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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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SCIAMACHY Absorbing Aerosol Index. Calibration issues and global results from 2002 - 2004
The Absorbing Aerosol Index (AAI) is the only operational aerosol product from the SCanning Imagi...
M de Graaf, P Stammes | Status: published | Journal: Atm. Chem. Phys. | Volume: 5 | Year: 2005 | First page: 2385 | Last page: 2394 | doi: 1680-7324/acp/2005-5-2385
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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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Obliquely incident surface waves in shallow water of variable depth
The propagation properties of obliquely incident, weakly nonlinear surface waves in shallow water...
CA van Duin | Status: submitted | Journal: J. Fluid Mech. | Year: 2005
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The effect of temporal variations in the surface mass balance and temperature-inversion strength on the interpretation of ice-core signals
The proxy for temperature (delta-signal) in ice cores is stored in the snow/ice during precipitat...
NPM van Lipzig, E van Meijgaard, J Oerlemans | Status: published | Journal: Journal of Glaciology | Volume: 48 | Year: 2002 | First page: 611 | Last page: 621
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