For the assessment of the Hydraulic Boundary Conditions (HBC), information is required on wind co...
Validation of OMI-TOMS and OMI-DOAS total ozone column using five Brewer spectroradiometers at th...
De zeedijkhoogte wordt bepaald aan de hand van de terugkeertijd van extreme wateropzet. In de Ned...
We investigate rapid around-the-world transport of a smoke aerosol plume released by intense fore...
Methane retrievals from the Scanning Imaging Absorption Spectrometer for Atmospheric Chartography...
Estimation of the detection efficiency of a operational lightning detection network is not a triv...
Extreme rainfall events can have a large impact on society and can lead to loss of life and prope...
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...
Vertical air speed plays an important role in several atmospheric processes e.g. like in turbulen...
The temperature and pressure differences between Tokyo and Nagasaki were used to reconstruct past...
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...
Product User Manual of the Ocean and Sea Ice Satellite Application Facility (OSI SAF) and EUMETSA...
Product User Manual of the Ocean and Sea Ice Satellite Application Facility (OSI SAF) SeaWinds wi...
This paper presents a detailed global comparison of SCIAMACHY and MOPITT carbon monoxide (CO) col...
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...