Control of the Oceanic Heat Content of the Getz‐Dotson Trough, Antarctica, by the Amundsen Sea Low
Tiago S. Dotto(University of Southampton), Adrian Jenkins(Northumbria University), Michel Tsamados(Centre for Polar Observation and Modelling), Laura Herráiz‐Borreguero(University of Tasmania), Ola Kalén(University of Gothenburg), Paul R. Holland(British Antarctic Survey), Satoshi Kimura(Japan Agency for Marine-Earth Science and Technology), Alberto C. Naveira Garabato(University of Southampton), Anna Wåhlin(University of Gothenburg), Sheldon Bacon(Bangor University)
Cited by 60
Related Papers
Contourites and associated sediments controlled by deep-water circulation processes: State-of-the-art and future considerations
|Marine Geology|2014|793
Sub-ice-shelf sediments record history of twentieth-century retreat of Pine Island Glacier
|Nature|2016|198
SUSTAINED MONITORING OF THE SOUTHERN OCEAN AT DRAKE PASSAGE: PAST ACHIEVEMENTS AND FUTURE PRIORITIES
|Reviews of Geophysics|2011|174
Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century
|Nature Climate Change|2023|155
Inflow of Warm Circumpolar Deep Water in the Central Amundsen Shelf*
|Journal of Physical Oceanography|2010|149