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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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Meteorological Source Variability in Atmospheric Gravity Wave Parameters Derived From a Tropical Infrasound Station
Gravity waves are an important part of the momentum budget of the atmosphere. Despite this, param...
GJ Marlton, AJ Charlton-Perez, RG Harrison, Blanc, LG Evers, A Le-Pichon, PSM Smets | Status: published | Journal: J. Geophys. Res. | Volume: 124 | Year: 2019 | First page: 4352 | Last page: 4364 | doi: https://doi.org/10.1029/2018JD029372
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A Year-Long Large-Eddy Simulation of the Weather over Cabauw: An Overview
Results are presented of two large-eddy simulation (LES) runs of the entire year 2012 centered at...
J Schalkwijk, HJJ Jonker, AP Siebesma, FC Bosveld | Status: published | Journal: Mon. Wea. Rev. | Volume: 143 | Year: 2015 | First page: 828 | Last page: 844 | doi: http://dx.doi.org/10.1175/MWR-D-14-00293.1
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Effects of soil moisture gradients on the path and the intensity of a West African squall line
During the West African monsoon season, precipitation is strongly coupled to soil moisture availa...
D Wolters, CC Van Heerwaarden, J Vilà -Guerau de Arellan, B Cappelaere, D Ramier | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 136 | Year: 2010 | First page: 2162 | Last page: 2175 | doi: 10.1002/qj.712
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Intransitive atmosphere dynamics leading to persistent hot-dry or cold-wet European summer
Persistent hot–dry or cold–wet summer weather can have significant impacts on agriculture, health...
R Sperna Weiland, K van der Wiel, F M Selten, D Coumou | Journal: Journal of Climate | Volume: 34 | Year: 2021 | First page: 6303 | Last page: 6317 | doi: 10.1175/JCLI-D-20-0943.1
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