No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum [PDF]
The Southern Ocean plays a key role in glacial-interglacial transitions and today, Weddell Sea derived Antarctic Bottom Water is one of the most important deep water masses.
Huang Huang +3 more
doaj +3 more sources
Age distribution of Antarctic Bottom Water off Cape Darnley, East Antarctica, estimated using chlorofluorocarbon and sulfur hexafluoride [PDF]
Chlorofluorocarbon (CFC) and sulfur hexafluoride (SF6) were used to investigate the timescale of Antarctic Bottom Water (AABW) that spreads off Cape Darnley (CD) in East Antarctica. The age of the AABW was estimated based on the observed SF6/CFC-12 ratio
Yoshihiko Ohashi +4 more
doaj +3 more sources
Circum-Antarctic bottom water formation mediated by tides and topographic waves [PDF]
The downslope plumes of dense shelf water (DSW) are critical for the formation of Antarctic Bottom Water (AABW), and thus to the exchange of heat and carbon between surface and abyssal ocean.
Xianxian Han +6 more
doaj +3 more sources
The suppression of Antarctic bottom water formation by melting ice shelves in Prydz Bay [PDF]
Antarctic bottom water (AABW) production is critical to the global ocean overturning circulation. Here, the authors show new observations of AABW formation from seal CTD data in Prydz Bay, East Antarctica that highlights its susceptibility to increased ...
G. D. Williams +11 more
doaj +3 more sources
Tides regulate the flow and density of Antarctic Bottom Water from the western Ross Sea. [PDF]
Antarctic Bottom Water (AABW) stores heat and gases over decades to centuries after contact with the atmosphere during formation on the Antarctic shelf and subsequent flow into the global deep ocean.
Bowen MM +8 more
europepmc +2 more sources
Dominant frazil ice production in the Cape Darnley polynya leading to Antarctic Bottom Water formation. [PDF]
Antarctic Bottom Water (AABW) occupies the abyssal layer of the world ocean and contributes to the global overturning circulation. It originates from dense shelf water, which forms from brine rejection during sea ice production.
Ohshima KI +8 more
europepmc +2 more sources
Observing Antarctic Bottom Water in the Southern Ocean
Dense, cold waters formed on Antarctic continental shelves descend along the Antarctic continental margin, where they mix with other Southern Ocean waters to form Antarctic Bottom Water (AABW).
Alessandro Silvano +56 more
doaj +2 more sources
Improving Antarctic Bottom Water precursors in NEMO for climate applications [PDF]
The world's largest ice shelves are found in the Antarctic Weddell Sea and Ross Sea where complex interactions between the atmosphere, sea ice, ice shelves and ocean transform shelf waters into High Salinity Shelf Water (HSSW) and Ice Shelf Water (ISW ...
K. Hutchinson +7 more
doaj +2 more sources
Reversal of freshening trend of Antarctic Bottom Water in the Australian-Antarctic Basin during 2010s. [PDF]
The Antarctic continental margin supplies the densest bottom water to the global abyss. From the late twentieth century, an acceleration in the long-term freshening of Antarctic Bottom Waters (AABW) has been detected in the Australian-Antarctic Basin ...
Aoki S +7 more
europepmc +2 more sources
A decadal warming trend of 2.1 (±0.2) m°C yr−1 in Antarctic Bottom Water within the western Argentine Basin is found by comparing Deep Argo temperature profiles from 2021 to 2022 to nearby historical shipboard data from 1972 to 1998.
Gregory C. Johnson
doaj +2 more sources

