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Field
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proxy data reflecting surface ocean changes, and simulations of sea level changes using comprehensive ice sheet models. The sea level in the Eemian was much higher than today, 3 to 6 m or even higher
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, funded by NWO, EMBRACER brings together a wide range of world-leading climate experts with the aim to address existing uncertainties about climate feedbacks at the boundaries between oceans, land, ice, and
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in atmospheric temperatures. The increase in freshwater inputs into the ocean are likely linked to changes in biological productivity, either through the resulting physical changes to the water column
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Carbon (POC) and bury this in deposits below the ocean floor. They additionally convey abundant nutrients and oxygenated water masses, which together with the POC (as food) support conditions for abundant
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The increasing size of offshore wind turbines, and wind farms, raises the question as to how they interact with the Marine Boundary Layer (MBL) which is the layer of the atmosphere immediately adjacent to the sea
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Job posting (PHY 09/2025) The Leibniz Institute for Baltic Sea Research Warnemünde (IOW) has a temporary vacancy for a PhD candidate in High Resolution Ecosystem Modeling and application
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Vulnerability of the Greenland Ice Sheet (GIS) to current climate warming, which could provide c. 7 m of dangerous sea-level rise if it melted completely, is a first-order global concern. GIS melt
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Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung | Bremerhaven, Bremen | Germany | 9 days ago
opportunity to decarbonize the transportation and chemical industries while enhancing marine biodiversity. The Ocean Gardens project pioneers offshore regenerative seaweed farming across European waters
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the city. Barcelona is very well connected by air, sea and ground transportation. The region of Catalonia has its own AI strategy, in which the CVC is a key player. CONTRACT CONDITIONS Location: Computer
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interactions with the ocean and the atmosphere. The properties that characterize it have been established through the analysis of satellite observations over a scale range from 10km to approximately 1000km, and