Monitoring Asian Dust Storms from NOAA-20 CrIS Double CO2 Band Observations

被引:2
|
作者
Fang, Chenggege [1 ,2 ,3 ]
Han, Yang [2 ,3 ]
Weng, Fuzhong [2 ,3 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Key Lab Aerosol Cloud Precipitat, China Meteorol Adm, Nanjing 210044, Peoples R China
[2] China Meteorol Adm, CMA Earth Syst Modeling & Predict Ctr CEMC, Beijing 100081, Peoples R China
[3] China Meteorol Adm, State Key Lab Severe Weather, Chinese Acad Meteorol Sci, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
sand and dust storms; emission and scattering; hyperspectral infrared sounding; NUMERICAL WEATHER PREDICTION; RADIATIVE-TRANSFER; SATELLITE OBSERVATION; REFRACTIVE-INDEXES; CLIMATE;
D O I
10.3390/rs14184659
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Sand and dust storms (SDSs) are common environmental hazards in spring in Asian continent and have significant impacts on human health, weather, and climate. While many technologies have been developed to monitor SDSs, this study investigates the spectral characteristics of SDSs in satellite hyperspectral infrared observations and propose a new methodology to monitor the storms. An SDS emission and scattering index (SESI) is based on the differential responses of infrared CO2 shortwave and longwave IR bands to the scattering and emission of sand and dust particles. For a severe dust storm process during 14-17 March 2021, the SESI calculated by the Cross-track Infrared Sounder (CrIS) observations shows very negative values in the dusty region and is consistent with the spatial distribution of dust identified from the true-color RGB imagery and the dust RGB imagery of the Visible Infrared Imaging Radiometer Suite (VIIRS) on the NOAA-20 Satellite. The use of the SESI index in the near-surface layer allows for monitoring of the dust storm process and enables an effective classification between surface variations and dust weather events.
引用
收藏
页数:17
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