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2Observation Representativeness Error
NWP models simulate the atmospheric state on a given model grid, thereby principally
limiting the...
GJ Marseille, A Stoffelen | Year: 2012
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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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Global aerosol effect retrieval from passive hyperspectral measurements
Absorbing aerosols can have a significant local direct radiative effect (DRE), while the global a...
M de Graaf, LG Tilstra, P Stammes | Conference: ESA Living Planet Symposium 2013 | Place: Edinburgh, United Kingdom | Year: 2013 | First page: 0 | Last page: 0
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Historical wind speed equivalents of the Beaufort scale, 1850-1950
The original Beaufort scale of wind force is a scale that does not present the actual velocity wi...
H Wallbrink, FB Koek | Year: 2009
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Application of CM-SAF cloud and radiation products to verify surface cloud radiative effects in climate models over ocean
Clouds play a major role in the climate system due to their impact on the energy budget, both at ...
T Hanschmann, A Macke, R Roebeling, H Deneke | Year: 2010
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