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2005~2017年全球大气边界层SO2时空变化
引用本文:康重阳,赵军,宋国富.2005~2017年全球大气边界层SO2时空变化[J].中国环境科学,2019,39(10):4033-4042.
作者姓名:康重阳  赵军  宋国富
作者单位:1. 西北师范大学地理与环境学院, 甘肃 兰州 730070; 2. 陇东学院历史与地理学院, 甘肃 庆阳 745000; 3. 西藏自治区生态环境遥感监测中心, 西藏 拉萨 850000
摘    要:使用2005~2017年遥感数据研究了全球大气边界层SO2时空分布特征及变化趋势.结果表明:空间分布上SO2呈现空间异质性,大气高SO2柱量值集中在以火山喷发为代表的自然源区域和以工业排放为代表的人为源及附近区域;一、二、三级SO2柱量值在全球范围内整体呈现纬度地带性分布特征,北半球受人为影响较为明显,分界线在陆地区域向南凸出,海洋上向北凹陷,而南半球受人为影响较小,分界线呈现与纬线平行趋势;2005~2017年全球大气边界层SO2单元栅格年均值整体呈现先增后减趋势,火山喷发导致2008、2009、2011年夏季出现了明显的波动,其余季节无显著变化;全球范围内大气边界层SO2年内变化,伴随太阳直射点南北移动,2005~2014年一级SO2柱量值延纬向对称轴的纬度,除10~12月份外,其余月份与对应月15日太阳赤纬基本吻合.

关 键 词:全球大气边界层  OMI  OMPS  SO2  
收稿时间:2019-03-10

Temporal and spatial distribution characteristics of global atmospheric boundary layer SO2 based on remote sensing data from 2005 to 2017
KANG Chong-yang,ZHAO Jun,SONG Guo-fu.Temporal and spatial distribution characteristics of global atmospheric boundary layer SO2 based on remote sensing data from 2005 to 2017[J].China Environmental Science,2019,39(10):4033-4042.
Authors:KANG Chong-yang  ZHAO Jun  SONG Guo-fu
Institution:1. College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China; 2. History and Geography Department, Long Dong College, Qingyang, 745000, China; 3. Tibet Autonomous Region Remote Sensing Monitoring Center, Lhasa 850000, China
Abstract:As the main precursor of the smog and acid rain in the atmosphere, SO2 plays an important role to the near-surface O3 pollution. Meanwhile, SO2 also affects the global and local atmospheric circulations because its strong absorption on the ultraviolet influences the solar radiation dramatically. Therefore, it is beneficial to study the temporal and spatial distributions of SO2 and their variations. In this paper, the spatial and temporal distributing features of SO2 at global atmospheric boundary layer were studied by the remote sensing data from 2005 to 2017. A spatial heterogeneity was observed from the analyzing results. Specifically, the high columns of SO2mainly concentrated on the volcanic eruption areas as a natural source and on the industrial emission areas as an anthropogenic source. The first, second and third grades of SO2 columns distributed zonally in the whole world. It was evidently affected by the human emissions in the Northern Hemisphere that the boundary line of SO2 column grades protruded southward on the land and sunk northward on the ocean. In the Southern Hemisphere, on the contrary, the boundary line paralleled to the latitude. From 2005 to 2017, the annual average of SO2 unit grid values at the global atmospheric boundary layer was increasing before 2011 and then decreasing. During this period of time, the volcanic eruptions led to obvious variations in the summer of 2008, 2009 and 2011. The alteration of SO2 at the atmospheric boundary layer was associated with the movement of the direct solar radiation point within each year. From 2005 to 2014, the latitudinal axis of symmetry of the first grade SO2 columns matched with the 15th day's solar declination of each month, except October, November, and December.
Keywords:global atmospheric boundary layer  OMI  OMPS  SO2  
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