The origin of summer monsoon rainfall at New Delhi by deuterium excess
The deuterium excess in summer monsoon precipitation, determined from isotopic measurements(δ<sup>18</sup>O 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. Furthermor...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2004-01-01
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Series: | Hydrology and Earth System Sciences |
Online Access: | http://www.hydrol-earth-syst-sci.net/8/115/2004/hess-8-115-2004.pdf |