Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3088
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dc.contributor.authorKrishan, Gopal-
dc.contributor.authorRao, M. S.-
dc.contributor.authorKumar, C. P.-
dc.contributor.authorKumar, Bhishm-
dc.date.accessioned2019-07-11T12:20:55Z-
dc.date.available2019-07-11T12:20:55Z-
dc.date.issued2014-
dc.identifier.citationJ Earth Sci Clim Change 2014, 5:2en_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3088-
dc.description.abstractAir moisture samples were collected from 2 stations of north India for the years 2012 and 2013: one located in high Himalayas inMarhi, Manali, Himachal Pradesh and second in Indo-gangetic plains of Roorkee, Uttarakhand using condensation method for studying seasonal variations in isotopic composition. In high Himalayas, the air moisture was found isotopically more enriched (δD) as compared to the moisture collected in Indo-gangetic plains. But due to the arrival of oceanic vaporduring the monsoon season, the isotopic values start getting depleted whichopens up the possibility to use isotopic composition of air moisture for seasonal studies.en_US
dc.language.isoenen_US
dc.publisherOMICSen_US
dc.subjectAir moistureen_US
dc.subjectStable isotopesen_US
dc.subjectHimalayasen_US
dc.subjectIndo-gangetic plainsen_US
dc.subjectGeographical effectsen_US
dc.titleIsotopic Observations from Two Stations of North India to Investigate Geographical Effects on Seasonal Air Moistureen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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