Abstract Global ocean circulation regulates climate and has undergone significant changes over the Cenozoic. Today, the Atlantic Meridional Overturning Circulation (AMOC) is driven by North Atlantic Deep Water (NADW) formation and Southern Ocean upwelling.
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Azimuthal sensitivity and spatio-temporal decimation of data from distributed acoustic sensing on submarine cables for offshore earthquake early warning systems. [PDF]
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Bathymetry estimation for coastal regions using self-attention. [PDF]
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Geoelectrical evidence of fluid controlling slow and regular earthquakes along a plate interface. [PDF]
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Marine Heatwave Event Maps in the Baltic Sea (1982-2023): A Gridded Dataset from Satellite-Derived L4 SST. [PDF]
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Presence of continental slivers in oceanic transform faults determined by rift inheritance. [PDF]
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Diversity of coatings on hydrothermal vent gastropods. [PDF]
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