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Stationary abyssal circulation forced by enhanced upwelling over a mid-ocean ridge
Stommel and co-workers calculated the stationary, geostrophic circulation in the abyssal ocean ...
CA Katsman | Status: published | Journal: J. Phys. Oceanogr. | Volume: 36 | Year: 2006 | First page: 1660 | Last page: 1671
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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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Tropical disturbances in a GCM
We have analyzed the tropical disturbances in a 11-layer atmospheric general circulation model (G...
RJ Haarsma, JFB Mitchell, CA Senior | Status: published | Journal: Clim. Dyn. | Volume: 8 | Year: 1993 | First page: 247 | Last page: 257
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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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Ambiguity Removal and Product Monitoring for SeaWinds, version 1.2
This report is a technical note on the implementation of Ambiguity Removal (AR) and the product m...
J de Vries, A Stoffelen, J Beysens | Year: 2005
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