Atmospheric Precipitable Water Vapour Over Manora-Peak Naini-Tal

dc.contributor.author	Bhatt, B. C
dc.contributor.author	Mahra, H. S
dc.date.accessioned	2006-04-11T04:55:11Z
dc.date.available	2006-04-11T04:55:11Z
dc.date.issued	1987
dc.identifier.citation	BASI, Vol. 15, No. 2 & 3, pp. 116-120	en
dc.identifier.uri	http://hdl.handle.net/2248/930
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 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.extent	330955 bytes
dc.format.mimetype	application/pdf
dc.language.iso	en	en
dc.publisher	Astronomical Society of Indian	en
dc.subject	Atmospheric precipitable water vapour	en
dc.subject	Site testing	en
dc.title	Atmospheric Precipitable Water Vapour Over Manora-Peak Naini-Tal	en
dc.type	Article	en