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The study examines the relationship between sudden- and gradual-onset climate events and migration, hypothesizing that this relationship is mediated by the adaptive capacity of affected individuals. We use survey data from regions of Cambodia, Nicaragua, Peru, Uganda, and Vietnam that were affected by both types of events with representative samples of non-migrant residents and referral samples of migrants. Although some patterns are country-specific, the general findings indicate that less educated and lower-income people are less likely to migrate after exposure to sudden-onset climate events compared to their counterparts with higher levels of education and economic resources. These results caution against sweeping predictions that future climate-related events will be accompanied by widespread migration. [ABSTRACT FROM AUTHOR]

Urban informal settlements have, over the years, been centres of conflicting development debates, yet, for people with low socio-economic status, these are areas of opportunities. However, the "peripheral" nature of these locations has far-reaching implications on how people in these areas participate in decision-making processes that affect them. Lately, the effects of climate-related events have also added another layer of socio-economic, political, and environmental challenge to the dynamics of life in the marginal areas of the urban setting. The purpose of this paper is to critically examine how people in marginal informal settlements of Lilongwe City respond to climate-related events and interact with the wider ecosystem of development stakeholders. The major thesis of the paper is that while critical policymakers ignore these peripheral voices in the provision of basic services, an enhanced support to these informal settlements can prove positive if efforts are harnessed to mitigate the effects of climate-related events and urban marginality and amplify marginal voices to change social policies for the good of all. This paper uses the case of Lilongwe City where three informal settlements of Mtandire, Kaliyeka, and Kawale form part of the study. [ABSTRACT FROM AUTHOR]

Rivers are critical ecosystems for protecting and harboring high biodiversity. Tropical rivers particularly are unique for facing extreme climatic events under the current accelerated disruption from human activities. The Bobos-Nautla river basin is exposed to climatic events and disturbances from anthropogenic impacts that stress aquatic organisms. We assessed the health condition of this river system using a non-conventional biomonitor, Corydalus sp., with a set of early-warning biomarkers including lipid peroxidation levels (LPO) and antioxidant activity, superoxide dismutase (SOD), catalase (CAT), glutathione peroxidase (GPx), and the neurotransmitter acetylcholinesterase (AChE) considering their spatial and temporal variations. Biomarkers and water quality parameters were analyzed, and the integrated biomarker response (IBR) was assessed as a stress index. Biomarkers showed no significant spatial differences; however, a high-stress period during the rainy season was detected, evidenced by the highest LPO levels; this period is related to the leaching of allochthonous materials from agricultural and urban zones. The peak IBR value during the rainy season confirmed the seasonality of biomarkers. A slight increase in IBR was recorded in lowlands, seemingly associated with agricultural land and human settlements. A principal component analysis showed nutrient enrichment during the rainy season and depletion during the cold-dry season, together with a peak activity of antioxidant enzymes. These results highlight the importance of climatic events such as the rainy season on the health condition of Corydalus sp., which is highly sensitive to the complex mixtures of pollutants that enter the waterbody during extreme climatic events, promoting oxidative stress. Our results also showed the ability of Corydalus sp. to recover and return to a basal level. [ABSTRACT FROM AUTHOR]

This study employs the event study method on the daily closing prices of 385 listed firms in Turkey from December 2020 to December 2022 to examine the market reactions to two significant climate-related events: the Glasgow Climate Pact (GCP) and the Sharm el-Sheikh Implementation Plan (SSIP). The GCP event triggered predominantly adverse market reactions, with significant and negative abnormal returns observed before and after the event and an adverse event day return. Conversely, the SSIP event generated a mixed market response, characterized by significant negative abnormal returns before the event and significant positive abnormal returns after the event. Additionally, the energy sector firms have been vulnerable to the SSIP, given their declining returns, while other sectors experienced significant positive returns. The cross-sectional regression analysis highlights the impact of firm-level characteristics on abnormal returns. For the GCP event, firm leverage, firm size, book-to-market ratio, and past returns exhibit significant associations with abnormal returns during different periods. Similarly, for the SSIP event, firm size, book-to-market ratio, past returns, and past volatility demonstrate significant relationships with abnormal returns. The findings suggest that firms should align their strategies with climate goals and capitalize on emerging clean energy and sustainability opportunities to maintain share prices. Investors must carefully evaluate climate-related events’ impact and consider firm-level characteristics when making investment decisions. This study contributes to understanding market reactions to climate events and provides insights for firms and investors in navigating the evolving landscape of climate change. [ABSTRACT FROM AUTHOR]

Climate events pose major challenges to food production and the livelihoods of rural inhabitants in northern Laos, where upland rice using swidden production is an important crop. The onset of the rainy season in this area is one such climate event, and it has occurred earlier and with less regularity in recent years. Not all households are able to cope with these changes. This study examines the ability of local farmers to cope with rice insufficiency. This investigation also clarifies household strategies in dealing with the climate event. We randomly interviewed 63 of 95 household heads, and performed a paired sample t test to examine the significance of differences in three household groups between the 2010 normal climate and the 2011 climate event. The groups were categorized according to rice self-sufficiency in 2011: groups I are households with rice self-sufficiency, group II are those facing a rice shortage of up to 3 months, and group III are those with insufficient rice for over 3 months. We also conducted a one-way ANOVA to examine the significance of differences in livelihood strategies among the three groups. We found that the household labor force was the most important factor in enhancing the villagers' ability to deal with the climate event and that the level of impact of that event shaped their coping strategies. Households with substantial labor force had more options for coping strategies than those with smaller ones. The villagers faced different levels of impact and adopted different coping strategies accordingly. Non-timber forest product collection was the principle livelihood strategy in response to non-climate factors such as education, access to health services, provision of equipment and clothing, and overcoming the impact of the climate event. Households heavily affected by the early rainy season onset tended to engage in intensive activities such as off-farm activity and outside work, rather than their major livelihood activities in the village (upland crop and livestock production). [ABSTRACT FROM AUTHOR]

Progress in Chinese loess research made in recent 15 years was introduced in this paper, including mainly distribution and paleoenvironment significance of Chinese loess, new development of loess formation age, red-brown paleosol types and environmental change, loess-paleosol sequence and climate cycles, monsoon strength change during last interglacial and last glacial periods in the Loess Plateau, climate events, and source areas of loess and material. [ABSTRACT FROM AUTHOR]