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DC Field | Value | Language |
---|---|---|
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 |
Appears in Collections: | BASI Publications |
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