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Spatiotemporal variation in the occurrence of sand-dust events and its influencing factors in the Beijing-Tianjin Sand Source Region, China, 1982-2013

机译:1982-2013年中国京津沙源地区沙尘事件发生时空变化及其影响因素

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The Beijing-Tianjin Sand Source Region (BTSSR) is an ecological barrier for Beijing, the capital of China. Exploration of the spatiotemporal patterns of sand-dust weather and their influencing factors is important for effective management of regional environments. Changes in patterns of sand-dust weather days from 1982 to 2013 were analyzed based on remote sensing and meteorological observation data, and the contributions of meteorological and vegetation factors to the variation in sand-dust events at the regional and sub-regional scales were investigated. The results showed that the number of sand-dust weather days in the BTSSR decreased with decreasing wind speed and variations in precipitation and vegetation restoration, from 24 in 1982 to 5 in 2013. The occurrence of sand-dust weather was related mainly to the mean wind speed during March and May, the cumulative precipitation from the antecedent July to the concurrent June, and the maximum vegetation cover of the antecedent year. These factors could explain 76.4% of the variation in sand-dust events, with meteorological factors, including wind speed and precipitation, contributing about 57%. The spatiotemporal patterns of sand-dust weather and their specific influencing factors were spatially heterogenous. In 70% of sub-regions, the influencing factors explained at least 50% of the variation in sand-dust events. Although meteorological factors dominated, the function of vegetation in the variation in sand-dust weather could not be ignored, with contributions of 26-48%. Existing eco-restoration projects (e.g., reforestation and afforestation, enclosure of grassland) should be effectively managed and protected to maintain vegetation and reduce the sand-dust event risk.
机译:京津沙源区(BTSSR)是中国首都北京的生态屏障。探索沙尘天气的时空格局及其影响因素对于有效管理区域环境具有重要意义。基于遥感和气象观测数据,分析了1982年至2013年沙尘天气日数的变化,并研究了气象和植被因素对区域和次区域尺度沙尘事件变化的贡献。 。结果表明,随着风速的减小以及降水量和植被恢复的变化,BTSSR沙尘天气的天数从1982年的24个减少到2013年的5个。沙尘天气的发生主要与平均值有关。 3月和5月的最大风速,7月以前到6月的累计降水量以及前一年的最大植被覆盖率。这些因素可以解释76.4%的沙尘事件变化,而气象因素(包括风速和降水)贡献了约57%。沙尘天气的时空格局及其具体影响因素在空间上是异质的。在70%的次区域中,影响因素至少解释了沙尘事件变化的50%。尽管气象因素占主导地位,但植被在沙尘天气变化中的作用不容忽视,贡献率为26-48%。应有效管理和保护现有的生态修复项目(例如重新造林和造林,围封草地),以维持植被并减少沙尘事件的风险。

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