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An LES model study of the influence of the free tropospheric thermodynamic conditions on the stratocumulus response to a climate perturbation
Twenty-five large-eddy simulations are performed to study how free tropospheric thermody-
namic c...
JJ van der Dussen, SR de Roode, S Dal Gesso, AP Siebesma | Status: published | Journal: J. of Advances in Modeling Earth Systems | Volume: 7 | Year: 2015 | First page: 670 | Last page: 691 | doi: doi:10.1002/2014MS000380
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A simple model for predicting the statistics of spatiotemporal extremes of sub-daily precipitation
For a single site (of a rain gauge, say), the statistics of extreme precipitation are convenientl...
Cees de Valk, Aart Overeem | Journal: Weather and Climate Extremes | Volume: 36 | Year: 2022 | First page: 1 | Last page: 12 | doi: 10.1016/j.wace.2022.100424
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NWP calibration applied to Aeolus Mie channel winds
Aeolus is the first Doppler wind lidar (DWL) to measure wind profiles from space. Aeolus is an ES...
Gert-Jan Marseille, Jos de Kloe, Uwe Marksteiner, Oliver Reitebuch, Michael Rennie, Siebren de Haan | Journal: Quarterly Journal of the Royal Meteorological Society | Volume: 148 | Year: 2022 | First page: 1020 | Last page: 1034 | doi: https://doi.org/10.1002/qj.4244
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The effect of increased freshwater from Antarctic ice shelves on future trends in Antarctic sea ice
Observations show that, in contrast to the Arctic, the area of Antarctic sea ice has increased si...
R Bintanja, GJ van Oldenborgh, CA Katsman | Status: published | Journal: Annals of Glaciology | Volume: 56 | Year: 2015 | First page: 120 | Last page: 126 | doi: 10.3189/2015AoG69A001
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Estimating seasonal variations in cloud droplet number concentration over the boreal forest from satellite observations
Seasonal variations in cloud droplet number concentration (NCD) in low-level stratiform clouds ov...
RHH Janssen, LN Ganzeveld, P Kabat, M Kulmala, T Nieminen, RA Roebeling | Status: submitted | Journal: Atm. Chem. Phys. | Year: 2011 | First page: 9999 | Last page: 10029 | doi: doi:10.5194/acpd-11-9999-2011
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