EXPERIMENTAL INVESTIGATION ON REAL-TIME REMOTE SENSING OF LAYERED ATMOSPHERIC PRECIPITABLE BY A GROUND-BASED RADIOMETER OF 1.35 cm WAVELENGTH

Huang Runkeng; Wei Chong

doi:10.1007/BF02680047

Impact Factor: 3.9

Volume 3 Issue 1

Jan. 1986

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1986 > 3(1): 86-93

EXPERIMENTAL INVESTIGATION ON REAL-TIME REMOTE SENSING OF LAYERED ATMOSPHERIC PRECIPITABLE BY A GROUND-BASED RADIOMETER OF 1.35 cm WAVELENGTH

1.
Institute of Atmospheric Physics, Academia Sinici, Beijing,Institute of Atmospheric Physics, Academia Sinici, Beijing

doi: 10.1007/BF02680047

Abstract
References
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Abstract:
The principle and technique of real-time remote sensing of the layered atmospheric precipitable by using a ground-based radiometer of 1.35 cm wavelength with a microcomputer as a controlling and data process-ing unit are presented. The stability and calibration of the instrument are outlined. Observations during the summer of 1984 show that the RMS deviation of the layered precipitable between the radiometer meas-urement and the radiosonde ranges from 0.20 to 0.25 g/cm2 with a correlation coefficient of above 90 %.
References

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[2]	Lin Hai, Xin Miaoxin, Wei Chong, Hao Yaokui, Zou Shouxiang, 1985: GROUND-BASED REMOTE SENSING OF LWC IN CLOUD AND RAINFALL BY A COMBINED DUAL-WAVELENGTH RADAR-RADIOMETER SYSTEM, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 93-103. doi: 10.1007/BF03179741
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Manuscript History

Manuscript received: 10 January 1986

Manuscript revised: 10 January 1986

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

EXPERIMENTAL INVESTIGATION ON REAL-TIME REMOTE SENSING OF LAYERED ATMOSPHERIC PRECIPITABLE BY A GROUND-BASED RADIOMETER OF 1.35 cm WAVELENGTH

1. Institute of Atmospheric Physics, Academia Sinici, Beijing,Institute of Atmospheric Physics, Academia Sinici, Beijing

Manuscript received: 1986-01-10
Manuscript revised: 1986-01-10

Abstract: The principle and technique of real-time remote sensing of the layered atmospheric precipitable by using a ground-based radiometer of 1.35 cm wavelength with a microcomputer as a controlling and data process-ing unit are presented. The stability and calibration of the instrument are outlined. Observations during the summer of 1984 show that the RMS deviation of the layered precipitable between the radiometer meas-urement and the radiosonde ranges from 0.20 to 0.25 g/cm2 with a correlation coefficient of above 90 %.