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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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The Atmospheric Water Vapour Budget Over Europeage (∂W/∂t) have been computed using aerological observations for Europe. Long-term averages for precipitation P, evapotranspiration E and runoff R are used together with the atmospheric data to elucidate the mean annual and monthly water vapour budget for Europe..Relatively good agreement is obtain
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Atmospheric Water Distributions Determined by the , Multichannel Microwave RadiometerRadiosonde data from the Joint Air Sea Interaction Experiment, JASIN, show that variations in q. and q. reflect changes of structure in the first 500 mb of the atmosphere. The SMMR measured q at least as accurately as the JASIN radiosondes. SMMR q. and rain rate values were in qualitative agreement
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Introduction to Techniques of Measurement and Analysis: Surface Processesce with the time and space scale of study) within the overall water cycle, they have a major impact on Man’s activities. Apart from the obvious harm caused by extremes — unhappily little studied in the water-budget context —even the average pattern of availability of water in its solid, liquid and g
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Monthly and Areal Patterns of Mean Global Precipitationual refinements used in deducing annual and seasonal variations of rainfall over large areas, a presentation is made of a gridding technique for evaluating precipitation over the continents and the oceans based on the subdivision of the Earth’s surface into nearly 2600 sectors and data obtained prio
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Comparison of Rainfall Rates Derived from Radar and , Microwave Observations in the Tropical Atlantiatmosphere system using a microwave radiometer on board the . satellite. These rainfall rates were compared with rainfall rates calculated from radar data for the same days. Reasons for the differences revealed are discussed.
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