Multitude of clouds and precipitation observations in Germany is described. Data are available no...
The height of the atmospheric boundary layer or mixing layer is an important parameter for unders...
A first direct intercomparison of aerosol vertical profiles from Multi-Axis Differential Optical ...
We evaluate the capability of the global atmospheric transport model TM5 to simulate the boundary...
Vertical profiles of the aerosol particles hygroscopic properties, their mixing state as well as ...
As described in Neggers et al. 2012, the KNMI Parameterization Testbed (KPT) consists of two main...
The Climate Changes Spatial Planning (CcSP) project ME02: Integrated observations and modelling o...
The vertical distribution of the shortwave flux in the atmosphere is important for understanding ...
Water vapour is a crucial parameter in atmospheric physics. Concentrations are low at upper tropo...
The mixing layer height (MLH) is a key parameter in studies of many atmospheric boundary layer pr...
Five active and passive remote sensing techniques that observe clouds are operated nearly continu...
The Royal Netherlands Meteorological Institute (KNMI) evaluated the usefullness of the NubiScope,...
The calibration of the CloudSat spaceborne cloud radar has been thoroughly assessed using very ac...
The mixing layer height (MLH) is a key parameter in studies of many atmospheric boundary layer pr...
A climatology of nocturnal low-level jets (LLJs) is presented for the topographically flat measur...
EAGLE2006 – an intensive field campaign for the advances in land surface hydrometeorological proc...
Climate of Northeastern Africa varies from humid to semi-arid with both abundant and scarce moist...