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Learn more about Bing search results hereOrganizing and summarizing search results for youAntarctic bottom water (AABW) is a cold, dense water mass in the Southern Ocean surrounding Antarctica. It has temperatures ranging from −0.8 to 2 °C (35 °F) and absolute salinities from 34.6 to 35.0 g/kg. Bottom water consists of cold, dense water near the ocean floor, characterized by low salinity and nutrient content. Bottom water produced in the Antarctic is characterized by low salinity from seasonal ice melt and freshwater river output.2 Sources
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See all on WikipediaAntarctic bottom water - Wikipedia
The Antarctic bottom water (AABW) is a type of water mass in the Southern Ocean surrounding Antarctica with temperatures ranging from −0.8 to 2 °C (35 °F) and absolute salinities from 34.6 to 35.0 g/kg. As the densest water mass of the oceans, AABW is found to occupy the depth range below 4000 m of all … See more
Antarctic bottom water is formed in the Weddell and Ross Seas, off the Adélie Coast and by Cape Darnley from surface water cooling in polynyas and below the ice shelf. … See more
Climate change and the subsequent melting of the Southern ice sheet have slowed the formation of AABW, and this slowdown is likely to continue. A complete shutdown of AABW formation is possible as soon as 2050. This shutdown would have dramatic … See more
Wikipedia text under CC-BY-SA license Bottom water - Wikipedia
Bottom water consists of cold, dense water near the ocean floor. This water is characterized by low salinity and nutrient content. Generally, low salinity from seasonal ice melt and freshwater river output characterizes bottom water produced in the Antarctic. However, during colder months, the formation of sea ice is a crucial process that raises the salinity of bottom water through brine rejection. As saltwater freezes, salt is expelled from the ice into the surrounding water. The oxy…
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Weddell Sea Bottom Water - Wikipedia
Weddell Sea Bottom Water (WSBW) is a subset of Antarctic Bottom Water (AABW) that is at a temperature of -0.7 °C or colder. It consists of a higher salinity branch and a lower salinity branch.
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Antarctic Bottom Water | oceanography | Britannica
Antarctic bottom water is an important water mass that forms on the Antarctic continental shelf as a cold, dense residual brine during the formation of sea ice. Its salinity of 34.62 parts per thousand and temperature of -1.9° C (28.6° F) …
Antarctic Bottom Water - an overview | ScienceDirect Topics
Antarctic bottom water (AABW) is the densest global-scale water mass. It is produced around Antarctica, sinks along the Antarctic continental slope and spreads northward to fill most of the …
Antarctic Bottom Water - Glossary of Meteorology
A water mass formed by deep winter convection at the coast of Antarctica, particularly in the Weddell and Ross Seas but also at other shelf locations.
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Antarctic bottom water - Oxford Reference
A dense bottom-water mass, formed in the Weddell and Ross Seas, which moves in an easterly direction around Antarctica under the influence of the deep-reaching, wind-driven, surface …
Antarctic Bottom Waters Freshening at Unexpected Rate
Jan 25, 2017 · Known as the Antarctic Bottom Waters (AABW), these deep, cold waters play a critical role in regulating circulation, temperature, and availability of oxygen and nutrients throughout the world’s oceans.
Quo vadis Antarctic bottom water? - ScienceDaily
Jan 22, 2020 · There, the so-called Antarctic Bottom Water (AABW) is formed. While today AABW is circulating northwards into the other ocean basins, results of a new study show, that this …
Climate Change Felt in Deep Waters of Antarctica
Mar 3, 2014 · Antarctic Bottom Water spreads across the global oceans at depths of 3,000 meters and more, delivering oxygen into these deep places. It’s also one of the drivers of global thermohaline...
Southern Ocean overturning circulation - Wikipedia
Southern Ocean overturning circulation (sometimes referred to as the Southern Meridional overturning circulation (SMOC) [1] or Antarctic overturning circulation) is the southern half of a …
Antarctic Bottom Water - Encyclopedia.com
May 8, 2018 · Antarctic bottom water (AABW) A dense bottom-water mass, formed in the Weddell and Ross Seas, which moves in an easterly direction around Antarctica under the influence of …
Scientists discover hidden 'plumbing' that's driving Antarctic ice ...
Feb 5, 2025 · The maps show the water networks beneath Antarctica, revealing a steady discharge of water through channels above the bedrock. (Image credit: Shivani Ehrenfeucht et …
What you need to know about Antarctic Bottom Water
Jan 17, 2025 · Put simply, Antarctic Bottom Water is dense, cold, oxygen-rich water that forms in just a few places around the Antarctic continent. This water forms as cold winds blowing off …
In search of Antarctic Bottom Water - AAPP
It’s one of four formation sites of Antarctic Bottom Water, the world’s densest water mass that fills much of the global ocean abyss and drives currents around the planet. Open-water areas …
Antarctica - Wikipedia
Antarctica was adopted in the 1890s, with the first use of the name being attributed to the Scottish cartographer John George Bartholomew. ... (GT) per year of meltwater from the ice dilutes the …
Antarctic Bottom Water - (Earth Systems Science) - Fiveable
Antarctic Bottom Water is a dense, cold water mass that forms around Antarctica and sinks to the ocean floor, playing a crucial role in global ocean circulation.
Antarctic Bottom Water - scientificlib.com
The 'Antarctic Bottom Water' (AABW) is a type of water mass in the seas surrounding Antarctica with temperatures ranging from 0 to -0.8 C, salinities from 34.6 to 34.7 psu, and a density near …
Southern Ocean - Wikipedia
The Southern Ocean, also known as the Antarctic Ocean, [1] [note 4] comprises the southernmost waters of the world ocean, generally taken to be south of 60° S latitude and encircling …
Antarctic Bottom Water - (Marine Biology) - Fiveable
Antarctic Bottom Water (ABW) is a dense, cold water mass that forms in the Southern Ocean near Antarctica, primarily due to the cooling and sinking of surface waters. This process contributes …
Why is the Antarctic Bottom Water so dense? - Answers
3 days ago · Antarctic Bottom Water is dense because it forms in the frigid waters around Antarctica, where the cold temperatures cause the water to become very cold and salty. This …
Antarctic lakes - Wikipedia
Antarctica also has some relatively small regions that are clear of ice and snow, and there are some surface lakes in these regions. ... When a glacier is very thick, the pressure at the …
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