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Titel The origin of summer monsoon rainfall at New Delhi by deuterium excess
VerfasserIn Hongxi Pang, Yuanqing He, Zhonglin Zhang, Aigang Lu, Juan Gu
Medientyp Artikel
Sprache Englisch
ISSN 1027-5606
Digitales Dokument URL
Erschienen In: Hydrology and Earth System Sciences ; 8, no. 1 ; Nr. 8, no. 1, S.115-118
Datensatznummer 250005391
Publikation (Nr.) Volltext-Dokument vorhandencopernicus.org/hess-8-115-2004.pdf
 
Zusammenfassung
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

 
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