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Interannual variation of the East Asia Jet Stream and its impact on the horizontal distribution of aerosol in boreal spring

机译:东亚急流的年际变化及其对北方春季气溶胶水平分布的影响

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摘要

Interannual variation of the aerosol optical depth (AOD) in East Asia has been investigated using Moderate Resolution Imaging Spectroradiometer (MODIS) data and Modern Era Retrospective analysis for Research and Applications Version 2 (MERRA-2) data for 2000-2018. The data analysis focuses on boreal spring when Siberian biomass burning is at its seasonal maximum. The results indicate that the significant increase in organic and black carbon is primarily caused by emissions from biomass burning in East Asia, which leads to significant interannual variations in aerosol loading and pan-Pacific transport. The anomalous large-scale climate variability associated with the East Asia Jet Stream (EAJS) provides favorable conditions for increasing the AOD of organic and black carbon in Northeast Asia and may represent an underlying physical mechanism. When the EAJS shows greater weakening than normal, abnormal high-pressure anomalies are maintained in East Asia, which tend to drive warm advection over Northeast Asia. This warm advection expedites the melting of the Eurasian snow cover, which helps increase surface dryness in late spring and provides favorable conditions for biomass burning. The EAJS index can be predictable with statistical significance up to lead 1 month by the dynamical ensemble seasonal forecasts, suggesting a possible implementation of the empirical AOD forecasts using climate forecast models.
机译:使用中分辨率成像光谱仪(MODIS)数据和2000-2018年研究和应用版本2(MERRA-2)数据的现代时代回顾性分析,研究了东亚气溶胶光学深度(AOD)的年际变化。数据分析的重点是西伯利亚生物量燃烧达到季节最大值时的寒冬。结果表明,有机碳和黑碳的显着增加主要是由东亚生物质燃烧产生的排放引起的,这导致了气溶胶负荷和泛太平洋运输的年际变化。与东亚急流(EAJS)相关的大规模气候异常变化为东北亚有机碳和黑碳的AOD增加提供了有利条件,并且可能代表了潜在的物理机制。当EAJS表现出比正常更大的减弱时,东亚将维持异常高压异常,这往往会推动东北亚上空的热对流。这种暖平流加速了欧亚积雪的融化,这有助于增加春末的表面干燥度,并为生物质燃烧提供了有利条件。 EAJS指数可以通过动态整体季节预报在长达1个月之前具有统计显着性,这表明可以使用气候预报模型实施经验性AOD预报。

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