Spatial‐temporal characteristics of aerosol loading over the Yangtze River Basin during 2001–2015

Zhang Ming; Ma Yingying; Wang Lunche; Gong Wei; Hu Bo; Shi Yifan

摘要

ABSTRACT > The spatial‐temporal characteristics of aerosol loading over the Yangtze River Basin, China during 2001–2015 were investigated using moderate resolution imaging spectroradiometer (MODIS), multi‐angle imaging spectroradiometer (MISR), and ground‐level particulate matter (PM) data. Aerosol optical depth (AOD) >0.8 occurs in the Yangtze River Delta, central China, and the Sichuan Basin, while AOD <0.3 occurs over higher‐elevation areas in the western Sichuan Plateau and the source regions of the Yangtze River. The western Sichuan Plateau is characterized by fine‐mode natural aerosols, while the source region of the Yangtze River is more influenced by dust aerosols. The Sichuan Basin, central China, and the Yangtze River Delta are dominated by anthropogenic aerosols. The spatial distribution of ground‐level PM <sub>2.5</sub> and its ratio to PM <sub>10</sub> confirm the high aerosol loading and dominance of small particles over the middle and lower Yangtze Basin. Over the Yangtze River Delta, central China, and the Sichuan Basin, AOD varies seasonally from low in the cold months to high in the warm months, being suppressed by rainfall and wind during the Asian summer monsoon. Precipitation increases aerosol loading in the western Sichuan Plateau but reduces dust particles in the source region of the Yangtze River. There is no significant AOD trend over most areas of the Yangtze River Basin during 2001–2015, while strong decreasing trends are found over most of the middle and lower Yangtze Basin during 2011–2015. These decreasing trends may relate to changes in annual precipitation, wind speed, and air‐pollution control policies. The NO <sub>2</sub> and SO <sub>2</sub> emissions decreased by 16.51 and 23.40% over major provinces and cities of the </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><abstract xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”xml：lang =“en”> <title type =“main”>抽象</ title> >空间使用中度分辨率成像分光仪（MODIS），多角度成像光谱辐射器（MISR）和地面颗粒物（PM）数据，研究了2001 - 2015年长江盆地气溶胶加载的青蒿盆载荷。在中国中部和四川盆地和四川盆地中发生气溶胶光学深度（AOD）> 0.8，而Aod <0.3发生在四川省西部高原和长江源区的高度高度升高区域。西川西部的高原的特点是细模天然气溶胶，而长江的源区受到尘埃气溶胶的影响。中国中部四川盆地和长江三角洲都是由人为气溶胶的主导。地下PM <Sub> 2.5 </ sub>的空间分布及其与PM <sub> 10 </ sub>在中间和下部和下扬子盆地中的小颗粒的高气溶胶载荷和优势。在亚洲夏季季风期间，在寒冷的月份，AOD在寒冷的几个月中，寒冷的月份季节性低于寒冷的几个月，在寒冷的月份季节季节性态度差异。沉淀增加了四川高原的气溶胶载荷，但减少了长江源区的灰尘颗粒。在2001 - 2015年期间长江流域大部分地区没有显着的AOD趋势，而2011 - 2015年的大部分中间和下游盆地大部分趋势都存在强劲的下降趋势。这些减少趋势可能与年降水量，风速和空气污染控制政策的变化有关。没有<sub> 2 </ sub>，因此<sub> 2 </ sub>排放减少了16.51和23.40％，主要省份和城市 </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" > 著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-21026/'>《International Journal of Climatology: A Journal of the Royal Meteorological Society 》</a> <b style="margin: 0 2px;">|</b><span>2018年第4期</span><b style="margin: 0 2px;">|</b> <span>共15页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Ming&option=202" target="_blank" rel="nofollow">Zhang Ming;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ma Yingying&option=202" target="_blank" rel="nofollow">Ma Yingying;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Lunche&option=202" target="_blank" rel="nofollow">Wang Lunche;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gong Wei&option=202" target="_blank" rel="nofollow">Gong Wei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hu Bo&option=202" target="_blank" rel="nofollow">Hu Bo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shi Yifan&option=202" target="_blank" rel="nofollow">Shi Yifan;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>State Key Laboratory of Information Engineering in Surveying Mapping and Remote SensingWuhan UniversityChina;</p> <p>State Key Laboratory of Information Engineering in Surveying Mapping and Remote SensingWuhan UniversityChina;</p> <p>Laboratory of Critical Zone Evolution School of Earth SciencesChina University of GeosciencesWuhan China;</p> <p>State Key Laboratory of Information Engineering in Surveying Mapping and Remote SensingWuhan UniversityChina;</p> <p>State Key of Laboratory of Atmospheric Boundary Physics and Atmospheric ChemistryInstitute of Atmospheric Physics Chinese Academy of SciencesBeijing China;</p> <p>State Key Laboratory of Information Engineering in Surveying Mapping and Remote SensingWuhan UniversityChina;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li> <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span> <a href="https://www.zhangqiaokeyan.com/clc/1232.html" title="气候学">气候学 ;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=aerosol optical depth&option=203" rel="nofollow">aerosol optical depth;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=?ngstr?m exponent&option=203" rel="nofollow">?ngstr?m exponent;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yangtze River Basin&option=203" rel="nofollow">Yangtze River Basin;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=MODIS&option=203" rel="nofollow">MODIS;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=PM 2.5&option=203" rel="nofollow">PM 2.5;</a> </p> <div class="translation"> 机译：气溶胶光学深度;？NGSTR？M指数;长江流域;MODIS;PM 2.5; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div 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