ACCUMULATED PRECIPITATION DISTRIBUTION BASED ON COMBINED SATELLITE INFORMATION AND GROUND M.pdf
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ACCUMULATED PRECIPITATION DISTRIBUTION BASED ON COMBINED SATELLITE INFORMATION AND GROUND M
ACCUMULATED PRECIPITATION DISTRIBUTION BASED ON
COMBINED SATELLITE INFORMATION AND GROUND
MEASUREMENTS
Piotr Struzik
Institute of Meteorology and Water Management
P. Borowego Str. 14, 30-215 Krakow, POLAND
ABSTRACT
The detailed space distribution of accumulated precipitation is highly required as input for both hydrological
and agro-meteorological models. Relatively precision but sparse ground measurement network is frequently
not adequate even using interpolation methods. The rainfall estimations based only on IR or IR/VIS satellite
data give more detailed structure of rainfall distribution but absolute error is large sometimes. To solve this
problem, the method for merged satellite and conventional information use, was developed. Polish network
of synoptic stations, climate posts and raingauges with addition of rainfall estimation based on METEOSAT
satellite data were used. The 24 hours accumulated rainfall product was tested. First tests based on 2001-
2002 cases showed interesting results, especially for convective precipitation. Description of the method and
discussion on obtained results are presented in the paper.
1. INTRODUCTION
Most important information for hydrology is amount of precipiatation accumulated in certain period of time.
Frequently used product is 24 hours accumulated precipitation. Standard measurement performed on the
ground have limited number of points represented by synoptic, climatic and raingauge posts. Due to
communication problems frequently only synoptic or synoptic + climatic posts deliver measurements in real
time. Modelling distribution of rainfall amount with this information is frequently misleading. Distances
between stations are large (sometime more then 100 km). Outside of country, precipitation information is
limited (neighbour countries) or completely not available (sea). As a result amount of precipitation is not
correctly spatially modelled specially in storm cases.
On the area of Poland, actually 57 Synop stations and 154
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