Titlebook: Variations in the Global Water Budget; Alayne Street-Perrott,Max Beran,Robert Ratcliffe Book 1983 D. Reidel Publishing Company, Dordrecht,

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Evaporation Models in the Global Water Budgetof water bodies, in terms of our ability to monitor its variation in time and over the surface of the globe. Attempts to introduce evaporation into the water budget as an independent term depends on our ability to model the process. This paper presents a classification scheme for such models which h

Pepsin

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Plant and Soil Water Storage in Arctic And Boreal Forest Ecosystemsnic matter above and below ground. The total water content of the biomass and seasonally-thawed layer of the Arctic and boreal forest was estimated to be 5700 Gt, most of which is stored in trees, peatlands, and that uppermost layer of the soil subject to seasonal thawing. The water held in the orga

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Recent Fluctuations of Alpine Glaciers and Their Meteorological Causes: 1880–1980cier mass balance are used here to give a climatic explanation for glacier fluctuations. In this way, it is possible to clarify the relationship between net mass balance and climate, to investigate the reaction of glaciers to changes in the rate of accumulation and to provide information on the clim

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Radiometric Chronology of Some Himalayan Glaciersusing the radionuclides .Si and .Pb. The ages of the snout ice of these three glaciers are about 500, 200 and 100 years, respectively. The bulk flow rates over the past few centuries on Nehnar, Gara and Changme Khangpu (CK) Glaciers are calculated as 6, 20 and 40 m yr., respectively. As expected, th

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Introduction to Techniques of Measurement And Analysis: Atmospheric Processesudget and their variations. The contributions in this section examine in detail the sources, transports and sinks of atmospheric water vapour, with particular emphasis on new techniques of measurement and analysis.

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The Atmospheric Water Vapour Budget Over Europeed between the annual mean values of ∇·. and E-P. However, E-P reaches a maximum around May, whereas (∂W/∂t) + ∇·. is at its highest value two months later. As this time lag occurs in all the study areas, it seems to be of a systematic nature.

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Comparison of Water Vapour Data from Monex-79 and the , Satellite in latitude and longitude, and the temporal separation between measurements that were compared being restricted to not more than 5 hours. The analysis demonstrated an excellent agreement between the satellite-derived and directly-measured data, with correlation coefficients of + 0.98 in both cases.

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