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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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Het hoe, wat en waarom van infrageluid metingen
Infrageluid is onhoorbaar geluid omdat het bestaat uit frequenties lager dan 20 Hz. Dit type gelu...
LG Evers | Journal: Meteorologica | Volume: 18 | Year: 2009 | First page: 24 | Last page: 26
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Technical description of the KNMI Rainfall Generators for the Rhine and Meuse basins
This report gives a technical description of what is briefly known as the KNMI Rainfall (or Weath...
Jules J. Beersma, T. Adri Buishand and Maurice J. Schmeits
| Year: 2014 | Pages: 32
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Lateral mixing in shallow convection: In theory and in practice
Analytical expressions, in principle also valid for an ensemble of clouds, are derived for $\eps$...
WC de Rooy, AP Siebesma | Journal: Hirlam Newsletter | Year: 2009
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Time series transformation tool version 3.1 Description of the program to generate time series consistent with the KNMI’14 climate scenarios
This report presents the ’Transformation Program version 3.1 KNMI’14’1,2. Chapter 2 to 4 are devo...
A. Bakker | Year: 2015 | Pages: 43
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