Measurement of Martian atmospheric winds by the O2 1.27 μm airglow observations using Doppler Michelson Interferometry: A concept study

被引:3
作者
Yang, Na [1 ]
Xia, Chunliang [1 ]
Yu, Tao [1 ]
Zuo, Xiaomin [1 ]
Sun, Yangyi [1 ]
Yan, Xiangxiang [1 ]
Zhang, Jian [1 ]
Wang, Jin [1 ]
Le, Huijun [2 ,3 ,4 ,5 ]
Liu, Libo [2 ,3 ,4 ,5 ]
Ward, William Edmund [6 ]
机构
[1] China Univ Geosci, Inst Geophys & Geomat, Hubei Subsurface Multiscale Imaging Key Lab, Wuhan 430074, Peoples R China
[2] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
[3] Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
[4] Chinese Acad Sci, Inst Geol & Geophys, Mohe Observ Geophys, Beijing 100029, Peoples R China
[5] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[6] Univ New Brunswick, Dept Phys, Fredericton, NB E3B 5A3, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Martian atmospheric wind; Doppler Michelson interferometer; 1.27 mu m airglow; ULTRAVIOLET SPECTROMETER; IMAGING INTERFEROMETER; INFRARED-SPECTROSCOPY; SATELLITE MEASUREMENT; STRATOSPHERIC WINDS; GRAVITY-WAVES; MARS; EMISSION; OZONE; TEMPERATURE;
D O I
10.1007/s11430-020-9814-7
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
China's Mars exploration mission has stimulated tremendous interest in planetary science exploration recently. To propose potential scientific research projects, this study presents a concept simulation for the measurement of Martian atmospheric winds using the Doppler Michelson interferometry technique. The simulation is based on the satellite instrument initially designed for the Dynamic Atmosphere Mars Observer (DYNAMO) project to measure vertical profiles of winds from the 1.27 mu m airglow observations in the Martian atmosphere. A comprehensive DYNAMO measurement simulation forward model based on an orbit submodel, an atmospheric background field submodel, and an instrument submodel is developed using the Michelson equation. The simulated interferogram signal over the field of view (FOV) calculated by the forward model is associated with the filter transmittance function, column emission rate of airglow, wind velocity, temperature, and the Michelson phase. The agreement between the derived atmospheric signals from the simulated interferogram without altitude inversion and the input parameters used to initiate the forward model confirms the validity of the forward model.
引用
收藏
页码:2027 / 2042
页数:16
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