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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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Modeling orbital induced variations in circum-Mediterranean climate
The climate of the Earth varies both irregular and (quasi)periodic over a broad range of time-sca...
E Tuenter | University: Universiteit Utrecht | Year: 2004
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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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Aeolus lidar surface return (LSR) at 355 nm as a new Aeolus Level-2A product
The Atmospheric Laser Doppler Instrument (ALADIN) aboard Aeolus was the first spaceborne high-reso...
Lev D. Labzovskii, Gerd-Jan van Zadelhoff, David P. Donovan, Jos de Kloe, L. Gijsbert Tilstra, Ad Stoffelen, Damien Josset, and Piet Stammes
| Journal: Atmos. Meas. Tech. | Volume: 17 | Year: 2024 | First page: 7183 | Last page: 7208 | doi: https://doi.org/10.5194/amt-17-7183-2024
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