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Attributing drivers of the 2016 Kenyan drought
In 2016 and continuing into 2017, Kenya experienced drought conditions, with over 3 million peopl...
P Uhe, AY Philip, SF Kew, K Shah, J Kimutai, E Mwangi, GJ van Oldenborgh, R Singh, J Arrighi, E Jjemba, H Cullen, FEL Otto | Status: published | Journal: Int. J. Climatology | Volume: 38 | Year: 2018 | First page: e554 | Last page: e568 | doi: 10.1002/joc.5389
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Modelling the climate and surface mass balance of polar ice sheets using RACMO2 – Part 2: Antarctica (1979–2016)
We evaluate modelled Antarctic ice sheet (AIS) near-surface climate, surface mass balance (SMB) a...
JM van Wessem, WJ van de Berg, BPY Noël, E van Meijgaard, LH van Ulft, MR van den Broeke, 13 CoAuthors | Status: published | Journal: The Cryosphere | Year: 2018 | First page: 1479 | Last page: 1498 | doi: 10.5194/tc-12-1479-2018
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Shallow crustal imaging using distant, high-magnitude earthquakes
Global phases, viz. seismic phases that travel through the Earth’s core, can be used to locally i...
J van IJsseldijk, EN Ruigrok, A Verdel, C Weemstra | Status: published | Journal: Geophys. J. Int. | Volume: 219 | Year: 2019 | First page: 1082 | Last page: 1091 | doi: 10.1093/gji/ggz343
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Evaluation of rainfall products derived from satellites and microwave links for The Netherlands
High-resolution inputs of rainfall are important in hydrological sciences, especially for urban h...
Rios Gaona, Overeem, Brasjen, Meirink, Leijnse, Uijlenhoet | Status: published | Journal: IEEE Transactions on Geoscience and Remote Sensing | Volume: 55 | Year: 2017 | First page: 6849 | Last page: 6859 | doi: 10.1109/TGRS.2017.2735439
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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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