Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties

Hydrological modelling of floods relies on precipitation data with a high resolution in space and time. A reliable spatial representation of short time step rainfall is often difficult to achieve due to a low network density. In this study hourly precipitation was spatially interpolated with the mul...

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Main Authors: A. Verworn, U. Haberlandt
Format: Article
Language:English
Published: Copernicus Publications 2011-02-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/15/569/2011/hess-15-569-2011.pdf
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spelling doaj-545a4965a10d4dbba02a1b147e0c4bae2020-11-24T22:04:09ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382011-02-0115256958410.5194/hess-15-569-2011Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm propertiesA. VerwornU. HaberlandtHydrological modelling of floods relies on precipitation data with a high resolution in space and time. A reliable spatial representation of short time step rainfall is often difficult to achieve due to a low network density. In this study hourly precipitation was spatially interpolated with the multivariate geostatistical method kriging with external drift (KED) using additional information from topography, rainfall data from the denser daily networks and weather radar data. Investigations were carried out for several flood events in the time period between 2000 and 2005 caused by different meteorological conditions. The 125 km radius around the radar station Ummendorf in northern Germany covered the overall study region. One objective was to assess the effect of different approaches for estimation of semivariograms on the interpolation performance of short time step rainfall. Another objective was the refined application of the method kriging with external drift. Special attention was not only given to find the most relevant additional information, but also to combine the additional information in the best possible way. A multi-step interpolation procedure was applied to better consider sub-regions without rainfall. <br><br> The impact of different semivariogram types on the interpolation performance was low. While it varied over the events, an averaged semivariogram was sufficient overall. Weather radar data were the most valuable additional information for KED for convective summer events. For interpolation of stratiform winter events using daily rainfall as additional information was sufficient. The application of the multi-step procedure significantly helped to improve the representation of fractional precipitation coverage. http://www.hydrol-earth-syst-sci.net/15/569/2011/hess-15-569-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Verworn
U. Haberlandt
spellingShingle A. Verworn
U. Haberlandt
Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties
Hydrology and Earth System Sciences
author_facet A. Verworn
U. Haberlandt
author_sort A. Verworn
title Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties
title_short Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties
title_full Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties
title_fullStr Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties
title_full_unstemmed Spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties
title_sort spatial interpolation of hourly rainfall – effect of additional information, variogram inference and storm properties
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2011-02-01
description Hydrological modelling of floods relies on precipitation data with a high resolution in space and time. A reliable spatial representation of short time step rainfall is often difficult to achieve due to a low network density. In this study hourly precipitation was spatially interpolated with the multivariate geostatistical method kriging with external drift (KED) using additional information from topography, rainfall data from the denser daily networks and weather radar data. Investigations were carried out for several flood events in the time period between 2000 and 2005 caused by different meteorological conditions. The 125 km radius around the radar station Ummendorf in northern Germany covered the overall study region. One objective was to assess the effect of different approaches for estimation of semivariograms on the interpolation performance of short time step rainfall. Another objective was the refined application of the method kriging with external drift. Special attention was not only given to find the most relevant additional information, but also to combine the additional information in the best possible way. A multi-step interpolation procedure was applied to better consider sub-regions without rainfall. <br><br> The impact of different semivariogram types on the interpolation performance was low. While it varied over the events, an averaged semivariogram was sufficient overall. Weather radar data were the most valuable additional information for KED for convective summer events. For interpolation of stratiform winter events using daily rainfall as additional information was sufficient. The application of the multi-step procedure significantly helped to improve the representation of fractional precipitation coverage.
url http://www.hydrol-earth-syst-sci.net/15/569/2011/hess-15-569-2011.pdf
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AT uhaberlandt spatialinterpolationofhourlyrainfalleffectofadditionalinformationvariograminferenceandstormproperties
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