首页> 外文会议>Conference on remote sensing of the atmosphere, clouds, and precipitation >Geographical and climatological characterization of aerosol optical depth distribution of MODIS in China
【24h】

Geographical and climatological characterization of aerosol optical depth distribution of MODIS in China

机译:MODIS气溶胶光学深度分布的地理和气候特征

获取原文

摘要

The Aihui-Tengchong Line or the internationally known "Hu Line" divides China into the east and west parts, based on differences in China's population, geography, climate and economy, all of which are closely associated with the aerosols over China. By using the aerosol optical depth (AOD) data of MODIS during years 2000-2010, the geographical and climatological distributions of aerosols over China are presented, and the 'Hu Line" is found also to describe a geographic division of aerosols over China: on the east part, the monthly AOD varies from the peak (>0.5) during March and June to the low of around 0.3 in November and December with an annual mean of about 0.45, mostly contributed by anthropogenic aerosols from the human activities; on the west part, the AOD is dominated by the naturally emitted aerosols with an annual mean of 0.25 changing between the high (about 0.3) in the period of April to July and the low (<0.2) from October to January. The positive and negative trends in annual AOD over 2000-2010 are respectively found in the regions on the east and west. Asian monsoon has a notable impact on the interannual variability of aerosols over the east region by modulating the atmospheric transport and precipitation washout. The interannual aerosol variations in the west are strongly influenced by dust emission sources in the deserts. The dust weather processes control the natural dust emissions. The maximal AOD of 0.3 in the west China could be brought by the frequent dust storm events.
机译:Aihui-Tengchong线或国际知名的“胡锦赛”将中国分成了中国进入东部和西部,基于中国人口,地理,气候和经济的差异,所有这些都与中国的气溶胶密切相关。通过使用2000 - 2010年多年来Modis的气溶胶光学深度(AOD)数据,提出了中国气溶胶的地理和气候学分布,“HU LINE”也被发现也可以描述中国气溶胶的地理分工:上东部,月度AOD在3月份和6月期间的峰值(> 0.5)变化到11月和12月的低于0.3的低于约0.45,大多是人类活动的人为气溶胶;在西方部分,AOD由自然发出的气溶胶主导,年度到7月至7月至7月与7月份的高(约0.3)之间的年平均值0.25,从10月到1月的低(<0.2)。积极和负面趋势2000 - 2010年的年度AOD分别在东部和西部的地区发现。通过调制大气运输和降水冲洗,亚洲季风对东部地区的气溶胶续变性的显着影响。西方的续航气溶胶变化受沙漠中的灰尘排放来源的强烈影响。灰尘天气过程控制自然粉尘排放。西部0.3的最大AOD可以通过频繁的尘埃风暴事件带来。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号