Expansion of Antarctic sea ice combined with ocean circulation changes sequesters carbon in the ocean abyss, causing a decline in atmospheric carbon dioxide during glacial periods.
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Expansion of Antarctic sea ice combined with ocean circulation changes sequesters carbon in the ocean abyss, causing a decline in atmospheric carbon dioxide during glacial periods.
Submesoscale feedback reduces marine heatwave severity by up to 18.1% in a global model simulation.
Surface warming accelerations since 1970 are concentrated mainly in mid-latitudes of the Northern Hemisphere, with variable onset times from the 1980s to 2010s.
AI-based WeatherNext Cyclones (WN-C) improves tropical cyclone forecasts by over one day in lead time, achieving state-of-the-art accuracy with large ensembles.
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