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An Application of a Large Scale Conceptual Hydrological Model Over the Elbe Region : Volume 3, Issue 3 (30/11/-0001)

By Lobmeyr, M.

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Book Id: WPLBN0003980730
Format Type: PDF Article :
File Size: Pages 12
Reproduction Date: 2015

Title: An Application of a Large Scale Conceptual Hydrological Model Over the Elbe Region : Volume 3, Issue 3 (30/11/-0001)  
Author: Lobmeyr, M.
Volume: Vol. 3, Issue 3
Language: English
Subject: Science, Hydrology, Earth
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Historic
Publication Date:
-0001
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Lohmann, D., Ruhe, C., & Lobmeyr, M. (-0001). An Application of a Large Scale Conceptual Hydrological Model Over the Elbe Region : Volume 3, Issue 3 (30/11/-0001). Retrieved from http://hawaiilibrary.net/


Description
Description: GKSS Research Center Geesthacht, Insitute for Atmospheric Physics D-21502 Geesthacht, Germany.. This paper investigates the ability of the VIC-2L model coupled to a routing model to reproduce streamflow in the catchment of the lower Elbe River, Germany. The VIC-2L model, a hydrologically-based land surface scheme (LSS) which has been tested extensively in the Project for Intercomparison of Land-surface Parameterization Schemes (PILPS), is put up on the rotated grid of 1/6 degree of the atmospheric regional scale model (REMO) used in the Baltic Sea Experiment (BALTEX). For a 10 year period, the VIC-2L model is forced in daily time steps with measured daily means of precipitation, air temperature, pressure, wind speed, air humidity and daily sunshine duration. VIC-2L model output of surface runoff and baseflow is used as input for the routing model, which transforms modelled runoff into streamflow, which is compared to measured streamflow at selected gauge stations. The water balance of the basin is investigated and the model results on daily, monthly and annual time scales are discussed. Discrepancies appear in time periods where snow and ice processes are important. Extreme flood events are analyzed in more dital. The influence of calibration with respect to runoff is examined.

Summary
An application of a large scale conceptual hydrological model over the Elbe region

 

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