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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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Hoe vaak komt extreme neerslag zoals op 28 juli tegenwoordig voor, en is dat anders dan vroeger?
Op 28 juli vielen grote hoeveelheden neerslag in Nederland, op sommige plaatsen ontstond waterove...
GJ van Oldenborgh, G Lenderink | Journal: KNMI Kenniscentrum | Year: 2014
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Post-EPS Competing Scatterometer Designs: ASCAT versus RFSCAT
Post–EPS is the successor of the EUMETSAT Polar System (EPS) and will provide continuity of opera...
G Egger, M Belmonte Rivas | Conference: ARSI - Advanced RF Sensors and Remote Sensing Instruments | Organisation: European Space Agency | Place: Noordwijk (The Netherlands) | Year: 2009 | First page: 0 | Last page: 0
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