We developed a user-friendly database with the 1750-1854 CLIWOC data, which is suitable to be int...
Changes in severity of extreme weather events under influence of the enhanced greenhouse effect c...
Simulations with regional climate models (RCMs), carried out for the Rhine basin, have been analy...
In many regions the strength of El Niño-Southern Oscillation (ENSO) teleconnections has varied ov...
A stochastic weather generator has been developed to simulate long daily sequences of rainfall an...
We present a series of daily pressure readings taken 1697-1698 in Leiden (Netherlands) by W. Sen...
The importance of horizontal and vertical advection of temperature for the Antarctic major strato...
Trends in the annual number of independent wind events over the Netherlands are studied for the p...
Wet deposition of reduced nitrogen is estimated for the United Kingdom using a Lagrangian long-te...
The Absorbing Aerosol Index (AAI) was investigated and used to analyze GOME data and compare it t...
The Absorbing Aerosol Index (AAI) is the only operational aerosol product from the SCanning Imagi...
Nadir ozone profiles retrieved from the GOME (Global Ozone Monitoring Experiment) instrument are ...
We introduce an alternative method for the retrieval of polarisation in the ultraviolet by the sa...
In this paper we present an extensive validation of calibrated SCIAMACHY nadir reflectance in the...
We present a reflectance validation method, using a polarized radiative transfer model as a refer...
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...
Recently, many people have found polarisation features in the SCIAMACHY Level-1c spectrum, in the...
A fast atmospheric General Circulation Model is used to generate three ensembles of atmospheric c...