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Antarctic Bottom Water in a changing climate Nature Reviews: Earth & Environment, 2025 (Ref: 17477)
Category 1: Peer-reviewed literature

Antarctic Bottom Water (AABW) is derived from dense water that sinks from the Antarctic continental shelf to the deep ocean. The sinking of AABW is balanced by a return flow of lighter water, and the resulting overturning circulation determines the density stratification of the deep ocean…

Algal enrichment process for newly formed sea ice in the Dalton polynya off East Antarctica during the late summer–early autumn Elementa: Science of the Anthropocene, 2025 (Ref: 17345)
Category 1: Peer-reviewed literature

Newly formed sea ice can incorporate considerable amounts of organic matter including phytoplankton during its freezing and growth. This initial incorporation influences the standing stocks of ice algae, a fundamental component of high-latitude marine ecosystems.

On-shelf circulation of warm water toward the Totten Ice Shelf in East Antarctica. Nature Communications, 2023 (Ref: 17117)
Category 1: Peer-reviewed literature

The Totten Glacier in East Antarctica, with an ice volume equivalent to >3.5?m of global sea-level rise, is grounded below sea level and, therefore, vulnerable to ocean forcing. Here…

Modeling Ocean–Cryosphere Interactions off Adélie and George V Land, East Antarctica Journal of Climate, 2017 (Ref: 17048)
Category 1: Peer-reviewed literature

Ocean–cryosphere interactions along the Adélie and George V Land (AGVL) coast are investigated using a coupled ocean–sea ice–ice shelf model. The dominant feature of the Mertz Glacier Tongue (MGT), located at approximately 145°E, was a highly productive winter coastal polynya system…

Interdecadal water mass changes in the Southern Ocean between 30°E and 160°E Geophysical Research Letters, 2005 (Ref: 13293)
Category 1: Peer-reviewed literature

Interdecadal water mass changes in the Indian -Western … Pacific sectors of the Southern Ocean were investigated … using the Japanese Antarctic Research Expeditions and … historical hydrographic observations from the 1950s to … 1990s.

A series of cyclonic eddies in the Antarctic Divergence off Adélie Coast Journal of Geophysical Research, 2007 (Ref: 13383)
Category 1: Peer-reviewed literature

The spatial and temporal characteristics of cyclonic eddies in the Antarctic … Divergence off Ade´lie Coast are described using repeated in situ observations between … 2001 and 2003, satellite observations, and results of a high-resolution ocean general … circulation model.

Frontal positions and mixed layer evolution in the Seasonal Ice Zone along 140°E in 2001/02 Polar Bioscience, 2006 (Ref: 13386)
Category 1: Peer-reviewed literature

We describe the circulation and seasonal development of the upper ocean … in the Seasonal Ice Zone (SIZ) of the Southern Ocean along 140°E. The 140°E section … was repeated four times between November 2001 and March 2002, spanning the period … from early spring to autumn.

Freshening of the Adélie Land Bottom Water near 140°E. Geophysical Research Letters, 2005 (Ref: 12608)
Category 1: Peer-reviewed literature

Repeat summer hydrographic observations along … 140E are used to document significant changes in the … properties of the Ade´lie Land Bottom Water (ALBW) between the mid-1990s and 2002–2003. Water on the 28.35 … kgm3 neutral density surface cooled by 0.2C and … freshened by 0.

Oceanography along East Antarctica (30-80º E) during the BROKE-West survey (CCAMLR Area 58.4.2) in the Austral summer of 2006. Abstracts from the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12606)
Category 3: Abstract

A second East Antarctic Baseline Regional Oceanography Krill and Environment survey, termed BROKE-West, was conducted January 10th – February 25th 2006 and covered … CCAMLR Area 58.4.2 west of the Princess Elizabeth Trough in the Weddell-Enderby Basin.

Eddies revealed by SeaWiFS ocean colour images in the Antarctic Divergence zone near 140°E. Geophysical Research Letters, 2003 (Ref: 12063)
Category 1: Peer-reviewed literature

Eddy-like distributions of chlorophyll a were clearly … detected in the Antarctic Divergence zone around 140E … by SeaWiFS ocean color images. The distribution was also … supported by in-situ measurements.

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