Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology Model

A fully integrated Atmospheric-Ocean-Hydrology Model (BALTIMOS = Baltic Integrated Model System) has been developed using existing model components. Experiment and model design has been adapted to the Baltic basin with a catchment area of approximately 1 750 000 km<sup>2</sup>. A compreh...

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Main Authors: K.-G. Richter, M. Ebel
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/9/31/2006/adgeo-9-31-2006.pdf
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author K.-G. Richter
M. Ebel
author_facet K.-G. Richter
M. Ebel
author_sort K.-G. Richter
collection DOAJ
description A fully integrated Atmospheric-Ocean-Hydrology Model (BALTIMOS = Baltic Integrated Model System) has been developed using existing model components. Experiment and model design has been adapted to the Baltic basin with a catchment area of approximately 1 750 000 km<sup>2</sup>. A comprehensive model validation has been completed using large meteorological and hydrological measurement database. Comparing the calculated runoff from the integrated and non-integrated model system with measurements for three different representative subbasins and the entire Baltic basin, the effect of the integrated model is described. The results display a good agreement between measured and calculated runoff. The effect of the integrated model is rather negligible looking at computed mean values: There is no significant difference between mean monthly runoff of the integrated and non-integrated model during the year with the exception of spring. There is a delay of one month with regard to peak runoff for the non-integrated model in spring caused by different interactive processes during the melting period.
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spelling doaj.art-0f7ac448892e4f448176ce5aaa9b4fcf2022-12-21T19:42:32ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592006-01-0193137Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology ModelK.-G. RichterM. EbelA fully integrated Atmospheric-Ocean-Hydrology Model (BALTIMOS = Baltic Integrated Model System) has been developed using existing model components. Experiment and model design has been adapted to the Baltic basin with a catchment area of approximately 1 750 000 km<sup>2</sup>. A comprehensive model validation has been completed using large meteorological and hydrological measurement database. Comparing the calculated runoff from the integrated and non-integrated model system with measurements for three different representative subbasins and the entire Baltic basin, the effect of the integrated model is described. The results display a good agreement between measured and calculated runoff. The effect of the integrated model is rather negligible looking at computed mean values: There is no significant difference between mean monthly runoff of the integrated and non-integrated model during the year with the exception of spring. There is a delay of one month with regard to peak runoff for the non-integrated model in spring caused by different interactive processes during the melting period.http://www.adv-geosci.net/9/31/2006/adgeo-9-31-2006.pdf
spellingShingle K.-G. Richter
M. Ebel
Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology Model
Advances in Geosciences
title Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology Model
title_full Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology Model
title_fullStr Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology Model
title_full_unstemmed Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology Model
title_short Analysis of runoff for the Baltic basin with an integrated Atmospheric-Ocean-Hydrology Model
title_sort analysis of runoff for the baltic basin with an integrated atmospheric ocean hydrology model
url http://www.adv-geosci.net/9/31/2006/adgeo-9-31-2006.pdf
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