Method for Retrieval of the HDO/H2O Ratio Vertical Profile in the Atmosphere from Satellite Spectra Simultaneously Measured in Thermal and Near-IR Ranges

被引:4
|
作者
Zadvornykh, I., V [1 ]
Gribanov, K. G. [1 ]
Denisova, N. Yu [1 ,2 ]
Zakharov, V., I [1 ,2 ]
Imasu, R. [3 ]
机构
[1] Ural Fed Univ, Inst Nat Sci & Math, Ekaterinburg 620000, Russia
[2] Russian Acad Sci, Ural Branch, Krasovsky Inst Math & Mech, Ekaterinburg 620990, Russia
[3] Univ Tokyo, Atmosphere & Ocean Res Inst, Chiba 2778568, Japan
基金
俄罗斯科学基金会;
关键词
remote sensing; inverse problem; water vapor isotopologues; GOSAT-2; RADIATIVE-TRANSFER CODE; WATER-VAPOR; DELTA-D;
D O I
10.1134/S1024856021020123
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
An original method is suggested for solving the inverse problem of hyperspectral satellite sounding of the atmosphere for retrieving the HDO/H2O ratio vertical profile in the atmosphere with simultaneous inversion of thermal and near-IR spectra. A computational experiment was performed to retrieve the vertical profile of the relative content of the HDO isotopologue in atmospheric water vapor from high-resolution spectra simulated with parameters of the TANSO-FTS spectrometer onboard the GOSAT-2 satellite. The inverse problem was solved by the optimal estimation method with simultaneous inversion of thermal and near-IR spectra. The output data of the isotopic version of the ECHAM6-wiso atmospheric general circulation model were used as an a priori statistical set of water vapor isotopologue vertical profiles.
引用
收藏
页码:81 / 86
页数:6
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