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Climate change increases the probability of heavy rains in Northern England/Southern Scotland like those of storm Desmond - a real-time event attribution revisited
On 4–6 December 2015, storm Desmond caused very heavy rainfall in Northern England and Southern S...
FEL Otto, K van der Wiel, GJ van Oldenborgh, S Philip, S Kew, P Uhe, H Cullen | Status: published | Journal: Environmental Research Letters | Volume: 13 | Year: 2018 | First page: 024006 | doi: 10.1088/1748-9326/aa9663
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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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Baseline Surface Radiation Network (BSRN): structure and data description (1992-2017)
Small changes in the radiation budget at the earth's surface can lead to large climatological res...
A Driemel and 38 others, WH Knap | Status: published | Journal: Earth System Science Data | Volume: 10 | Year: 2018 | First page: 1491 | Last page: 1501 | doi: https://doi.org/10.5194/essd-10-1491-2018
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Rainfall retrieval with commercial microwave links in São Paulo, Brazil
In the last decade there has been a growing interest from the hydrometeorological community regar...
MF Rios Gaona, A Overeem, TH Raupach, H Leijnse, R Uijlenhoet | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 11 | Year: 2018 | First page: 4465 | Last page: 4476 | doi: 10.5194/amt-11-4465-2018
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From near-neutral to strongly stratified: adequately modelling the clear-sky nocturnal boundary layer at Cabauw
In this study, the performance of an atmospheric single-column model (SCM) is studied systematica...
Baas, Wiel, Linden, Bosveld | Status: published | Journal: Bound.-Layer Meteorol. | Year: 2017 | doi: 10.1007/s10546-017-0304-8
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