangjinglou site, a walled city of the Erligang culture (ca. 1600–1400 BC), allows us to explore the use of animal resources and husbandry specializations during the time period between Erlitou and the late Shang. Domesticated animals, especially pigs and cattle, were dominant species in the faunal assemblage, while wild animals, mainly deer, were small in number. Moreover, the percentages of cattle and sheep were higher in prosperous phases at Wangjinglou and lower in the later phase during the site's decline. Analysis of the estimated death ages for various taxa suggests that pigs were raised for meat consumption, while sheep were used for secondary products. This research on Wangjinglou shows the varied nature of the animal economy at an early Bronze Age City in East Asia. [ABSTRACT FROM AUTHOR]

This special issue of World Water Policy focuses on water policy and practice in Africa, specifically addressing the increasing global water use and resulting water scarcity in regions like Central Africa, East Asia, and parts of South America. The document emphasizes the need for new approaches to address these challenges, including the adoption of water-saving irrigation technologies like micro-irrigation. The issue includes papers on state-of-the-art technologies, improving micro-irrigation in practice, and supportive water and agricultural policy and planning frameworks in Africa and beyond. The journal also discusses the policy conflicts surrounding the Grand Ethiopian Renaissance Dam and highlights the importance of innovative approaches to improve water use efficiency. Overall, this journal provides a comprehensive and informative resource for those interested in water security and policy. [Extracted from the article]

The quantitative relationship between Mesoscale Convective Systems (MCSs) and floods over East Asia has not been established. In this study, MCSs are clustered into four types with Self‐Organizing Map approach. Floods in June‐August of 2000–2021 are linked with different types of MCS by automated algorithms we constructed. We find that among the major floods (potential flood peak periods), 91% (87%) are related to MCS, 65% (78%) are dominated by MCS, and 38% (20%) are dominated by multi‐types of MCS. Types 1 and 2 MCS have higher flood‐inducing efficiencies than common MCS (Type‐4). Type‐1 MCS, characterized by the least number (2% of the total number), the largest precipitation volume, longest lifetime, slowest moving, strongest precipitation, can most efficiently produce floods. Type‐2 MCS, characterized by the second largest precipitation volume, more numerous than Type‐1 particularly over land, can induce floods not only relatively efficiently but also more frequently than Type‐1. Plain Language Summary: Mesoscale Convective Systems (MCS) can cause large flood events but how they work in East Asia at climatic scale remains unexplored. In this study, we tracked MCS over the time period of 2000–2021 and grouped them into four types using the Self‐Organizing Map approach. We connected summer floods with the four types of MCS using automated algorithms. We found that most large flood events and potential flood peak periods are dominated by MCS. Type‐1 MCS, which features large land‐rain area, longest lifetime, slowest movement and strongest precipitation, is most efficient in inducing floods. A Longer lifetime not only contributes to greater total precipitation volume but also increases the overlap area, thereby enhancing the precipitation volume per area. The slow movement further increases the overlap area. The high overlap area helps reduce the proportion of precipitation absorbed by the soil. Type‐2 MCS, which features with the second largest precipitation volume, occurs more frequently than Type‐1 especially over land, and can cause floods more frequently than Type‐1. These findings can enhance our understanding of flood formation over East Asia. Key Points: Among the major floods (potential flood peak periods) occurred in 2000–2021 summer, 91% (87%) are related to Mesoscale Convective Systems (MCS), and 66% (78%) are dominated by MCSType‐1 MCS is the most efficient among the four types in causing floods for its strongest precipitation rate, longest lifetime and slowest movementLong lifetime and slow movement increase the overlap area, boosting precipitation per area and reducing the proportion of rainfall absorbed by soil [ABSTRACT FROM AUTHOR]

A novel sub‐sampling method has been used to isolate the dynamic effects of the response of the North Atlantic Oscillation (NAO) and the Siberian High (SH) from the total response to projected Arctic sea‐ice loss under 2°C global warming above preindustrial levels in very large initial‐condition ensemble climate simulations. Thermodynamic effects of Arctic warming are more prominent in Europe while dynamic effects are more prominent in Asia/East Asia. This explains less‐severe cold extremes in Europe but more‐severe cold extremes in Asia/East Asia. For Northern Eurasia, dynamic effects overwhelm the effect of increased moisture from a warming Arctic, leading to an overall decrease in precipitation. We show that the response scales linearly with the dynamic response. However, caution is needed when interpreting inter‐model differences in the response because of internal variability, which can largely explain the inter‐model spread in the NAO and SH response in the Polar Amplification Model Intercomparison Project. Plain Language Summary: The projected loss of Arctic sea‐ice under 2°C global warming will cause large warming in the Arctic region and climate and weather anomalies outside the Arctic. The warming in the Arctic will mean warmer airmasses coming from the Arctic and also more moisture from the open Arctic Ocean. Furthermore, it will also change atmospheric circulation. These effects together will determine the impacts of Arctic warming. In this study, we introduce a novel sub‐sampling method to isolate atmospheric circulation change in response to the Arctic warming. The method involves selecting members of simulations from the experiment with future Arctic sea‐ice conditions, the average of which is equal to the average of the members of simulations in the experiment with present‐day Arctic sea‐ice conditions. We found that atmospheric circulation change in European regions is relatively weak so that warming effects will dominate the climate and weather response there. On the other hand, atmospheric circulation change will dominate the climate and weather response in East Eurasia. We also found that stronger atmospheric circulation changes will generally increase the response to the Arctic warming. We suggest caution when assessing whether different responses in different models can be interpreted as true differences in model physics. Key Points: A novel sub‐sampling method is introduced to isolate the role of dynamics in the response to projected Arctic sea‐ice lossA dynamical Siberian High response dominates the temperature response over East Eurasia while that of the North Atlantic Oscillation is weakInter‐model differences in Polar Amplification Model Intercomparison Project likely contain a large fraction of internal variability due to the unconstrained dynamic effects [ABSTRACT FROM AUTHOR]

Obvious biases in simulating tropical cyclone (TC) genesis of the current climate models hamper our understanding of TC changes. In this study, we found a delay of the seasonal cycle of TC genesis frequency over the western North Pacific (WNP) in most Coupled Model Intercomparison Project Phase 6 models. During the active TC season, the simulated south‐warming and north‐cooling surface temperature bias amplifies the meridional gradient and excites thermal winds. This weakens the western North Pacific Subtropical High and easterly monsoon trough, which further reduces TC genesis frequency over the western WNP in summer. But in autumn, positive TC genesis biases were only observed in coupled models over the eastern WNP. Both seasons contribute to the delayed seasonal cycle of TC frequency in models. Our findings highlight the importance of accurate simulation of surface temperature by climate models to TC simulations and aid in future model improvements. Plain Language Summary: Tropical cyclone (TC) is a devastating weather system generated over the tropical ocean, and the climate model serves as an important tool to study the long‐term variability of TC activity. Hence, it is imperative to explore the biases of climate models in simulating TC genesis. In this investigation, we find a substantial influence of surface temperature bias in Coupled Model Intercomparison Project Phase 6 (CMIP6) climate models on the simulation of the seasonal cycle of TC genesis frequency over the western North Pacific (WNP). The delay in the seasonal cycle of TC genesis frequency is widespread among most CMIP6 models. During boreal summer and autumn, the simulated bias of south‐warming and north‐cooling surface temperature increases its meridional gradient and triggers thermal winds. In summer, the weak western North Pacific Subtropical High and easterly monsoon trough, two crucial large‐scale circulation systems, cause a large negative TC genesis bias in models over the western WNP, substantially contributing to the delay of the seasonal cycle. Meanwhile, the relatively small positive bias of coupled models over the eastern WNP in autumn makes a secondary contribution. The combined contributions of these biases cause delays in seasonal simulation of TC genesis frequency. Key Points: Coupled Model Intercomparison Project Phase 6 models produce delayed seasonal cycles of tropical cyclone genesis frequency over the western North PacificBiases in East Asia summer monsoon and western North Pacific subtropical high lead to underestimation of tropical cyclone genesis during summerThe biased large‐scale circulation systems are further related to a warm southern and cold northern surface temperature bias [ABSTRACT FROM AUTHOR]

Objective: We aimed to examine the factors associated with treatment outcomes in patients with Alzheimer's disease (AD) after 1 year of acetylcholinesterase inhibitors (AChEI) treatment. Method: We obtained electronic medical records from a medical center in Southern Taiwan between January 2015 and September 2021. Participants aged ≥60 who were newly diagnosed with AD and had been prescribed AChEIs were included. Cognitive assessments were performed before the AChEIs were prescribed and at the 1 year follow‐up. Cognition progressors were defined as a Mini‐Mental State Examination decline of >3 or a Clinical Dementia Rating decline of ≥1 after 1 year of AChEI treatment. The relationship between the baseline characteristics and cognitive status after follow‐up was investigated using logistic regression analysis after adjusting for potential confounders. Results: A total of 1370 patients were included in our study (mean age, 79.86 ± 8.14 years). After adjustment, the body mass index (BMI) was found to be significantly lower in the progressor group [adjusted odds ratio (AOR): 0.970, 95% confidence intervals (95% CIs): 0.943 to 0.997, P = 0.033]. The usage of antipsychotics was significantly higher in the progressor group (AOR: 1.599, 95% CIs: 1.202 to 2.202, P = 0.001). The usage of benzodiazepine receptor agonists also tended to be significantly higher in the progressor group (AOR: 1.290, 95% CIs: 0.996 to 1.697, p = 0.054). Conclusion: These results suggest that patients with AD who receive 1 year of AChEI treatment and have a lower BMI or concurrent treatment with antipsychotics and benzodiazepine receptor agonists are more likely to suffer from cognitive decline. [ABSTRACT FROM AUTHOR]

The changes in the East Asian polar‐front jet (EAPJ) and the East Asian subtropical jet (EASJ) profoundly impact the weather and climate in East Asia. However, the link between aerosols and the jet streams is still unclear. Here, we investigated the decadal co‐variation of aerosols and the East Asian jet streams in the boreal winter during the period of 1980–2019. In synch with a positive change in aerosol optical depth over East Asia, 300‐hPa winds show an equatorward shift of the land branch of the EASJ, and weakened EAPJ and oceanic branch of the EASJ. This can be linked to the enhanced meridional temperature gradient along 30°–50° N but weakened in northern regions and the decreasing synoptic‐scale transient eddy kinetic energy over subtropical Pacific. Relative importance estimation of aerosols and ocean signals emphasized the contributions of aerosols in jet variations. In turn, meteorological conditions related to jet streams also contribute to variations in aerosols, the decadal co‐variations are a result of their interactions, particularly for the oceanic branch of EASJ. The findings would be helpful in providing potential indicators of climate change. [ABSTRACT FROM AUTHOR]

Wildfires emit atmospheric aerosols, affecting climate and air quality. Siberia is a known source region of wildfires. However, comprehensive knowledge regarding the impact associated with particulate matter pollution due to Siberian wildfires on climate and air quality and their effects on mortality and the economy under present and near‐future warmer atmospheric conditions remains poor. Thus, we performed model sensitivity experiments (atmospheric model and coupled atmosphere‐ocean model settings) simulating the effects of changing Siberian wildfire emissions under the present and near‐future climate conditions, using the Model for Interdisciplinary Research on Climate version 5 (MIROC5). Increased Siberian wildfire smoke likely caused a cooling effect in broad areas of the Northern Hemisphere and worsened the air quality near the source and in the downwind region (i.e., East Asia). The more Siberian wildfires occur, the more air pollution is present in those regions, which likely increases mortality and welfare losses there. However, the total impact of changing temperature on the gross domestic product under present and near‐future climate conditions is ambiguous. Our comprehensive results on the air quality changes due to Siberian wildfires under present and near‐future climate conditions suggest that increased efforts to limit the aerosol impact of Siberian wildfires are crucial to prevent possible excess mortality and economic losses. Plain Language Summary: Comprehensive knowledge of worsening air quality due to increased Siberian wildfires and its impact on climate and economy is needed to assess the impact of such fires both near their source and in the surrounding regions. Therefore, we performed global climate model simulations and analyzed the changing atmospheric aerosol emissions, including a precursor gas, from Siberian wildfires under the present and near‐future climate conditions using the Japanese global climate model called MIROC5. The increased aerosol emissions from Siberian wildfires generated a cooling effect in broad areas of the Northern Hemisphere and worsened the air quality near the source and in the downwind areas of East Asia. The effects we observed are associated with excess mortality and economic welfare losses. Future studies are needed to fully understand and prevent those negative impacts. Key Points: Comprehensive impacts of increasing Siberian wildfires on air quality, climate, and economy were estimated using the MIROC5 climate modelWe observed a cooling effect broadly across the Northern Hemisphere and worsened air quality near wildfire source and downwind regionsThe effects are closely related to lowering achievement rates of PM2.5 environmental standards, excess mortality, and economic losses [ABSTRACT FROM AUTHOR]

Climate change exacerbates the threat of water scarcity over the drylands in East Asia (DEA), the world's most densely populated arid region. The water cycle continuously supplies water to support all life. Previous studies have focused on the change in individual hydrological components over DEA; however, how the projected water cycle changes under climate warming remains unclear. We demonstrate the projected response of the water cycle to global warming in different seasons utilizing the Coupled Model Intercomparison Project Phase 6. Winter in the DEA presents an intensification of the water cycle, reflected in coherent increases in evapotranspiration (E), precipitation (P), runoff, and surface soil moisture. In contrast, summer will experience a weakened water cycle in the northwestern DEA, while the southeastern part exhibits the opposite trend. From the surface and atmospheric water balance perspective, we further attribute the changes in E and P to gain a more comprehensive understanding. The increasing E is attributed to the combined effects of P and the vapor pressure deficit during summer, whereas it is dominated by P in winter. The increased P in summer is primarily attributed to the horizontal dynamic and vertical thermodynamic components associated with the strengthening and westward expansion of East Asia summer monsoon in the future. During winter, the increased P is mainly due to the vertical dynamic and horizontal thermodynamic components associated with the enhancement of vertical ascending motion and increased moisture. Plain Language Summary: Water scarcity threatens 1–2 billion people living in drylands worldwide, with drylands in East Asia (DEA) having the largest population. Future climate change can alter the availability of water resources by altering the water cycle. Therefore, analyzing the water cycle's response to global warming during both summer and winter is vital for water management and climate adaptation, particularly in DEA. Under a high‐emissions scenario, winter will experience an intensified water cycle, manifested as coherent increases in evapotranspiration (E), precipitation (P), runoff, and surface soil moisture. In summer, a weakened water cycle is anticipated in northwestern DEA, while southeastern DEA is expected to show the opposite trend. Furthermore, we offer a quantitative attribution of the response of E and P to global warming to gain a more profound understanding. The attribution of E indicates that the supply of energy and water commonly dominate the increase in E during summer. The attribution of P illustrates that the westward expansion of the monsoon with enhanced southeastern winds favors increased P during summer. In winter, strengthened vertical ascending motions and increased water vapor content provide favorable conditions for enhancing P. Water cycle intensification is accompanied by more frequent extreme events, necessitating increased attention. Key Points: Future global warming will intensify the water cycle of drylands in East Asia in winterDuring summer, evapotranspiration will increase due to precipitation and vapor pressure deficit; in winter, it is dominated by the formerIn winter and summer, the dominant roles of the dynamic and thermodynamic components influencing future precipitation are different [ABSTRACT FROM AUTHOR]

Key points: Although mindfulness practices have originated in East Asia, including non‐English literature in systematic reviews of mindfulness interventions for cancer care will enable researchers to explore its application in various cultural contexts.A systematic analysis of online bibliographic databases: AMED, Embase, CINHAL, LILACS, MEDLINE, ProQuest Central, PsycINFO, PsycArticles, and WoS revealed that non‐English literature accounted for 2.72% of original research papers on mindfulness where no language restriction was applied.This suggests that the exclusion of non‐English literature in systematic reviews on mindfulness interventions for cancer care may not lead to a biased effect size if a search is restricted to articles indexed in an English language‐specific database.In comparison, an exploratory analysis of the China National Knowledge Infrastructure database revealed a higher percentage, up to 19.2% of indexed non‐English language literature.The authors caution that results of systematic reviews of mindfulness interventions that exclude non‐English databases may still constitute a biased generalizability because most literature published in non‐English journals are not indexed in major research databases. [ABSTRACT FROM AUTHOR]

Precipitation plays a significant role in human society and the environment, and how large‐scale climatic features influence precipitation has obtained worldwide attention. The nonhomogeneous hidden Markov model (NHMM) is a typical method to downscale large‐scale climatic elements to the regional level for many hydrologic applications. The traditional NHMM using point estimates of parameters has the risk to have no solutions for parameter estimation, but the Bayesian‐NHMM provides a Bayesian method to estimate parameters and avoids the risk. In this study, the suitability of the Bayesian‐NHMM in East Asia is evaluated. Two typical regions (i.e., the Yangtze River basin and the Zhujiang River basin in China) dominated by different climates were chosen to check model performance. Results show that: (1) the model could divide rainy‐season precipitation into several hidden states, whose variation is correspondent to the variability of monsoon and flux moisture transportation; (2) the model captures seasonality and inter‐annual variation of precipitation amount and also wet days during rainy season well in both river basins. These results suggest that the model could improve the prediction of daily precipitation in East Asia, which in turn could help many regions with similar climatic conditions worldwide to supervise floods and droughts. [ABSTRACT FROM AUTHOR]

Based on outputs of 28 coupled models from the Phase 6 of the Coupled Model Intercomparison Project (CMIP6), we show that the response of the Southeast Asian summer monsoon to the El Niño‐Southern Oscillation (ENSO) during post‐ENSO summer will likely strengthen in a warmer climate, which can be attributed to concurrently weakened sea‐surface temperature anomalies (SSTAs) in the western equatorial Pacific (WEP). The weakened WEP SSTAs are primarily caused by enhanced latent heat damping due to increased surface wind speed anomalies, which are associated with the eastward shift of the El Niño‐induced anomalous Walker circulation due to El Niño‐like sea surface temperature change in the tropical Pacific under global warming. Besides, the climatological zonal ocean currents will slow down due to the weakening of climatological Walker circulation, which also acts to weaken the WEP SSTAs via reducing the advection of anomalous temperature by the mean current. Plain Language Summary: As an important component of the Asian monsoon system, the Southeast Asian summer monsoon (SEASM) is crucial for the livelihoods of billions of people in East Asia, and is closely connected to a climate phenomenon called El Niño‐Southern Oscillation (ENSO). Understanding how the relationship between SEASM and ENSO will change in the future is important for enhancing our knowledge of climate change in East Asia. Outputs of 28 climate models from the Phase 6 of the Coupled Model Intercomparison Project show that ENSO will exert enhanced impacts on the SEASM in a warmer climate. The enhanced influences of ENSO on the monsoon will exacerbate the reduction of rainfall over the western North Pacific during the post‐El Niño summer. We find that such projected changes are mainly caused by weakened warm sea surface temperature (SST) anomalies (SSTAs) in the western equatorial Pacific (WEP). Further analyses indicate that the change in WEP SSTAs can be linked to the El Niño‐like change in climatological SSTs in the tropical Pacific. This study depicts detailed physical processes responsible for the projected changes in ENSO's impacts on the SEASM. Key Points: The effects of the El Niño‐Southern Oscillation on the Southeast Asian summer monsoon will strengthen under global warmingThe enhanced El Niño's impacts result from the weakened warm sea‐surface temperature (SST) anomalies in the western equatorial Pacific (WEP)The weakened WEP SST anomalies are related to the eastward shift of anomalous Walker circulation and the slackened mean zonal ocean currents [ABSTRACT FROM AUTHOR]

The impact of mid‐Pliocene boundary conditions on Afro‐Asian summer monsoon (AfroASM) rainfall is examined using the fully coupled Earth System Model EC‐Earth3‐LR. Our focus lies on the effects of varying CO2 concentration, diminished ice sheets and vegetation dynamics. We find that the enhanced AfroASM rainfall is predominantly caused by the "warmer‐gets‐wetter" mechanism due to elevated CO2 levels. Additionally, the ice sheet, similar in size to that of the mid‐Pliocene era, creates several indirect effects. These include sea ice‐albedo feedback and inter‐hemispheric atmosphere energy transport. Such influences result in the southward shift of Hadley circulation and formation of Pacific‐Japan pattern, leading to reduced rainfall in North African and South Asian monsoon regions but increased rainfall in East Asian monsoon region. Interestingly, while dynamic vegetation feedback has a minimal direct effect on AfroASM rainfall, it significantly influences rainfall in the mid‐high latitudes of the North Hemisphere by enhancing water vapor feedback. Plain Language Summary: The mid‐Pliocene (3.3–3.0 Ma) was a pre‐Quaternary warming period with similar high CO2 level as we have today. The period is often considered as an analog for future greenhouse driven climate projections. Previous studies indicate that the Afro‐Asian summer monsoon (AfroASM) rainfall was more abundant then. However, the underlying mechanisms of relative contributions of boundary conditions on increased AfroASM rainfall remains to be clarified. Here, we use an Earth System Model, performed nine simulations to study the separate effects of CO2 level, ice sheets size, and vegetation dynamics on AfroASM rainfall patterns during the mid‐Pliocene. We found that (a) A rise in CO2 concentration during the mid‐Pliocene enhanced AfroASM rainfall through "warmer‐gets‐wetter" mechanism. (b) The dynamics of the ice sheet during this period, including both melting and distribution changes, contributed to more pronounced warming in South Hemisphere than the north due to ice‐albedo feedback. This change affected global atmospheric circulation, leading to decreased rainfall in North Africa and South Asia, but increased rainfall in East Asia. (c) We observed that during the mid‐Pliocene, vegetation expanded and move further north in the North Hemisphere. This increases summer rainfall at Northern mid‐high latitudes through local water vapor feedback. Key Points: Elevated CO2 levels during mid‐Pliocene increase Afro‐Asian summer monsoon rainfall mainly due to the "warmer‐gets‐wetter" mechanismMid‐Pliocene ice sheets changes favor to reduce North African/South Asian monsoon rainfall and increase East Asian monsoon rainfallDynamic vegetation feedback has less effect on Afro‐Asian monsoon, but more on mid‐high latitudes rainfall [ABSTRACT FROM AUTHOR]

Miscanthus is a genus of perennial grasses native to East Asia that shows promise as a biofuel energy source. Breeding efforts for increasing biofuel capability in this genus have focused on two species, namely M. sinensis (Msi) and M. sacchariflorus (Msa). For these efforts to succeed, it is critical that both Msi and Msa, as well as their interspecific crosses, can be grown at a wide range of latitudes. Therefore, the purpose of this study was to investigate how well existing data from Msi and Msa trials grown at locations throughout the northern hemisphere can train state‐of‐the‐art genomic selection (GS) models to predict genomic estimated breeding values (GEBVs) of dry yield for untested Msi and Msa accessions in untested environments. We found that accounting for genotype by environment interaction in the GS model did not notably improve predictive ability. Additionally, we observed that locations at lower latitudes showed higher predictive ability relative to locations at higher latitudes. These results suggest that it is crucial to increase the number of trial locations at higher latitude locations to investigate the source of this correlation. This will make it possible to train GS models using data from environments that are similar to growing conditions at the locations targeted by Msi and Msa breeders. Such an increase of trial locations in target environments could pave the way toward advancing breeding efforts for overwintering ability in Msi and Msa, and ultimately support the potential of Miscanthus as a biofuel crop. We evaluated the extent to which existing data from two Miscanthus species grown at multiple locations can be used for genomic prediction. We assessed the ability of two multi‐environment genomic prediction models to predict breeding values of yield for genotypes and environments that were not included in a training set. We found that considering genotype‐by‐environment interactions did not substantially improve predictive ability, and that predictive abilities tended to be lower at locations at higher latitudes. [ABSTRACT FROM AUTHOR]

Populations of Eurasian otters Lutra lutra, one of the most widely distributed apex predators in Eurasia, have been depleted mainly since the 1950s. However, a lack of information about their genomic diversity and how they are organized geographically in East Asia severely impedes our ability to monitor and conserve them in particular management units. Here, we re‐sequenced and analyzed 20 otter genomes spanning continental East Asia, including a population at Kinmen, a small island off the Fujian coast, China. The otters form three genetic clusters (one of L. l. lutra in the north and two of L. l. chinensis in the south), which have diverged in the Holocene. These three clusters should be recognized as three conservation management units to monitor and manage independently. The heterozygosity of the East Asian otters is as low as that of the threatened carnivores sequenced. Historical effective population size trajectories inferred from genomic variations suggest that their low genomic diversity could be partially attributed to changes in the climate since the mid‐Pleistocene and anthropogenic intervention since the Holocene. However, no evidence of genetic erosion, mutation load, or high level of inbreeding was detected in the presumably isolated Kinmen Island population. Any future in situ conservation efforts should consider this information for the conservation management units. [ABSTRACT FROM AUTHOR]

Based on observations and numerical simulations, this study explores the responses of Asian precipitations in summer to the vertical structure of Stratospheric quasi‐biennial oscillation (QBO), and the relevant mechanisms. Compared to the QBO phase defined by a particular level traditionally, considering QBO's vertical structure leads to more significant precipitation responses. When the tropical zonal winds exhibit easterlies (westerlies) at 70 hPa and westerlies (easterlies) at both 30 and 50 hPa, there are downwellings (upwellings) over tropics and upwellings (downwellings) over mid‐latitudes in the upper troposphere and lower stratosphere. The meridional movement of the subtropical westerly jet is related to this secondary circulation, accompanied by anomalies of the South Asian High. These circulation anomalies lead to anomalous lower tropospheric circulations, causing abnormal vertical velocities and moisture transports, resulting in increased precipitation over South Asia and decreased precipitation in the Yangtze River basin. Plain Language Summary: With large populations and developed agriculture, understanding the factors influencing summer precipitation in South and East Asia is crucial for predicting future changes. While the quasi‐biennial oscillation (QBO) has been recognized as a predictive factor for summer precipitation in these regions, its effects are still uncertain. This study finds that the vertical structure of QBO should be considered when predicting summer precipitation over South and East Asia, rather than the QBO index on a certain level. When the zonal winds over the tropics exhibits the westerlies at 30 and 50 hPa and easterlies at 70 hPa, there's increased precipitation in South Asia, and decreased precipitation in the Yangtze River basin, and vice versa. The possible mechanism is the QBO's vertical structure stimulates secondary circulations, leading to anomalies in the SWJ and the SAH, resulting in summer precipitation changes. These findings could contribute to the extended forecast for summer precipitation in South and East Asia. Key Points: Summer precipitation in South and East Asia significantly responds to the specific vertical structure of the quasi‐biennial oscillation (QBO)Easterlies at 70 hPa and westerlies at 30 and 50 hPa drive more summer precipitation in South Asia while less in Yangtze River BasinThe mechanism is abnormally strong secondary circulation motivated by QBO affects the subtropical jet stream and the South Asian High [ABSTRACT FROM AUTHOR]

The Multiband Ultraviolet Spectrum Imager (MUSI) is an optical remote sensing instrument scheduled to launch on the Fengyun‐4C meteorological satellite in 2024. MUSI is designed to measure the airglow emissions between ∼120 and 160 nm above the East Asia and Pacific region from a geostationary orbit to infer ionospheric parameters. Here we develop a lookup‐table algorithm for retrieving the peak electron density (nmF2) and the Total Electron Content (TEC) from nighttime observations of the OI 135.6 nm emission. The algorithm takes into account the north‐south asymmetry of the equatorial ionization anomaly and the atmospheric variations with solar activity and local time. Analysis of synthetic observations shows that the assumptions made in the algorithm only lead to ∼2%–4% uncertainties in the retrievals under the modeled ionospheric conditions. The algorithm is verified by retrieving nmF2 and TEC from the Global‐Scale Observations of the Limb and Disk (GOLD) mission and comparing with coincided radio measurements. The comparison indicates almost negligible systematic differences (typically less than ∼3%) between the GOLD and the ionosonde nmF2, which are within the error limit of the GOLD retrievals. The accuracy of the GOLD TEC retrievals is shown to be comparable to (or in some sense even better than) that of the measurements from the Global Navigation Satellite System. Several simplified yet robust retrieval methods are also developed, which can be readily implemented for both existing and upcoming missions. Our results promote far ultraviolet (FUV) remote sensing to be a key technology for accurate determination of the ionospheric state. Key Points: We develop a lookup‐table algorithm for ionosphere retrieval with the FUV spectral imager on the Fengyun‐4C geostationary satelliteAssumptions made in the algorithm lead to only ∼2%–4% uncertainties in the nmF2 and Total Electron Content (TEC) retrievals under the modeled ionospheric conditionsThe algorithm is verified by retrieving nmF2 and TEC from the Global‐Scale Observations of the Limb and Disk observations and comparing with external radio measurements [ABSTRACT FROM AUTHOR]

The variability of the summer North Pacific Subtropical High (NPSH) has substantial socioeconomic impacts. However, state‐of‐the‐art climate models significantly disagree on the response of the NPSH to anthropogenic warming. Inter‐model spread in NPSH projections originates from models' inconsistency in simulating tropical precipitation changes. This inconsistency in precipitation changes is partly due to inter‐model spread in tropical sea surface temperature (SST) changes, but it can also occur independently of uncertainty in SST changes. Here, we show that both types of precipitation uncertainty influence the NPSH via the Matsuno‐Gill wave response, but their relative impact varies by region. Through the modulation of low cloud fraction, inter‐model spread of the NPSH can have a further impact on extra‐tropical land surface temperature. The teleconnection between tropical precipitation and the NPSH is examined through a series of numerical experiments. Plain Language Summary: The North Pacific Subtropical High (NPSH) is a semi‐permanent high‐pressure system located in the subtropical North Pacific. The variability in the summer NPSH has a significant impact on the monsoon and typhoons over East Asia and the hydroclimate of California. However, future projections of the NPSH using state‐of‐the‐art climate models remain highly uncertain. By evaluating how much individual models deviate from the multi‐model mean at different locations, we find four hot spots of high uncertainty in NPSH projections. Our analysis further reveals that the primary source of model variance in changes in the NPSH is tropical precipitation, which can be attributed to both inter‐model SST‐driven and non‐inter‐model SST‐driven factors. Through numerical experiments, we demonstrate that the teleconnection between tropical precipitation and the NPSH is achieved through wave propagation. Key Points: Model spread in the response of the summer North Pacific Subtropical High (NPSH) to CO2 stems from model spread in simulating tropical processesModel spread in tropical sea surface temperature (SST) changes modulates the NPSH by influencing tropical precipitationModel spread in tropical precipitation changes independent of model spread in SST changes also adds to the uncertainty of the NPSH response [ABSTRACT FROM AUTHOR]

Many previous studies have documented the relationship between the North Pacific Oscillation (NPO) and the weather/climate of upstream and downstream regions. However, the stability of NPO precursor signals of East Asian summer precipitation, which is important for climate prediction, has received little attention. This study identified temporal variations in the connection between the May NPO and subsequent midsummer precipitation over Northeast China (NEC) during 1961–2020. During 1986–2010, the correlation between the May NPO and midsummer precipitation over NEC was found significantly positive, whereas the relation was found statistically insignificant during 1961–1985/2011–2020. Further results indicated that the NPO stimulated a Rossby wave source over the North Pacific that was stronger during 1986–2010 than during 1961–1985/2011–2020. The Rossby wave source anomalies shifted to North America and to the North Atlantic during the subsequent June and midsummer, respectively. Consequently, a teleconnection wave train, which originated over the North Pacific, propagated eastward to North America, across the North Atlantic, and on to East Asia on the subseasonal time scale, influencing midsummer precipitation over NEC through modulation of the atmospheric circulation (e.g., horizontal wind, moisture transport, and vertical movement). Moreover, the intensified Rossby wave anomalies associated with the May NPO were attributed to the strengthened NPO, which could be related to the enhanced standard deviation of SLP over the North Pacific. Additionally, the strengthened out‐of‐phase relation between the NPO and the North Atlantic Oscillation, resulting from changes in the background circulation, partially contributed to intensification of the Rossby wave train. Plain Language Summary: The North Pacific Oscillation (NPO) is an important intrinsic atmospheric variability which is characterized by a north–south seesaw in sea level pressure over the North Pacific Ocean. The NPO has substantial influences on the weather/climate conditions over North America and East Asia. However, the relation between NPO and East Asian climate is not stationary. This study identified a temporal variation in the connection between the May NPO and the midsummer precipitation over Northeast China (NEC) during 1961–2020, which shows a strong (weak) correlation during 1986–2010 (1961–1985 and 2011–2020). This is attributed to the different atmospheric circulation patterns caused by the NPO during the three periods. The NPO can simulate stronger perturbation to the atmosphere during 1986–2010 than during 1961–1985 and 2011–2020. Consequently, the perturbed atmospheric waves can propagate eastward to North America, across the North Atlantic, and toward East Asia during 1986–2010, leading to anomalous atmospheric circulation in East Asia and influencing the midsummer precipitation over NEC. The strengthening of the NPO and the enhanced relation between the NPO and North Atlantic Oscillation during 1986–2010 can explain the above changes. This study may deepen our understanding of the influence of NPO on the East Asian climate and may be meaningful for climate prediction. Key Points: The effect of May North Pacific Oscillation (NPO) on summer rainfall at Northeast China (NEC) is not stable, with a strong (weak) relation for 1986–2010 (for 1961–1985 and 2011–2020)This is attributed to a stronger Rossby wave source stimulated by NPO during 1986–2010 than during 1961–1985 and 2011–2020The strengthened Rossby wave related with NPO is attributed to the intensification of NPO and to the enhanced relation between NPO and North Atlantic Oscillation [ABSTRACT FROM AUTHOR]

Modeling deep convection accurately in tropical regions is important. However, biases remain in current trigger functions. To alleviate the overestimation of frequency and wrong depiction of the diurnal cycle, we propose a deep convection trigger function, ResU‐Deep, based on the framework of U‐net with three modifications to better suit the problem of deep convection identification: (a) adding the upsampling process into the encoder part, (b) replacing the double convolution block with a residual‐convolutional block, and (c) adding a dynamic weight into the loss function. Thirty‐three environmental variables within tropical regions are used in ResU‐Deep, including 31 features from ECMWF atmospheric reanalysis (ERA5) data set, and two historical convection fields. Tropical Rainfall Measuring Mission 3B42 data set is used as the precipitation observation. Central America, North Africa, South and East Asia, and West Pacific Ocean within 0°∼30°N are selected as the study regions for the high frequency of deep convection activities. ResU‐Deep, incorporating the surrounding information, is separately trained and evaluated in four regions and has the F1‐scores of 58%, 53%, 60%, and 63% for the occurrence, outperforming the single‐column‐based machine learning methods. Also, a unified model has similar performance in four regions. Further comparisons are made with convective available potential energy‐based trigger functions in Southern Great Plains. Results show that ResU‐Deep can capture the trends and peaks of diurnal cycles on complex terrains in large regions. According to feature importance test, the contribution levels of environmental features are different in four regions, indicating the model can learn the mechanisms of deep convection in specific region, thus improving the prediction accuracy. Plain Language Summary: The deep convection trigger function is a widely‐used method to determine the occurrence of deep convection in general circulation models. However, many trigger functions face the overestimation of deep convections and cannot accurately capture the variations of occurrence frequency. We propose a convection trigger function based on deep learning, called ResU‐Deep, to improve the trigger function in tropical regions. Three modifications are made based on the framework of U‐net. Both the architecture and the loss function are modified to improve the model's performance and increase the training speed. Thirty‐one environmental variables from ERA5 data set and two historical deep convection occurrence information are used as the features. Central America, North Africa, South and East Asia, and West Pacific Ocean within the tropics have high deep convection frequency. The model is trained and tested independently on each site, reflecting the non‐uniform physical mechanisms for deep convection. Also, a unified model has similar performance. Besides, incorporating surrounding information in ResU‐Deep can help improve prediction accuracy. To compare with the convective available potential energy‐based trigger functions, we test the model on Southern Great Plains in central United States. Results show that deep learning is a promising solution to identify deep convection. Key Points: A location‐aware and deep‐learning‐based deep convection trigger function is proposed to improve the diurnal cycle simulation in tropicsResults show that terrain information, temporal dependence of convection, and water vapor content are essential for predicting convectionIncluding information from neighboring atmospheric columns can improve the performance of the deep convection trigger function [ABSTRACT FROM AUTHOR]

In this study, a global variable‐resolution modeling framework of atmospheric dust and its radiative feedback is established and evaluated. In this model, atmospheric dust is simulated simultaneously with meteorological fields, and dust‐radiation interactions are included. Five configurations of global mesh with refinement at different resolutions and over different regions are used to explore the impacts of regional refinement on modeling dust lifecycle at regional and global scales. The model reasonably produces the overall magnitudes and spatial variabilities of global dust metrics such as surface mass concentration, deposition, aerosol optical depth, and radiative forcing compared to observations and previous modeling results. Two global variable‐resolution simulations with mesh refinement over major deserts of North Africa (V16 km‐NA) and East Asia (V16 km‐EA) simulate less dust emissions and smaller dry deposition rates inside the refined regions due to the weakened near‐surface wind speed caused by better resolved topographic complexity at higher resolution. The dust mass loadings over North Africa are close to each other between V16 km‐NA and the quasi‐uniform resolution (∼120 km) (U120 km), while over East Asia, V16 km‐EA simulates higher dust mass loading. Over the non‐refined areas with the same resolution, the difference between global variable‐resolution and uniform‐resolution experiments also exists, which is partly related to their difference in dynamic time‐step and the coefficient for horizontal diffusion. Refinement at convection‐permitting resolution around the Tibetan Plateau (TP) simulates less dust due to its more efficient wet scavenging from resolved convective precipitation around the TP against coarse resolution. Plain Language Summary: Mineral dust plays an important role in Earth's climate system. Numerical simulation of dust and its impacts on a regional scale still has large uncertainties, partly due to the relatively coarse horizontal resolution. Limited‐area simulation at relatively high resolution can generally better characterize dust and its impacts on a regional scale; however, lateral boundary conditions may introduce some numerical issues and constrain regional feedback, such as dust‐cloud and dust‐radiation interactions, to large‐scale circulation. In this study, a novel modeling framework of atmospheric dust and its climatic feedbacks with the capability of global variable‐resolution simulation is established and evaluated. The model produces reasonable global spatial distributions of dust compared to observations and previous studies. The difference between the simulations at global quasi‐uniform resolution and global variable resolution with regional refinement over East Asia and North Africa is significant, particularly with refinement at convection‐permitting resolution. This model may be used in the future to provide new insights into the impacts of dust on regional and global climate systems. Key Points: A modeling framework of atmospheric dust with the capability of global variable‐resolution simulation is introduced and evaluatedExperiments with regional refinement produce less dust emissions and mass loading and smaller dry deposition due to weaker surface windRefinement at convection‐permitting resolution simulates stronger wet scavenging and less dust mass compared to coarse resolution [ABSTRACT FROM AUTHOR]

Antibiotic overuse and the subsequent environmental contamination of residual antibiotics poses a public health crisis via an acceleration in the spread of antibiotic resistance genes (ARGs) through horizontal gene transfer. Although the occurrence, distribution, and driving factors of ARGs in soils have been widely investigated, little is known about the antibiotic resistance of soilborne pathogens at a global scale. To explore this gap, contigs from 1643 globally sourced metagnomes are assembled, yielding 407 ARG‐carrying pathogens (APs) with at least one ARG; APs are detected in 1443 samples (sample detection rate of 87.8%). The richness of APs is greater in agricultural soils (with a median of 20) than in non‐agricultural ecosystems. Agricultural soils possess a high prevalence of clinical APs affiliated with Escherichia, Enterobacter, Streptococcus, and Enterococcus. The APs detected in agricultural soils tend to coexist with multidrug resistance genes and bacA. A global map of soil AP richness is generated, where anthropogenic and climatic factors explained AP hot spots in East Asia, South Asia, and the eastern United States. The results herein advance this understanding of the global distribution of soil APs and determine regions prioritized to control soilborne APs worldwide. [ABSTRACT FROM AUTHOR]

A high‐precision earthquake catalog is made from continuous waveform data recorded at 360 portable seismographs deployed for one month in the Changbaishan‐Tianchi volcanic area based on an automatic earthquake detection and location workflow. Then we investigate detailed 3‐D structures of P and S wave velocities (Vp and Vs) and Vp/Vs ratio of the crust beneath the study region. Our results reveal a high‐Vp/Vs zone accompanied with active volcanic earthquakes beneath the Tianchi caldera at ∼5 km depth, which may reflect a magma chamber. The intense seismic activities within 2 km depth beneath the Tianchi caldera from 2002 to 2005 occurred directly above the magma chamber revealed by this study, which could be related to upward migration of high‐pressure volatiles originating from the magma chamber. A potential middle‐crustal magma chamber might provide continuous magmatic materials feeding the upper‐crust magma chamber and lead to ruptures of surrounding rocks, resulting in two swarms of volcanic seismicity during the observation period. We deem that the diverse eruption styles of the Changbaishan volcano are closely associated with the multilevel structure of magma chambers in the upper and middle crust. Plain Language Summary: It is difficult for the earthquake monitoring system to identify and locate microearthquakes by using traditional seismic detection methods due to their weak signals, leading to a relatively low quantity and quality of seismic data in a study region, which cannot meet the demands of high‐resolution seismic tomography. In this study, we detect and locate microseismic events beneath the Changbaishan‐Tianchi volcanic area using 1‐month waveform data recorded at our 360 portable seismographs deployed in the volcanic area. Then we investigate high‐resolution 3‐D crustal structures of P and S wave velocities (Vp, Vs) and Vp/Vs ratio beneath the study area. Our results reveal a possible crustal magma reservoir at ∼5 km depth beneath the Tianchi caldera, which is accompanied with volcanic earthquakes during our observation period. In addition, small earthquakes occurred actively at a depth of ∼2 km during 2002–2005, which are located right above the magma reservoir. We deem that the joint effect of magma reservoirs in the upper and middle crust could explain the active volcanic seismicity and distinctive eruption behaviors of the Changbaishan volcano. Key Points: A magma chamber at ∼5 km depth beneath the Tianchi caldera of the Changbaishan volcano (CBV) is revealedThe CBV unrest during 2002–2005 was related to reactivation of the crustal magma chamberDistinctive eruption behaviors of the volcano are related to multilevel magma chambers in the crust [ABSTRACT FROM AUTHOR]

Autumn precipitation in the central region of China (APCC) can considerably influence on agricultural production and human livelihood. With reanalysis data from 1979 to 2020, it revealed that APCC is significantly affected by the second mode of the meridional wind field at 200 hPa over the Eurasian continent on the interannual scale, which featured a quasi‐barotropic "+‐+" wave‐like pattern from Europe to China (EC pattern) in extratropical zone. When the EC pattern is in a positive phase, central China lags behind the downstream positive geopotential height (anticyclone) anomaly. In this context, the transport of moisture from the south and east is enhanced and the advancement of the southerly monsoon is blocked, providing sufficient water vapor to support the occurrence of APCC. Further diagnosis revealed that local ascending motion is strengthened owing to the warm advection induced by anomalous southerly and positive vorticity advection associated with the anomalous anticyclone over East Asia. Additionally, wave flux analysis and model simulation suggest that the EC pattern results from the propagation of stationary Rossby wave, which could be excited by dipole sea surface temperature anomalies in the North Atlantic. These discoveries will contribute to improving the predictability of APCC. Plain Language Summary: The interannual variability of autumn precipitation in central China (APCC) is largely affected by a wave train over the Eurasian continent (EC pattern), which can influence the local moisture and dynamic uplift conditions by an anomalous anticyclone over East Asia. The North Atlantic dipole sea surface temperatur anomalies play an important role in the prediction of APCC, and could stimulate an extratropical teleconnection to shape the EC pattern over the Eurasian continent, as confirmed in the linear baroclinic model. Key Points: The autumn rainfall in central China is related to the second mode of V200 (EOF2) over the Eurasian continent on interannual timescaleEOF2 features in a "+‐+" wave‐like pattern, resulting in an anticyclone anomaly over East Asia in its positive phaseExtratropical EOF2 pattern wave train could be excited by the North Atlantic dipole sea surface temperature anomaly [ABSTRACT FROM AUTHOR]