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Determination of the mixing layer height from ceilometer backscatter profiles
The mixing layer height (MLH) is a key parameter in studies of many atmospheric boundary layer pr...
MJ de Haij, H Klein Baltink, WMF Wauben | Journal: KNMI Kenniscentrum | Year: 2010
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The impact of varying ice sheets and greenhouse gases on the intensity and timing of boreal summer monsoons
Climate models, forced only with insolation, indicate that boreal summer monsoons respond to orbi...
SL Weber, E Tuenter | Status: published | Journal: Quatern. Science Rev. | Volume: 30 | Year: 2011 | First page: 469 | Last page: 479 | doi: 10.1016/j.quascirev.2010.12.009
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Interim report on the validation of Harmonie
For the derivation of the Hydraulic Boundary Conditions, information of extreme winds over open-w...
P Baas, H de Waal | Year: 2012
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Spatial and Temporal Propagation of Scatterometer Winds
Ocean models are generally forced by synthetic (global) NWP model wind fields. It has however bee...
D Harutyunyan, A Stoffelen | Year: 2011
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Detecting Labrador Sea Water formation from space
In situ monitoring of deep water formation in the Labrador Sea is severely hampered by the harsh ...
R Gelderloos, CA Katsman, K Vage | Status: published | Journal: J. Geophys. Res. | Volume: 118 | Year: 2013 | First page: 2074 | Last page: 2086 | doi: 10.1002/jgrc.20176
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