Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/930
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dc.contributor.authorBhatt, B. C-
dc.contributor.authorMahra, H. S-
dc.date.accessioned2006-04-11T04:55:11Z-
dc.date.available2006-04-11T04:55:11Z-
dc.date.issued1987-
dc.identifier.citationBASI, Vol. 15, No. 2 & 3, pp. 116-120en
dc.identifier.urihttp://hdl.handle.net/2248/930-
dc.description.abstractPrecipitable water vapour is one of the variable atmospheric constituents and its short-term and seasonal variations may affect the infrared photometric observations. From the analysis of the measurements, made at Manora Peak, Naini Tal, 1981 November - 1983 December, of the total precipitable water vapour content in the atmosphere, the relative-humidity, and the temperature at ground level, it is concluded that the precipitable water vapour content is maximum during the months of May and June; and a minimum of 2.5 to 3.5 mm of precipitable water vapour content is observed during the winter observing season from November to March. The precipitable water vapour (mm) shows a poor correlation with the ground absolute humidity (gm/m/sup3/)en
dc.format.extent330955 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoenen
dc.publisherAstronomical Society of Indianen
dc.subjectAtmospheric precipitable water vapouren
dc.subjectSite testingen
dc.titleAtmospheric Precipitable Water Vapour Over Manora-Peak Naini-Talen
dc.typeArticleen
Appears in Collections:BASI Publications

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