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科技导报  2015 

卫星遥感监测全球和中国区域大气CO变化特征

DOI: 10.3981/j.issn.1000-7857.2015.17.005, PP. 52-62

Keywords: 卫星遥感,MOPITT,CO柱总量

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Abstract:

利用2000年3月——2014年12月TERRA/MOPITTCO柱总量数据,研究了全球及中国区域大气CO柱总量的时空变化特征。分析表明,北半球大气CO柱总量显著高于南半球。中国东部是全球CO高值区,青藏高原、格陵兰岛、南美洲西部沿海安第斯山脉为全球CO低值区。CO柱总量在全球范围内表现出显著的季节变化,北半球CO含量在北半球春季最高,北半球冬季达到最低;南半球CO含量在南半球春季最高,南半球秋季达到最低。在月时间尺度上呈现出规律性波动,高值月份分别出现在3—4月、9—10月,低值时段分别出现在7月和1月。中国区域CO柱总量呈东高西低的阶梯状分布,东部的高值区主要分布在河北南部、山东西部、河南东部。中国区域CO柱总量在春季最高,南方地区在夏季达到最低值;北方地区在秋季达到最低值。对全球和中国区域CO含量长时间序列分析显示,2011—2014最近4年全球及中国区域大气CO柱总量呈下降趋势。中国东部沿海经济区和南部沿海经济区的年下降速率在1%左右,大西北经济区下降幅度最小。

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