高分五号大气痕量气体差分吸收光谱仪观测数据的火山喷发SO_(2)总量反演  

Volcanic SO_(2) retrieved from GF-5 Environmental trace gas Monitoring Instrument

作　　者：闫欢欢 王后茂 王维和[1] 张兴赢[1] YAN Huanhuan;WANG Houmao;WANG Weihe;ZHANG Xingying(Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites,National Satellite Meteorological Center,China Meteorological Administration,Beijing 100081,China;National Space Science Center,Chinese Academy of Sciences,Beijing 100190,China)

机构地区：[1]国家卫星气象中心中国气象局中国遥感卫星辐射测量和定标重点开放实验室,北京100081 [2]中国科学院国家空间科学中心,北京100190

出　　处：《遥感学报》2021年第11期2326-2338,共13页NATIONAL REMOTE SENSING BULLETIN

基　　金：国家重点研发计划(编号:2019YFC0214603);高分辨率对地观测系统重大项目(编号:05-Y20A16-9001-15);许建民气象卫星创新中心。

摘　　要：火山喷发产生的高浓度SO_(2)气体及其远距离输送会对全球气候变化和航空飞行安全产生重要影响。卫星遥感技术以大面积连续观测、高时空分辨率等优势成为大气SO_(2)监测的重要手段之一。作为中国第一颗紫外可见光波段的高光谱载荷,高分五号卫星大气痕量气体差分吸收光谱仪(GF-5 EMI)通过探测地球大气或表面反射、散射的紫外辐射来解析SO_(2)总量的分布和变化。本文首先基于大气辐射传输模型SCIATRAN,选择中低纬地区地表类型均一的海洋区域像元,模拟了典型大气条件下的晴空天顶反照率,用以评价EMI载荷天顶观测光谱的精度。其次,基于TROPOMI L1 Radiance辐亮度数据和DOAS反演原理,经477 nm O_(4)云筛选、光谱定标、慢变剔除、斜柱转垂直柱等步骤后,获得同一火山喷发区域的SO_(2)总量反演结果并与TROPOMI官方offline L2 SO_(2)产品进行对比分析。最后,利用GF-5 EMI UV-2通道观测数据,采用DOAS算法反演获得GF-5 EMI大气SO_(2)总量,并将反演结果与国际同类载荷S5P/TROPOMI SO_(2)总量结果进行比较分析,评判GF-5 EMI在全球火山活动SO_(2)变化监测方面的能力。结果显示,300—400 nm波段范围内,海洋区域采样点EMI观测光谱值低于SCIATRAN模拟光谱值,EMI与TROPOMI观测光谱呈现出相似的系统性偏差。基于高空间高光谱分辨率的TROPOMI L1 Radiance辐亮度数据、315—327 nm、325—335 nm和360—390 nm共3个波段窗口、以及上述DOAS反演原理获得的SO_(2)结果与TROPOMI官方发布的offline L2 SO_(2)产品结果相关性较高,两者的相关系数可达到0.97—0.99,相对偏差在3%—9%。GF-5 EMI能够获取火山喷发SO_(2)排放的时空分布特征,并与国际同类载荷TROPOMI反演结果具有较高的空间一致性,能够满足全球火山喷发监测、预警及其气候影响研究的应用需求。Sulfur dioxide(SO_(2))from volcanic eruption and its long-distance transportation has a significant impact on global climate change and aviation safety.Satellite remote sensing technology provides an unprecedented advantage for continuous,large spatial and shortrevisit monitoring for atmospheric SO_(2).GF-5 Environmental trace gas Monitoring Instrument(EMI)with high spatial resolution is the China’s first instrument of hyper spectral measurements with wavelength range from 240 nm to 710 nm,and makes daily global observations of key atmospheric constituents,including ozone,nitrogen dioxide,sulfur dioxide.In this paper,based on the atmospheric radiation transfer model SCIATRAN,the clear sky albedo under typical atmospheric conditions is simulated by selecting the ocean area pixels with uniform surface types in the middle and low latitudes to evaluate the accuracy of the EMI Top-of-Atmosphere(TOA)albedo.Secondly,based on the S5P/TROPOMI L1 Radiance data and the DOAS algorithm,after 477 nm O_(4) cloud screening,spectral calibration,slant column to vertical column conversion,the inversion results of total SO_(2)columns over volcanic eruption areas were obtained and compared with TROPOMI offline L2 SO_(2)products.Finally,GF-5/EMI SO_(2)columns were retrieved by using GF-5 EMI UV-2 band observations and DOAS algorithm,and then the retrieved GF-5/EMI SO_(2)columns were compared with similar S5 P/TROPOMI SO_(2)columns to evaluate the ability of GF-5/EMI on monitoring global SO_(2)change from volcanic activity.Results show that,in the band range of 300—400 nm,the EMI spectra of the sampling points in the ocean area are lower than the simulated spectra of SCIATRAN,and EMI and TROPOMI spectra show similar systematic biases.SO_(2)obtained by using TROPOMI L1 Radiance data,three band windows of 315—327 nm,325—335 nm and 360—390 nm,and DOAS inversion algorithm are compared with the TROPOMI offline L2 SO_(2)products,which show high correlations(correlation coefficient between 0.97—0.99,relative deviation between 3%an

关 键 词：遥感 GF-5 EMI 火山 SO_(2)总量 DOAS TROPOMI 

分 类 号：P237[天文地球—摄影测量与遥感]