大气与环境光学学报 ›› 2019, Vol. 14 ›› Issue (6): 442-454.

• 光学遥感 • 上一篇    下一篇

基于AIRS卫星的全球和东亚地区CO2时空特征分析

张绍会1,2, 谢冰1,3, 张华1,2,周喜讯2   

  1. 1 南京信息工程大学气象灾害预报预警与评估协同创新中心,江苏南京 210044;
    2 中国气象科学研究院灾害天气国家重点实验室,北京 100081;
    3 中国气象局气候研究开放实验室,中国气象局国家气候中心,北京 100081
  • 出版日期:2019-11-28 发布日期:2019-11-21

Spatial-Temporal Distribution Characteristics of CO2 over Globe and East Asia by AIRS Satellite

  • Published:2019-11-28 Online:2019-11-21

摘要: 利用2002年12月到2016年11月的大气红外探测仪(Atmospheric infrared sounder, AIRS)卫星观测资料,分析了全球
和东亚地区(70~140E, 10~55N)CO2浓度的时空变化和季节分布特征,并与地面观测
资料进行了对比。结果表明: 1) AIRS反演的CO2资料与地表观测资料相关系数均在0.9以上,且年均值相对误差均
在1%以内。2)全球CO2年平均浓度从2003年的375.16 ml/m3增加到2016年的401.24 ml/m3,
年平均增长率约2.01 ml/m3;同期,东亚地区CO2平均浓度从2003年的375.13 ml/m3增加
到2016年的402.22 ml/m3,年增长率约为2.08 ml/m3,高于全球的年平均增长率。
在2010~2016年,北半球大部分地区CO2浓度增长率低于2003~2009年的增长率。CO2增幅较明显
的区域位于北半球高纬度地区如中西伯利亚和格陵兰岛等地上空。3)CO2分布存在明显的区域性,高值区主要位于
北半球的中高纬度地区;低值区主要位于青藏高原上空。在南半球,CO2浓度的高值区主要位于南美洲中纬度地区;
低值区主要出现在低纬度(0~20S, 50W~5E)的大西洋上空。在对流层中低层(4~6 km),
AIRS反演的CO2浓度的季节变化特征准确性较高,特别在冬季,北半球大部分地区的CO2浓度随着时间
变化呈现先减小后增加的趋势。4)在东亚地区,CO2高值区位于中国北方地区,呈带状分布。

关键词: CO2浓度, AIRS, 东亚地区, 时空分布

Abstract: Based on atmospheric infrared sounder (AIRS ) satellite data from December 2002 to November 2016, 
the spatial-temporal characteristics of CO2 concentration in different seasons over globe and East 
Asia (70~140E, 10~55N) were analyzed and compared with the surface observation 
data. The results show that: 1) the correlation coefficient between the CO2  data of AIRS and the 
surface observation data is above 0.9, and the relative error of annual mean value is within 1%. 
2) The global annual mean CO2  concentration increased from 357.16 ml/m3 in 2003 
to 401.24 ml/m3 in 2016, with an average annual growth date of about 2.01 ml/m3
While it increased from 357.13 ml/m3 to 402.22 ml/m3 during the same 
period over East Asia, with an average annual growth rate of about 2.08 ml/m3 which is 
a bit higher than that of globe. Over most of the Northern Hemisphere,  the CO2  concentration 
growth rate during 2010~2016 is lower than that of during 2003~2009. In particular, 
mean CO2  concentration increased markedly over central Siberia and Greenland. 3) The distributions 
of CO2  concentrations had obviously regional features. The regions with high CO2  concentration 
were over middle and high latitudes in the Northern Hemisphere, whereas the regions wtih low CO2 
concentration were mainly located over Tibet Plateau. In the Southern Hemisphere, the regions with 
high concentration was located in the middle latitudes, while the region with low concentration was 
located in the low latitudes of Atlantic (0~20S, 50W~5E). 
In the middle and lower troposphere (4~6 km), the seasonal variation characteristics of CO2  
concentration retrieved by AIRS was highly reliable. Especially in winter, over most of the Northern 
Hemisphere, CO2  concentration decreased first and then increased with time. 4) In East Asia, 
the high CO2 concentration was located in the Northern China with zonal distribution. 

Key words: CO2 concentration, AIRS, East Asia, spatial-temporal distribution

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