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CMIP5-Derived Single-Forcing, Single-Model, and Single-Scenario Wind-Wave Climate Ensemble: Configuration and Performance Evaluation
Abstract: A Coupled Model Intercomparison Project Phase 5 (CMIP5)-derived single-forcing, single-...
A Semedo, M Dobrynin, G Lemos, A Behrens, J Staneva, H de Vries, AKA Sterl, J Bidlot, PMA Miranda, J Murawski | Status: published | Journal: Journal of Marine Science and Engineering | Volume: 6 | Year: 2018 | First page: 90 | doi: 10.3390/jmse6030090
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The mid‐Cretaceous North Atlantic nutrient trap: Black shales and OAEs
Organic‐rich sediments are the salient marine sedimentation product in the mid‐Cretaceous of the ...
J Trabucho Alexandre, E Tuenter, GA Henstra, KJ van der Zwan, RSW van de Wal, HA Dijkstra, PL de Boer | Status: published | Journal: Paleoceanography | Volume: 25 | Year: 2010 | doi: 10.1029/2010PA001925
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A regional ocean circulation model for the mid-Cretaceous North Atlantic Basin: implications for black shale formation
High concentrations of organic matter accumulated in marine sediments during Oceanic Anoxic Event...
RPM Topper, J Trabucho Alexandre, E Tuenter, PT Meijer | Status: published | Journal: Climate of the Past | Volume: 7 | Year: 2011 | First page: 277 | Last page: 297 | doi: 10.5194/cp-7-277-2011
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A roadmap to climate data rescue services
Quantitative approaches to climate risk management such as mapping or impact modelling rely on pa...
S Brönnimann, Y Brugnara, P Siegmund | Status: published | Journal: Geoscience Data Journal | Volume: 5 | Year: 2018 | First page: 28 | Last page: 39 | doi: 10.1002/gdj3.56
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Quantifying the Effect of Different Urban Planning Strategies on Heat Stress for Current and Future Climates in the Agglomeration of The Hague (The Netherlands)
In the Netherlands, there will be an urgent need for additional housing by the year 2040, which m...
S Koopmans, RJ Ronda, GJ Steeneveld, AAM Holtslag, AMG Klein Tank | Status: published | Journal: Atmosphere | Volume: 9 | Year: 2018 | First page: 353 | doi: https://doi.org/10.3390/atmos9090353
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