The Investigation of Microwave Precipitation Measurement at 37GHz

Liu Jinli; Xiao Jianming; Zhang Ling

doi:10.1007/BF02919173

Impact Factor: 5.8

Volume 7 Issue 1

Jan. 1990

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1990 > 7(1): 104-110

The Investigation of Microwave Precipitation Measurement at 37GHz

1.
Institute of Atmospheric Physics, Academia Sinica, Beijing 100011,Institute of Atmospheric Physics, Academia Sinica, Beijing 100011,Institute of Atmospheric Physics, Academia Sinica, Beijing 100011

doi: 10.1007/BF02919173

Abstract
References
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Abstract:
In this paper we use a 10-layer radiation transfer model to systematically investigate the relation between brightness temperature and the rainfall rates at 37 GHz, including various viewing of microwave (MW) remote sens-ing and different surface condition, with main focus on the influence of the structure of ice-phase layer. The results show that the quantitative rainfall measurement can not be reliably obtained over the land from spaceborne radiometer at this wavelength and the structures of ice layer are very important in determining the “observed” bright-ness temperature for the spaceborne MW remote sensing.
References

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Manuscript History

Manuscript received: 10 January 1990

Manuscript revised: 10 January 1990

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

The Investigation of Microwave Precipitation Measurement at 37GHz

1. Institute of Atmospheric Physics, Academia Sinica, Beijing 100011,Institute of Atmospheric Physics, Academia Sinica, Beijing 100011,Institute of Atmospheric Physics, Academia Sinica, Beijing 100011

Manuscript received: 1990-01-10
Manuscript revised: 1990-01-10

Abstract: In this paper we use a 10-layer radiation transfer model to systematically investigate the relation between brightness temperature and the rainfall rates at 37 GHz, including various viewing of microwave (MW) remote sens-ing and different surface condition, with main focus on the influence of the structure of ice-phase layer. The results show that the quantitative rainfall measurement can not be reliably obtained over the land from spaceborne radiometer at this wavelength and the structures of ice layer are very important in determining the “observed” bright-ness temperature for the spaceborne MW remote sensing.