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Modelling the climate and surface mass balance of polar ice sheets using RACMO2 – Part 1: Greenland (1958–2016)
We evaluate modelled Greenland ice sheet (GrIS) near-surface climate, surface energy balance (SEB...
BPY Noël, WJ van de Berg, JM van Wessem, E van Meijgaard, LH van Ulft, MR van den Broeke, 6 CoAuthors | Status: published | Journal: The Cryosphere | Year: 2018 | First page: 811 | Last page: 831 | doi: 10.5194/tc-12-811-2018
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A study on the ambient noise field at a hydroacoustic array near Robinson Crusoe Island
Continuous long-term sound sources are recorded at hydroacoustic station H03S, a threeelement hyd...
KAM Sambell, PSM Smets, DG Simons, M Snellen, LG Evers | Status: published | Journal: Geophys. J. Int. | Volume: 218 | Year: 2019 | First page: 88 | Last page: 99 | doi: https://doi.org/10.1093/gji/ggz124
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Constraints on the geomorphological evolution of the nested summit craters of Láscar volcano from high spatio-temporal resolution TerraSAR-X interferometry
Small-scale geomorphological changes that are associated with the formation, development, and act...
N Richter, JT Salzer, E De Zeeuw-van Dalfsen, D Perissin, TR Walter | Status: published | Journal: Bull Volcanol | Volume: 80 | Year: 2018 | First page: 1 | Last page: 17 | doi: 10.1007/s00445-018-1195-3
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Identifying the Origin of Anomalous High Tropospheric Ozone in the Ozonesonde Data at Uccle by Comparison with Nearby De Bilt
The ozonesonde stations at Uccle (Belgium) and De Bilt (Netherlands), separated by only 175 km, o...
R van Malderen, H de Backer, A Delcloo, M Allaart | Journal: Atmosphere-Ocean | Volume: 0 | Year: 2014 | First page: 1 | Last page: 15 | doi: 10.1080/07055900.2014.886552
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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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