Interrelationships between volume extinction oefficient, ice water content (IWC), and effective r...
ERA-40 is a re-analysis of meteorological observations from September 1957 to August 2002 produce...
The NCEP/NCAR re-analyses data as well as ensemble integrations with an atmospheric GCM indicate ...
This paper describes the global chemistry Transport Model, version 5 (TM5) which allows two-way ...
Characteristics and origin of the aerosol in the lowermost stratosphere at northern midlatitudes ...
We investigate the role of the ocean feedback on the climate response to insolation forcing durin...
Simulations with regional climate models (RCMs), carried out for the Rhine basin, have been analy...
Nadir ozone profiles retrieved from the GOME (Global Ozone Monitoring Experiment) instrument are ...
A Regional Atmospheric Climate MOdel RACMO has been run over the Nile Basin (12°S, 36°N and 10°W ...
Large evaporation occurs over the Sudd wetland, a huge swamp located on the Upper Nile. Historica...
A fast atmospheric General Circulation Model is used to generate three ensembles of atmospheric c...
This is the second part of a rigorous model evaluation study involving five global Chemistry-Tra...
The transformation of water masses induced by air-sea fluxes in the South Atlantic is calculated...