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Understanding the characteristics of minute‐scale short‐duration intense rainfall and its possible link with urbanization is valuable for addressing urban climate change and evaluating biases in high‐resolution historical precipitation data series. This study analyses the long‐term trends of rainy‐season minute‐scale intense rainfall events at different continuous time periods based on precipitation data from 20 national meteorological stations in the Beijing area covering the period from 1961 to 2021. This study shows that during the whole period analysed, the number of events of intense rainfall lasting 15 min or longer decreased, while the number of shorter‐duration events and the accumulated precipitation increased. The frequency and amount of minute‐scale intense rainfall recorded by urban stations are generally higher than those recorded by rural stations in terms of climatological means. The signal of the urbanization effect in minute‐scale precipitation changes is detectable, with the contribution of urbanization to the trends in average precipitation of 30‐min intense rainfall being 68.8%, whereas the contributions with respect to the frequency of 20‐ and 30‐min intense rainfall and the maximum precipitation of intense rainfall with a duration of 45 min reach 100%. The results of the analysis can provide reference for understanding long‐term changes in short‐duration rainfall and the possibility that they are driven by local anthropogenic activity, as well as bias in the minute‐scale precipitation data series of urban observation sites when they are used in studies of large‐scale intense precipitation changes. [ABSTRACT FROM AUTHOR]

Human-induced environmental and climate change are widely blamed for causing rapid global biodiversity loss, but direct estimation of the proportion of biodiversity lost at local or regional scales are still infrequent. This prevents us from quantifying the main and interactive effects of anthropogenic environmental and climate change on species loss. Here, we demonstrate that the estimated proportion of species loss of 252 key protected vertebrate species at a county level of China during the past half century was 27.2% for all taxa, 47.7% for mammals, 28.8% for amphibians and reptiles and 19.8% for birds. Both human population increase and species richness showed significant positive correlations with species loss of all taxa combined, mammals, birds, and amphibians and reptiles. Temperature increase was positively correlated with all-taxa and bird species loss. Precipitation increase was negatively correlated with species loss of birds. Human population change and species richness showed more significant interactions with the other correlates of species loss. High species richness regions had higher species loss under the drivers of human environmental and climate change than low-richness regions. Consequently, ongoing human environmental and climate changes are expected to perpetuate more negative effects on the survival of key vertebrate species, particularly in high-biodiversity regions.

The present study aims to detect the variation of precipitation extreme events in the northern part of the Korean Peninsula during 1961–2020, as well as to investigate its possible causes, based on daily precipitation data from 37 representative stations. Nonparametric tests such as Mann‐Kendall and Kendall‐tau were used to detect statistical characteristics of changes in precipitation indices and climate variables. Findings are as follows: (a) the annual total precipitation manifested a clear shifting point in 1968, with a decreasing rate of about −37.7 mm/decade, conversely, daily precipitation intensity had a clear upward trend, and extreme precipitation events above 100 mm/day became more frequent. (b) There occurred significant upward trends of 8.9 mm/decade for intense rainfall (>95th percentile) and 6.3 mm/decade for extreme intense rainfall (>99th percentile). (c) The continuous wet (dry) days showed a decreasing (increasing) trend of about −0.2 days/decade (1.0 days/decade). The decrease rate of 5‐day max precipitation is five times as large as 1‐day max precipitation. (d) For June‐September, the strengthened West Pacific Subtropical High intensity and the variation of its ridge‐axis position, the southerly shift of the upper subtropical Jetstream and the weakening of lower moisture supplement may have suppressed the northerly move of the summer rain band and delayed the development of rainy season over the study area. (e) In view of the urbanization effect, the possible causes of the precipitation externalization were investigated, and it was found that the upward trends in daily precipitation intensity and 95th percentile intense precipitation in big cities are generally higher than rural regions. Plain Language Summary: The investigation of variation in precipitation extreme events and its possible causes was conducted for the northern Korean Peninsula during 1961–2020. Annual total precipitation had experienced a significant decreasing trend, but extreme precipitation intensity had a clear upward trend, and extreme rainfall events became more frequent, with upward trends of 8.9 mm/decade for rainfall (>95th percentile) and 6.3 mm/decade for rainfall (>99th percentile) and a decreasing (increasing) trend of about −0.2 days/decade (1.0 days/decade) in continuous wet (dry) days. These changes were directly driven by changes in the atmospheric circulation factors for June–September, such as West Pacific Subtropical High, upper subtropical Jetstream, and lower moisture supplement. In some urbanized regions, an asymmetrical shift in the temporal variation of precipitation is seeable. In particular, the decadal trends in daily precipitation intensity and 95th percentile precipitation in the big city are generally higher (about 50% and 15%) than those in rural regions. Key Points: Annual precipitation manifested a decreased trend, but extreme precipitation events became more frequentDecreasing rainy season rainfall is related to variation in West Pacific Subtropical High, low layer moisture flux, and upper subtropical JetstreamAn asymmetrical shift in precipitation pattern over the cities due to the urbanization effect is more detectable than those related to the atmospheric circulation [ABSTRACT FROM AUTHOR]