
Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Atmosferisch Onderzoek
Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Atmosferisch Onderzoek
4 Projects, page 1 of 1
assignment_turned_in Project2014 - 2017Partners:University of Utah, Geological Survey of Denmark and Greenland (GEUS), Universiteit Utrecht, NWO-JSTP-China, Université de Liège +11 partnersUniversity of Utah,Geological Survey of Denmark and Greenland (GEUS),Universiteit Utrecht,NWO-JSTP-China,Université de Liège,Université de Liège,Technische Universiteit Delft, Faculteit Luchtvaart- en Ruimtevaarttechniek, Astrodynamics and Satellite Systems (AS),NWO-JSTP-China,Ministerie van Infrastructuur en Waterstaat,Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Klimaatonderzoek en Seismologie,Technische Universiteit Delft,Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Atmosferisch Onderzoek,Geological Survey of Denmark and Greenland (GEUS),University of Utah,Universiteit Utrecht, Faculteit Bètawetenschappen, Departement Natuurkunde, Instituut voor Marine en Atmosferisch onderzoek (IMAU),Technische Universiteit Delft, Faculteit Civiele Techniek en Geowetenschappen, Afdeling Geoscience & Remote Sensing (GRS)Funder: Netherlands Organisation for Scientific Research (NWO) Project Code: 866.12.403An estimated 60% of the presently observed sea level rise is attributed to melting glaciers, ice caps and ice sheets. The contribution of Arctic glaciers and especially the Greenland ice sheet (GrIS) has more than doubled over the period 1961-2008, and is likely to increase further when global temperature increases over the coming century. A first order effect of increasing temperatures on the glacier mass budget is an increase in surface melt. However, not all melt contributes to mass loss via runoff, because part of the meltwater refreezes in the cold snow. For the GrIS, an estimated 30-50% of all meltwater refreezes. Infiltration of water and subsequent refreezing is not well included in existing mass balance models, and estimates of refreezing are not well validated due to a lack of observations. Given the importance of refreezing for the mass budget of Arctic glaciers, in this proposal we focus on improving refreezing estimates for the GrIS and therewith other Arctic ice masses, by using a combined observational and modelling approach. Existing satellite and in-situ observations, complemented with detailed snow temperature observations to be carried out in western Greenland (K-transect), will be used to evaluate the mass balance terms and refreezing modelled with the regional climate model RACMO2, which includes a multi-layer snow model. After improvements to the snow model have been implemented and evaluated, RACMO2 will be run for the period 1958-present-2100 in order to study the role of refreezing in the mass balance of the GrIS in a changing climate.
more_vert assignment_turned_in Project2014 - 2019Partners:NWO-institutenorganisatie, NIOZ - Koninklijk Nederlands Instituut voor Onderzoek der Zee, Deltares, Onbekend, Technische Universiteit Delft, Universiteit Utrecht, Faculteit Bètawetenschappen, Departement Natuurkunde, Meteorologie & Fysische Oceanografie +8 partnersNWO-institutenorganisatie, NIOZ - Koninklijk Nederlands Instituut voor Onderzoek der Zee,Deltares,Onbekend,Technische Universiteit Delft,Universiteit Utrecht, Faculteit Bètawetenschappen, Departement Natuurkunde, Meteorologie & Fysische Oceanografie,Technische Universiteit Delft,Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Atmosferisch Onderzoek,NWO-institutenorganisatie,Universiteit Utrecht,Ministerie van Infrastructuur en Waterstaat,Deltares, Deltares, Locatie Utrecht,Onbekend,Universiteit Utrecht, Faculteit Bètawetenschappen, Departement Natuurkunde, Instituut voor Marine en Atmosferisch onderzoek (IMAU)Funder: Netherlands Organisation for Scientific Research (NWO) Project Code: 866.13.001Up to now most sea level projection where mainly for the global scale and did not consider the probability density functions in much detail. This is not sufficient for coastal management where projections for local rise are needed. Moreover for risk analyses it is important to study the extreme values, which may have only a small probability. Recent work indicates that in particular the changes in the dynamics of ice sheets may lead to skewed distributions, which need to be taken into account in total local projections of sea level. New developments in sea level research enable the start of the construction of probability density functions for the North-Sea region based on CMIP5 ensemble results. Updated calculations of the contribution of thermal expansion, glaciers and ice sheets, groundwater depletion, air pressure differences and changing wind and wave patterns will be combined in a sea level equation model that accounts for gravitational and rotational effects of the changes in mass in the ocean. Results will be validated with local data for the North-Sea region, corrected for tidal effects in order to attribute sea level changes and increase the reliability of future projections. The end result are trends and the variability in the trend of local sea level rise including a probability density function, which can be used for coastal management purposes.
more_vert assignment_turned_in ProjectFrom 2025Partners:Universiteit Leiden, Faculteit der Wiskunde en Natuurwetenschappen, Centrum voor Milieuwetenschappen, Vrije Universiteit Amsterdam, Faculteit der Bètawetenschappen (Faculty of Science), Afdeling Aardwetenschappen (Department of Earth Sciences), NWO-institutenorganisatie, SRON - Netherlands Institute for Space Research, Wageningen University & Research, Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Atmosferisch Onderzoek +4 partnersUniversiteit Leiden, Faculteit der Wiskunde en Natuurwetenschappen, Centrum voor Milieuwetenschappen,Vrije Universiteit Amsterdam, Faculteit der Bètawetenschappen (Faculty of Science), Afdeling Aardwetenschappen (Department of Earth Sciences),NWO-institutenorganisatie, SRON - Netherlands Institute for Space Research,Wageningen University & Research,Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Atmosferisch Onderzoek,Copernicus Institute for Sustainable Development,Universiteit Twente, Faculty of Geo-Information Science and Earth Observation (ITC), Water Resources (WRS),Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut,Wageningen University & Research, Afdeling OmgevingswetenschappenFunder: Netherlands Organisation for Scientific Research (NWO) Project Code: ENW.GO.001Wildfires impact ecosystems, air quality, and the climate, with human activities and climate change making them more intense. The INFLAMES project takes an interdisciplinary approach, combining Dutch atmospheric satellite data, computer models, and field research to understand how wildfires evolve and affect the environment around the world. Experts from climate science, ecology, and social sciences work together to study how fire emissions influence air pollution, vegetation, and future climate patterns. By integrating these perspectives, INFLAMES aims to improve wildfire predictions and inform strategies to manage their risks in a changing world.
more_vert assignment_turned_in Project2023 - 9999Partners:Technische Universiteit Delft, Faculteit Civiele Techniek en Geowetenschappen, Afdeling Geoscience & Remote Sensing (GRS), Technische Universiteit Delft, Faculteit Elektrotechniek, Wiskunde en Informatica, Technische Universiteit Eindhoven - Eindhoven University of Technology, Centrum Bouwonderzoek (TNO-TUE), Technische Universiteit Delft, Faculteit Elektrotechniek, Wiskunde en Informatica, Microelectronics, NWO-institutenorganisatie, ASTRON - Netherlands Institute for Radio Astronomy +19 partnersTechnische Universiteit Delft, Faculteit Civiele Techniek en Geowetenschappen, Afdeling Geoscience & Remote Sensing (GRS),Technische Universiteit Delft, Faculteit Elektrotechniek, Wiskunde en Informatica,Technische Universiteit Eindhoven - Eindhoven University of Technology, Centrum Bouwonderzoek (TNO-TUE),Technische Universiteit Delft, Faculteit Elektrotechniek, Wiskunde en Informatica, Microelectronics,NWO-institutenorganisatie, ASTRON - Netherlands Institute for Radio Astronomy,Technische Universiteit Eindhoven - Eindhoven University of Technology,TNO Den Haag,Rijksuniversiteit Groningen,Technische Universiteit Delft, Faculteit Civiele Techniek en Geowetenschappen, Afdeling Watermanagement, Water Resources,Robin Radar Systems,Robin Radar Systems,Technische Universiteit Delft, Faculteit Elektrotechniek, Wiskunde en Informatica, Microelectronics, Elektronische Instrumentatie,Rijksuniversiteit Groningen, Faculty of Science and Engineering (FSE), Energy and Sustainability Research Institute Groningen (ESRIG), Centre for Isotope Research (CIO),Technische Universiteit Delft, Faculteit Elektrotechniek, Wiskunde en Informatica, Microwave Sensing, Signals and Systems (MS3),Technische Universiteit Delft, Faculteit Civiele Techniek en Geowetenschappen,TNO Rijswijk,Ministerie van Infrastructuur en Waterstaat,Technische Universiteit Delft,Technische Universiteit Eindhoven - Eindhoven University of Technology,Ministerie van Infrastructuur en Waterstaat, Koninklijk Nederlands Meteorologisch Instituut, Atmosferisch Onderzoek,NWO-institutenorganisatie,TNO Den Haag, Fysisch en Elektronisch Laboratorium,TNO Rijswijk,Technische Universiteit Eindhoven - Eindhoven University of Technology, Faculteit Electrical Engineering - Department of Electrical Engineering, Electromagnetics (EM)Funder: Netherlands Organisation for Scientific Research (NWO) Project Code: 175.2021.038How do we prepare for increasingly extreme weather conditions? The answer to this question is hidden in an essential part of our climate system: clouds. Researchers will develop a new type of radar that can observe the whole sky in a matter of seconds. It is designed to both reveal how particles grow inside clouds and precipitation and to track large-scale movements of weather systems. The transportable radar will contribute to breakthroughs in climate and atmospheric research, more precise weather forecasts (crucial for water management) and further (radar) innovations.
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