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Hoe warmen broeikasgassen de aarde op? Deel 1: directe stralingseffecten
Er zijn veel manieren om het versterkte broeikaseffect te beschrijven, variërend van `een dekentj...
GJ van Oldenborgh, R van Dorland, P Siegmund | Journal: KNMI Kenniscentrum | Year: 2010
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Data access for atmospheric research
As data acquisition techniques advance, enormous quantities of data are gathered and stored. Ofte...
WJ Som de Cerff, J van de Vegte, RM van Hees | Year: 2002
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The spatial and temporal variability of the surface mass balance in Antarctica: results from a regional atmospheric climate model
A 14-year integration with a regional atmospheric model (RACMO) is used to obtain detailed inform...
NPM van Lipzig, E van Meijgaard, J Oerlemans | Status: published | Journal: Int. J. Climatology | Year: 2002 | First page: 1197 | Last page: 1217
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Evaluation of a regional atmospheric model using measurements of surface heat exchange processes from a site in Antarctica
A regional atmospheric climate model with a horizontal grid spacing of 55 km has been used to sim...
NPM van Lipzig, E van Meijgaard, J Oerlemans | Status: published | Journal: Mon. Wea. Rev. | Volume: 127 | Year: 1999 | First page: 1994 | Last page: 2011
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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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