The mixing layer height (MLH) is a key parameter in studies of many atmospheric boundary layer pr...
The Cabauw Experimental Site for Atmospheric Research (CESAR) was established in 2002 as a consor...
Deep convective clouds, such as Towering Cumulus (TCu) and Cumulonimbus (Cb) clouds, may pose a s...
This paper describes the PROMOTE UV Record, which aims to provide a global long-term record of th...
Mass budget calculations, validated with satellite gravity observations [from the Gravity Recover...
The strongly increasing interest for historical climate data (HISKLIM, CLIWOC, RECLAIM, ACRES) ov...
The original Beaufort scale of wind force is a scale that does not present the actual velocity wi...
Monthly temperature series for Central Europe back to AD 1500 are developed from documentary inde...
The origin of aerosol particles in the upper troposphere and lowermost stratosphere over the Eura...
For the assessment of the Hydraulic Boundary Conditions (HBC), information is required on wind co...
In recent years, a substantial reduction of the sea ice in the Arctic has been observed. At the s...
In the ECHAM5/MPI-OM model a collapse of the Atlantic thermohaline circulation results in a globa...
The U.S. Maury Collection (1796 1861), further denoted as MC, has been digitized in China during ...
Studies have demonstrated that precipitation on Northern Hemisphere mid-latitudes has increased i...
In this technical report we document the updates which have been made to the heterogeneous reacti...
Experiments in a cold wind tunnel were used to verify drifting snow sublimation models. A layer o...
This paper presents a standard procedure for the validation of cloud properties retrievals from s...
Als onderdeel van het project Dynamische Maximumsnelheden onderzoekt Rijkswaterstaat het effect v...
Voor de nieuwe operationele luchtkwaliteitverwachting van het RIVM, TNO en het KNMI is er een nie...
The impact of surface emissions on the zonal structure of tropical tropospheric ozone and carbon ...