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Observing Three dimensional Water Vapour using a surface network of GPS receivers
Atmospheric water vapour is highly variable both in space and time.
In an operational sense, only...
S de Haan, H van der Marel | Status: submitted | Journal: Atm. Chem. Phys. | Year: 2008
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On Scatterometer Ocean Stress
Scatterometers estimate the relative atmosphere-ocean motion at spatially high resolution and pro...
M Portabella, ACM Stoffelen | Status: published | Journal: J. Atm. Oceanic Technol. | Volume: 26 | Year: 2009 | First page: 368 | Last page: 382 | doi: 10.1175/2008JTECHO578.1
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A non-stationary index-flood model for precipitation extremes in transient Regional Climate Model simulations
The Generalized Extreme Value (GEV) distribution has often been used to describe the distribution...
M Hanel, TA Buishand, CAT Ferro | Year: 2009
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Turbulent dispersion in cloudy boundary layers
Compared to dry boundary layers, dispersion in cloud-topped boundary layers has received less att...
RA Verzijlbergh, T Heus, HJJ Jonker, J Vila | Status: published | Journal: Atm. Chem. Phys. | Volume: 8 | Year: 2008 | First page: 19637 | Last page: 19677 | doi: 10.5194/acpd-8-19637-2008
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Evaluation of the daylight cycle of model predicted cloud amount and condensed water path over Europe with observations from MSG-SEVIRI
The evaluation of the diurnal cycle of Cloud Amount (CA) and cloud Condensed Water Path (CWP) as ...
RA Roebeling, E van Meijgaard | Status: published | Journal: J. Climate | Volume: 22 | Year: 2009 | First page: 1749 | Last page: 1766 | doi: 10.1175/2008JCLI2391.1
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