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

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Sabine Urban,Ulrike Mayrhofer,Bj?rn Walliseristical methods does not eliminate the systematic error. Both kinds of inhomogeneities can be eliminated only using the correction procedures. In this way compatible and homogeneous data sets of precipitation for any time period and any size of area can be provided.

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,Unternehmensethische überlegungen, streamlined body in a shape of a flat plate protected by the wind shield. Yet such gauges are not used at all. A common precipitation gauge consists of an upright cylinder having rather poor aerodynamic properties. Therefore, with regard to a considerable systematic error due to wind, the measured precipitation values have to be corrected.

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Extreme Precipitation in the Northern Hemisphere the series has been evaluated, the maximal precipitation’s temporal structure has been investigated. Record amounts of precipitation for various durations have been obtained..In the future, all the generalized climatological infommtion can be displayed in the form of monthly maps, which will be used for applied purposes and for forecasting.

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Terrestrial Precipitation Analysis: Operational Method and Required Density of Point Measurements has prepared analyses of 24 months (1987,1988). Some intercomparisons of large areal means over the continents are presented for different precipitation data sets (GPCC analyses. Legates climatology, satellite data, accumulated daily forecast results of the ECMWF model).

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The Effect of Dimensions and Shape of Precipitation Gauges on the Wind-Induced Error streamlined body in a shape of a flat plate protected by the wind shield. Yet such gauges are not used at all. A common precipitation gauge consists of an upright cylinder having rather poor aerodynamic properties. Therefore, with regard to a considerable systematic error due to wind, the measured precipitation values have to be corrected.