As part of an international intercomparison project, the weak temperature gradient (WTG) and damp...
Op 24 april was het precies een jaar geleden dat het KNMI het crowdsourcing initiatief WOW-NL lan...
Station-based observations and bias-corrected model simulations show that the frequency of short-...
The vulnerability of the European airspace to volcanic eruptions was brought to the attention of ...
The Ozone Monitoring Instrument (OMI) is a push-broom imaging spectrometer, observing solar...
Most papers in this focus issue on 'climate and climate impact projections for adaptation strateg...
Time series of visibility and aerosol optical thickness for the Netherlands have been constructed...
Results are presented of two large-eddy simulation (LES) runs of the entire year 2012 centered at...
Twenty-five large-eddy simulations are performed to study how free tropospheric thermody- namic c...
Six Single-Column Model (SCM) versions of climate models are evaluated on the basis of their repr...
Observational data of rainfall from a rain radar in Darwin, Australia, are combined with data def...
A methodology for the round-robin evaluation and the geophysical validation of ozone profile data...
As described in Neggers et al. 2012, the KNMI Parameterization Testbed (KPT) consists of two main...
Fundamental puzzles of climate science remain unsolved because of our limited understanding of ho...
As part of an international intercomparison project, a set of single-column models (SCMs) and clo...
Equilibrium states of stratocumulus are evaluated for a range of free tropospheric conditions in ...
This report documents and motivates the KNMI’14 climate change scenarios. It has an intermediate ...
To test the impact of modeling uncertainties and biases on the simulation of cloud feedbacks, sev...