Atmospheric Precipitable Water Vapour Over Manora-Peak Naini-Tal

Details Atmospheric Precipitable Water Vapour Over Manora-Peak Naini-Tal Atmospheric Precipitable Water Vapour Over Manora-Peak Naini-Tal

Jun 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987basi...15..116b&link_type=abstract

Bulletin of the Astronomical Society of India V.15:2, P. 116, 1987

Astronomy and Astrophysics

Astronomy

2

Scientific paper

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/m3).

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