The Atmospheric Dynamics Mission ADM-Aeolus is scheduled for launch in April 2011. ADM-Aeolus is ...
De KNMI klimaatscenario’s voor Nederland uit 2006 zijn getoetst aan de nieuwste nationale en inte...
The possibilities of calibrating the wind results by means of surface reflections is studied. To ...
This document describes the work done and the results obtained for Work Package (WP) 4 of the Ver...
The difference between the theoretical Rayleigh-Brillouin lineshape and the measured lineshape fr...
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...