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The North Icelandic Jet and its contribution to the Denmark Strait overflow water
Denmark Strait overflow water (DSOW) is a main contributor to the formation of the deep branch of...
C Corsaro, A Sterl | Status: submitted | Journal: Geophys. Res. Lett. | Year: 2013
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A maximum entropy approach to the parametrization of subgrid processes in two-dimensional flow
In numerical models of geophysical fluid systems parametrization schemes are needed to account fo...
WTM Verkley, PC Kalverla, CA Severijns | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 142 | Year: 2016 | First page: 2273 | Last page: 2283 | doi: 10.1002/qj.2817
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Extreme droogte in Zuidoost-Azië vanwege El Niño
Het sterkste effect van de `Zuidelijke Schommeling’ (Southern Oscillation, tegenwoordig beter bek...
GJ van Oldenborgh | Journal: Meteorologica | Volume: 26 | Year: 2015 | First page: 26 | Last page: 27
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SCIENTIFIC PREPARATIONS FOR AEOLUS AND AEOLUS FOLLOW-ON
In spring 2010 the ESA Core Explorer Atmospheric Dynamics Mission, ADM-Aeolus is due for launch. ...
ACM Stoffelen, GJ Marseille, J de Kloe, K Houchi, H Körnich, N Žagar | Conference: 9th International Winds Workshop | Organisation: NOAA | Place: Annapolis, maryland, USA | Year: 2008 | First page: 0 | Last page: 0
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To what extent can the 2002 Antarctic major stratospheric warming be explained by horizontal advection of the vortex from the pole?
The importance of horizontal and vertical advection of temperature for the Antarctic major strato...
PC Siegmund, PJF van Velthoven | Status: published | Journal: Meteor. Atmos. Phys. | Volume: 90 | Year: 2005 | First page: 165 | Last page: 177 | doi: 10.1007/s00703-004-0085-8
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