Geostationary Hyperspectral Infrared Sounder Channel Selection for Capturing Fast-Changing Atmospheric Information

被引:13
|
作者
Di, Di [1 ]
Li, Jun [2 ]
Han, Wei [3 ,4 ]
Yin, Ruoying [3 ,4 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Sch Atmospher Phys, Nanjing 210044, Peoples R China
[2] Univ Wisconsin, Cooperat Inst Meteorol Satellite Studies, Madison, WI 53706 USA
[3] China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China
[4] China Meteorol Adm, Numer Weather Predict Ctr, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
Atmospheric measurements; Hyperspectral imaging; Jacobian matrices; Temperature measurement; Information entropy; Covariance matrices; Atmospheric modeling; Channel selection; geostationary satellite; hyperspectral infrared (IR) sounder; RADIATIVE-TRANSFER MODEL; SPECTRAL-RESOLUTION; ASSIMILATION; SOUNDINGS; RADIANCE;
D O I
10.1109/TGRS.2021.3078829
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Various methodologies have been developed for selecting a subset of channels from a hyperspectral infrared (IR) sounder for assimilation. The information entropy iterative method was considered optimal for channel selection. However, this method only considers the decrease in uncertainty in the atmospheric state caused by measurements at a single time, without considering the dynamic effect of measurements over a period of time; therefore, it might not be optimal for hyperspectral IR sounders onboard geosynchronous satellites that mainly aim to observe rapidly changing weather events. An alternative channel selection method is developed by adding an M index, which reflects the Jacobian variance over time; the adjusted algorithm is ideal for the Geosynchronous Interferometric Infrared Sounder (GIIRS), which is the first high-spectral-resolution advanced IR sounder onboard a geostationary weather satellite. Comparisons between the conventional algorithm (information entropy iterative method) and the adjusted algorithm show that the channels selected from GIIRS by the adjusted algorithm will have larger brightness temperature diurnal variations and better information content than the conventional algorithm, based on the same background error covariance matrix, the observational error covariance matrix, and the channel blacklist. The adjusted algorithm is able to select the channels for monitoring atmospheric temporal variation while retaining the information content from the conventional method. The 1-D variational (1Dvar) retrieval experiment also verifies the superiority of this adjusted algorithm; it indicates that using the channel selected by the adjusted algorithm could enhance the water vapor profile retrieval accuracy, especially for the lower and middle troposphere atmosphere.
引用
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页数:10
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