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Impact of changes in the formulation of cloud‐related processes on model biases and climate feedbacks
To test the impact of modeling uncertainties and biases on the simulation of cloud feedbacks, sev...
C Lacagnina, FM Selten, AP Siebesma | Status: published | Journal: J. of Advances in Modeling Earth Systems | Year: 2014 | First page: 1224 | Last page: 1243 | doi: 10.1002/2014MS000341
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The CMOD7 Geophysical Model Function for ASCAT and ERS Wind Retrievals
A new geophysical model function (GMF), called CMOD7, has been developed for intercalibrated ERS ...
A Stoffelen, J Verspeek, J Vogelzang, A Verhoef | Status: published | Journal: IEEE Journal of Selected Topics in Applied Earth O | Year: 2017 | First page: 1 | Last page: 12 | doi: 10.1109/JSTARS.2017.2681806
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The influence of aggregation and statistical post‐processing on the subseasonal predictability of European temperatures
The succession of European surface weather patterns has limited predictability because disturbanc...
C van Straaten, K Whan, D Coumou, B van den Hurk, M Schmeits | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 146 | Year: 2020 | First page: 2654 | Last page: 2670 | doi: 10.1002/qj.3810
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Rainfall-induced attenuation correction for two operational dual-polarization C-band radars in the Netherlands
The Royal Netherlands Meteorological Institute (KNMI) operates two operational dual-polarization ...
A Overeem, H de Vries, H Al Sakka, R Uijlenhoet, H Leijnse | Status: published | Journal: J. Atm. Oceanic Technol. | Volume: 38 | Year: 2021 | First page: 1125 | Last page: 1142 | doi: 10.1175/JTECH-D-20-0113.1
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Linear and non-linear response of late Neogene glacial cycles to obliquity forcing and implications for the Milankovitch theory
Constraints are given for the geometry and time lags of the prominent obliquity-paced glacial sta...
LJ Lourens, J Becker, R Bintanja, FJ Hilgen, E Tuenter, RSW van de Wal, M Ziegler | Status: published | Journal: Quatern. Science Rev. | Volume: 29 | Year: 2010 | doi: 10.1016/j.quascirev.2009.10.018
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