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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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[Global Climate] Stratospheric ozone [in
In 2013, the vast majority of the monitored climate
variables reported here maintained trends est...
M Weber, W Steinbrecht, RJ van der A, M Coldewey-Egbers, VE Fioletov, SM Frith, CS Long, D Loyola, JD Wild | Journal: Bull. Amer. Meteor. Soc. | Volume: 95 | Year: 2014 | First page: S38 | Last page: S40 | doi: http://dx.doi.org/10.1175/2014BAMSStateoftheClimate.1
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Time scale interaction in low-order climate models
Over the last decades, the study of climate variability has attracted ample attention. The observ...
L van Veen | University: Universiteit Utrecht | Year: 2002
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North Sea Wind Climatology Part 2: ERA-Interim and Harmonie model data
The national government needs high quality offshore wind climatology at and around hub height to ...
I.L. Wijnant, H.W. van den Brink and A. Stepek | Year: 2014 | Pages: 52
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Ruimtelijke klimatologische verschillen binnen Nederland
Weer- en klimaatinformatie wordt gebruikt in veel sectoren in de samenleving, zoals het waterbehe...
D Wolters, C Homan, J Bessembinder | Year: 2011
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