Observations show that subdaily precipitation extremes increase with dew point temperature at a r...
Large-eddy simulations with strong lateral forcing representative of precipitation over the Nethe...
The low-frequency contribution to the systematic and random sampling errors in single-tower eddy-...
Results of four Lagrangian stratocumulus-to-shallow-cumulus transition cases as obtained from six...
Conditional Markov chain (CMC) models have proven to be promising building blocks for stochastic ...
Some climate modeling results suggest that the Hadley circulation might weaken in a future climat...
Six Single-Column Model (SCM) versions of climate models are evaluated on the basis of their repr...
Fundamental puzzles of climate science remain unsolved because of our limited understanding of ho...
As described in Neggers et al. 2012, the KNMI Parameterization Testbed (KPT) consists of two main...
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...
Observational data of rainfall from a rain radar in Darwin, Australia, are combined with data def...
Equilibrium states of stratocumulus are evaluated for a range of free tropospheric conditions in ...
To test the impact of modeling uncertainties and biases on the simulation of cloud feedbacks, sev...
The relationship between the inversion stability and the liquid water path (LWP) tendency of a ve...
Mixing processes in deep precipitating cumulus clouds are investigated by tracking Lagrangian par...
Equilibrium states of stratocumulus are evaluated for a range of free tropospheric conditions in ...
The physical properties of rain spectra are gener- ally modeled using an analytical distribution....
A mixed-layer model is used to study the response of stratocumulus equilibrium state solutions to...
CGILS—the CFMIP-GASS Intercomparison of Large Eddy Models (LESs) and single column models (SCMs)—...
Large-eddy simulations of a Lagrangian transition from a vertically well-mixed stratocumulus-topp...