The MERCURE project
 
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Institute
 regional climate research
 
 
Dr. habil. Dietrich Heimann

Institut für Physik der Atmosphäre
DLR Oberpfaffenhofen
D-82234 Weßling, Germany
Telephone: ++49-8153-28-2508
Telefax:      ++49-8153-28-1841
eMail: d.heimann@dlr.de

Dr. Udo Busch
 

MERCURE - Modelling European Regional Climate, Understanding and Reducing Errors

MERCURE is a European framework IV project financed by the European Commission under contract ENV4-CT97-0485

November 1997 - November 2000
 
Coordinator: Dr. Richard Jones U.K. MetOffice - HadleyCentre
Partners: Dr. Dietrich Heimann DLR - Institut für Physik der Atmosphäre
Dr. Jens Hesselbjerg Christensen Danmarks Meteorologiske Institut
Prof. Dr. Christoph Schär ETH Zürich - Institut für Klimaforschung
Dr. Michel Déqué Météo France
Dr. Bennert Machenhauer Max-Planck-Institut für Meteorologie



Objectives and goals:
The project has the following five main objectives and associated goals:
  1. To improve regional climate models (RCMs) by understanding the source of errors and reducing them by improving the model's representation of physical processes (including increasing resolution). The focus will be on improving the simulation of surface air temperature, reducing errors to 1 K over most of Europe and 2 K locally, and precipitation, reducing errors to 1 mm/day over Europe. Higher resolution models will be expected to perform better than equivalent standard resolution over their common area.
  2. To improve the hydrological cycle in regional models via improved formulations of land-surface processes, radiation and precipitation physics. New aspects of the simulations will be validated by comparing with run-off, snow-pack and soil-moisture data.
  3. To assess the ability of regional models to reproduce observed precipitation freqeuncy distribution, including the frequency of heavy events, not just climatological means. The models should have realistic frequency distributions and increases in resolution should improve the simulation on all scales.
  4. To further characterise errors in regional climate simulations nested in general circulation models (GCMs) derived from the GCM driving data. GCM errors which induce large-scale errors in the RCMs will be identified and GCM modellers will be encouraged to reduce them.
  5. To provide a statistical-dynamical tool linking RCM and GCM simulations to extend the length of RCM integrations. The method will be able to repruduce the main features of long RCM simulations from large-scale driving data given shorter sets of both for calibration.


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 Last change 20 November 2001