Preprint Article Version 1 Preserved in Portico This version is not peer-reviewed

Analysis of the Contribution of Water Vapor from the Arabian Sea to the Local Rainstorm Process in Southern Xinjiang

Version 1 : Received: 31 October 2020 / Approved: 2 November 2020 / Online: 2 November 2020 (16:20:31 CET)

How to cite: Bao, D.; Zheng, Z.; Gao, H.; Emer, M. Analysis of the Contribution of Water Vapor from the Arabian Sea to the Local Rainstorm Process in Southern Xinjiang. Preprints 2020, 2020110063 (doi: 10.20944/preprints202011.0063.v1). Bao, D.; Zheng, Z.; Gao, H.; Emer, M. Analysis of the Contribution of Water Vapor from the Arabian Sea to the Local Rainstorm Process in Southern Xinjiang. Preprints 2020, 2020110063 (doi: 10.20944/preprints202011.0063.v1).

Abstract

Based on NCEP FNL 1°*1° analysis data and Xinjiang meteorological bureau area numerical operation prediction, a local precipitation event in southern Xinjiang on June 26 was analyzed, and the results showed that the water vapor involved in this process originated from the northwestern Gangetic Plain and was transported along the Indus River plain and over the northwestern end of the mountains. Driven by the Iranian low-pressure trough, water vapor at 500 hPa was transported across the northwestern end of the Gangdise Mountains, past Georgoli Peak, and northwest over the Kunlun Mountains to arrive in southern Xinjiang.

Subject Areas

water vapor; local rainstorm; southern Xinjiang; Arabian Sea.

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