Cold, relatively low salinity water mass found mostly at intermediate depths in the Southern Ocean
Antarctic Intermediate Water (AAIW) is a cold, relatively low salinity water mass found mostly at intermediate depths in the Southern Ocean. The AAIW is formed at the ocean surface in the Antarctic Convergence zone or more commonly called the Antarctic Polar Front zone. This convergence zone is normally located between 50°S and 60°S, hence this is where almost all of the AAIW is formed.
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AntarcticIntermediateWater (AAIW) is a cold, relatively low salinity water mass found mostly at intermediate depths in the Southern Ocean. The AAIW is...
so the water moves down and along the ocean floor. North Atlantic Deep Water (NADW) Circumpolar Deep Water (CDW) AntarcticIntermediateWater (AAIW) Subantarctic...
salty thermocline water, with the remaining 5 Sv being cold, low salinity AntarcticIntermediateWater. Since Indian Ocean water is significantly warmer...
Atlantic Deep Water (NADW), the Antarctic Bottom Water (AABW), AntarcticIntermediateWater (AAIW), as well as recirculated deep water from the Indian...
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)...
Sub-Antarctic Mode Water (SAMW) is an important water mass in Earth's oceans. It is formed near the Sub-Antarctic Front on the northern flank of the Antarctic...
such as Subantarctic Mode Water (SAMW) and AntarcticIntermediateWater (AAIW). Around 22 ± 4 Sv of the total upwelled water in the overturning circulation...
within the Antarctic Circumpolar Current. Within this current, the Subantarctic Mode Water is partially converted to AntarcticIntermediateWater. When the...
Subantarctic Surface Water (Subantarctic Mode Water or SAMW), Antarctic Surface Water, and the AntarcticIntermediateWater). This convergence creates a unique...
major water masses within the system: Upper Circumpolar Water (UCPW), Lower Circumpolar Water (LCPW), Central Water (CW), AntarcticIntermediateWater (AAIW)...
"Evidence from the high-latitude North Atlantic for variations in AntarcticIntermediatewater flow during the last deglaciation". Geochemistry, Geophysics...
South Atlantic central water originates in this gyre, while AntarcticIntermediateWater originates in the upper layers of the circumpolar region, near...
around 23,200 and 22,300 BP. In the western South Atlantic, where AntarcticIntermediateWater forms, sinking particle flux was heightened as a result of increased...
Outflow water depths. This salinity surplus would propagate southwestward, as a mid-depth salinity front, suppressing the supply of fresher Antarctic Intermediate...
resulting in an Agulhas Passage depleted of sediments at this level. AntarcticIntermediateWater flows from Antarctica into the Indian Ocean from where it reaches...
Antarctic Bottom Water (roughly 34.7 psu) and saltier North Atlantic Deep Water. Antarctic Bottom Water can be distinguished from other intermediate and...
ultimately separate ocean water into distinct water masses, such as the North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW). These two waters...
Miyama, Thomas J. Müller 2005 'Pathways and variability of the AntarcticIntermediateWater in the western equatorial Pacific Ocean' Progress in Oceanography...
modified Atlantic water (32%), and intermediatewater from the Nordic seas (20%), that entrain and mix with other water masses (contributing 30%) as they...
mixing with North Atlantic Deep Water (NADW) results in warmer water than other CDW masses. AntarcticIntermediateWater (AAIW) flows above the CDW in the...
Antarctic bottom water – A cold, dense, water mass originating in the Southern Ocean surrounding Antarctica AntarcticIntermediateWater – A cold, relatively...
Sea dense water formation project. In 2005-2006, Talley used hydrography, CTD, and profiling floats to understand AntarcticIntermediateWater formation...
freezing. The dense water that forms in the Arctic are called North Atlantic Deep Water (NADW), while the Antarctic Bottom Water (AABW) forms in the southern...
recrystallized into a substance denser than névé. It is ice that is at an intermediate stage between snow and glacial ice. Firn has the appearance of wet sugar...