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The adjoint of the WAM model
This manual gave a description how to use the WamC5 system, which allows for adjoint runs of the ...
H Hersbach | Year: 1997 | Pages: 33
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Back-up modellering van windmeetmasten op luchthavens
Information about the wind speed and wind direction is of great importance for an airplane during...
Ilja Smits | Year: 1999 | Pages: 71
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A scintillation experiment over a forest
Scintillation measurements were carried out on a path of 1640 m over an inhomogeneous forest.
Th...
W. Kohsiek | Year: 1992 | Pages: 14
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A directional surface reflectance climatology determined from TROPOMI observations
In this paper, we introduce a spectral surface reflectivity climatology based on observations mad...
L.G. Tilstra, M. de Graaf, V.J.H. Trees, P. Litvinov, O. Dubovik, P. Stammes | Journal: Atmospheric Measurement Techniques | Volume: 17 | Year: 2024 | First page: 2235 | Last page: 2256 | doi: 10.5194/amt-17-2235-2024
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Variability in Labrador Sea Water formation
The Labrador Sea is located in the northwestern corner of the North Atlantic Ocean. Although smal...
R Gelderloos | University: Universiteit Utrecht | Year: 2012
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