Titlebook: Global Precipitations and Climate Change; Michel Desbois,Fran?oise Désalmand Conference proceedings 1994 Springer-Verlag Berlin Heidelberg

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1431-7125 cipitation are also likely to occur. Such changes have been redorded in the past by paleoclimatological studies or in the field of climatology. Different approaches to monitoring and forecasting the evolution of climate-scale precipitation are reviewed by paleoclimatologists, hydrologists, satellite

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Henning Kehr,J?rg Michael Gummersbachoviet Union, together with forty-year time series of snowfall and total precipitation over most of North America. Trends analyses confirm previous results about precipitation increase of northern extratropics and quantify them for North America.

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Precipitation Changes Over the Northern Hemispheric Extratropics During the Last Hundred Yearsoviet Union, together with forty-year time series of snowfall and total precipitation over most of North America. Trends analyses confirm previous results about precipitation increase of northern extratropics and quantify them for North America.

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1431-7125 ent approaches to monitoring and forecasting the evolution of climate-scale precipitation are reviewed by paleoclimatologists, hydrologists, satellite meteorologists, and climate modellers. .978-3-642-79270-0978-3-642-79268-7Series ISSN 1431-7125

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Internationales Emissionsgesch?ftggest that during stage 5.5 and the early Holocene, the SW monsoon was probably stronger which resulted in higher precipitation and lower surface salinity. In contrast, during the time interval between 90 and 15 kyr and in particular during the glacial stages 6, 2 and substage 5.2 the SW monsoon was

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n of water balance elements was carried out according to the Zubenok - Budyko complex method. At assessment of climate warming impacts upon changes of relative air humidity and snow cover characteristics was used an empirical correlation method. Two climatological stations (Hurbanovo 115 m a.s.l. an

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