Atmospheric precipitable water vapour over Manora Peak, Naini Tal

dc.contributor.author	Bhatt, B. C.
dc.contributor.author	Mahra, H. S.
dc.date.accessioned	2010-02-19T08:58:33Z
dc.date.available	2010-02-19T08:58:33Z
dc.date.issued	1987
dc.identifier.citation	This article is downloaded for ADS	en_US
dc.identifier.uri	http://hdl.handle.net/123456789/559
dc.description.abstract	Precipitable 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 watervapour 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 form November to March. The precipitable water vapour (mm) shows a poor correlation with the ground absolute humidity (gm/m³)	en_US
dc.language.iso	en_US	en_US
dc.relation.ispartofseries	basi15-116
dc.subject	Water vapour	en_US
dc.title	Atmospheric precipitable water vapour over Manora Peak, Naini Tal	en_US
dc.type	Article	en_US