Simulations with seven regional climate models driven by a common control climate simulation of a...
Ten single-column models (SCMs) from eight groups are used to simulate a nocturnal nonprecipitati...
The IFE-1.6 scientific data set of SCIAMACHY limb ozone profiles is validated for the period Aug...
Het Rijn-Maas mondingsgebied is één van de locaties in Nederland waar zoutindringing vanuit zee...
The Southern Hemisphere major warming event in September 2002 has led to a breakup of the vortex ...
Using the CARIBIC Boeing 767 aircraft, a suite of trace gases and aerosols was measured between G...
ERA-40 is a re-analysis of meteorological observations from September 1957 to August 2002 produce...
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 ...
A method is presented to manually adjust the analysis of a numerical weather forecasting model a...
We investigate the role of the ocean feedback on the climate response to insolation forcing durin...
A stochastic weather generator has been developed to simulate long daily sequences of rainfall an...
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...
Nadir ozone profiles retrieved from the GOME (Global Ozone Monitoring Experiment) instrument are ...
Recently, many people have found polarisation features in the SCIAMACHY Level-1c spectrum, in the...
A global comparison of altimeter and ERA-40 mean wave period data is performed for the first time...
A new nonparametric method to correct model data is proposed. At any given point in space and tim...
In this article global estimates of 100-yr return values of wind speed and significant wave heigh...