Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3109
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dc.contributor.authorRao, M. S.-
dc.contributor.authorKrishan, Gopal-
dc.contributor.authorKumar, Bhishm-
dc.contributor.authorAnitha, M.-
dc.contributor.authorKumar, B. Kiran-
dc.contributor.authorNagabhushanam, P.-
dc.date.accessioned2019-07-16T12:00:33Z-
dc.date.available2019-07-16T12:00:33Z-
dc.date.issued2012-
dc.identifier.citationInternational Journal of Earth Sciences and Engineering, ISSN 0974-5904, Volume 05, No. 05 October 2012, P.P. 1123-1128en_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3109-
dc.description.abstractStable isotopes (δ18O and δD) of ground level atmospheric vapour (GLV) are used to identify long range spatial correlation in moisture variability between two geo-graphically and geo-climatically different places Roorkee in the foot hills of Siwaliks in the north western part of the Gangetic plains and Hyderabad in the Deccan Plateau of peninsular India. A very good isotopic correlation in atmospheric moisture and absolute humidity was observed during 2008-10 in southern and northern part of India due to common (Arabian Sea and Bay of Bengal) dominant moisture source to both the regions but their magnitude in the total moisture and time of onset and duration is different in both the regions. These components and their timings are also changing in the recent years. In southern India, these are appearing early while are getting delayed in northern India. The results on long range correlation in GLV help understanding monsoon dynamics and climate change.en_US
dc.language.isoenen_US
dc.publisherCafet Innovaen_US
dc.subjectStable Isotopesen_US
dc.subjectAtmospheric Vapouren_US
dc.subjectMonsoon Dynamicsen_US
dc.subjectArabian Seaen_US
dc.subjectBay of Bengalen_US
dc.subjectIWINen_US
dc.titleStable Isotope Systematics of Atmospheric Vapour at Hyderabad and Roorkeeen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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