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The Origin of Summer Monsoon Rainfall at New Delhi by Deuterium Excess : Volume 8, Issue 1 (30/11/-0001)

By Pang, Hongxi

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Book Id: WPLBN0003988848
Format Type: PDF Article :
File Size: Pages 4
Reproduction Date: 2015

Title: The Origin of Summer Monsoon Rainfall at New Delhi by Deuterium Excess : Volume 8, Issue 1 (30/11/-0001)  
Author: Pang, Hongxi
Volume: Vol. 8, Issue 1
Language: English
Subject: Science, Hydrology, Earth
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Historic
Publication Date:
-0001
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Zhang, Z., Lu, A., He, Y., Gu, J., & Pang, H. (-0001). The Origin of Summer Monsoon Rainfall at New Delhi by Deuterium Excess : Volume 8, Issue 1 (30/11/-0001). Retrieved from http://hawaiilibrary.net/


Description
Description: Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou 730000, China. The deuterium excess in summer monsoon precipitation, determined from isotopic measurements(δ18O and <δD) at New Delhi, has been shown to be correlated, negatively, with relative humidity at the 1000 hPa level over the western Arabian Sea. Furthermore, summer rainfall in north-western India is correlated, positively, with the zonal wind speed at the 1000 hPa level over the western Arabian Sea, while relative humidity is correlated, negatively, with zonal wind speed at the same level. It is concluded that evaporation from the western Arabian Sea is a major source of the summer rainfall at New Delhi.

Keywords: deuterium excess, relative humidity, origin of precipitation

Summary
The origin of summer monsoon rainfall at New Delhi by deuterium excess

 

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