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A Study of the leakage of the Antarctic polar vortex in late austral winter and spring using isentropic and 3-D trajectories
The permeability of the Antarctic polar vortex is investigated in late austral winter and spring ...
MC Öllers, PFJ van Velthoven, HM Kelder, LPJ Kamp | Status: published | Journal: J. Geophys. Res. | Volume: 107 | Year: 2002 | First page: 4328 | doi: doi:10.1029/2001JD001363
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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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Rigorous test of the performance of shear-wave velocity correlations derived from CPT soundings: A case study for Groningen, the Netherlands
An improved correlation between shear-wave velocity VS and cone penetration test (CPT) parameters...
PP Kruiver, G de Lange, F Kloosterman, M Korff, J van Elk, D Doornhof | Status: published | Journal: Soil Dynamics and Earthquake Engineering | Volume: 140 | Year: 2021 | doi: 10.1016/j.soildyn.2020.106471
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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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