

Author: Hantel Michael
Publisher: E. Schweizerbart'sche Verlagsbuchhandlung
ISSN: 0941-2948
Source: Meteorologische Zeitschrift, Vol.11, Iss.6, 2002-11, pp. : 415-417
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Abstract
When the global precipitation increases the precipitable water decreases and vice versa. Here we study the impact of a harmonic precipitation fluctuation (with zero time mean and constant global evaporation) on the precipitable water; fluctuations of the precipitable water imply fluctuations of global surface pressure. The relation between the amplitudes of the forcing and the response is frequency dependent. A global 27 day surface pressure fluctuation with amplitude of 0.1 hPa, as suggested by the IGY data, could be explained by a precipitation fluctuation with the same frequency and an amplitude of about 0.25 mm/day; the precipitation wave would lead the surface pressure wave by about 7 days. These estimates are consistent with, although they do not prove the reality of, the
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