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Observation Based Estimate of Net Community Production in Antarctic Sea Ice Geophysical Research Letters, 2025 (Ref: 17295)
Category 1: Peer-reviewed literature

Antarctic sea ice is one of the largest biomes on Earth providing a critical habitat for ice algae. Measurements of primary production in Antarctic sea ice remain scarce and an observation-based estimate of primary production has not been revisited in over 30 years.

Return of the Maud Rise Polynya: Climate litmus or sea ice anomaly? [In: State of the Climate in 2017] Bulletin of the American Meteorological Society, 2018 (Ref: 17043)
Category 1: Peer-reviewed literature

The Maud Rise polynya is a persistent area of open water within the sea ice cover of the Southern Ocean, which overlies an area of elevated topography called Maud Rise (66°S, 3°E) located in the eastern sector of the Weddell Sea (Fig. SB6.1a).

Polar oceans and sea ice in a changing climate Elementa: Science of the Anthropocene, 2023 (Ref: 16909)
Category 1: Peer-reviewed literature

Polar oceans and sea ice cover 15% of the Earth's ocean surface, and the environment is changing rapidly at both poles. Improving knowledge on the interactions between the atmospheric and oceanic realms in the polar regions, a Surface Ocean–Lower Atmosphere Study (SOLAS) project key focus…

Holocene climate and ecosystem variability on sub-Antarctic Campbell, Macquarie and Marion Islands. International Quaternary Association, University of Bern, Switzerland 21-27 July 2011, 2011 (Ref: 14855)
Category 3: Poster

The sub-Antarctic region between 45-60°S is primarily ocean. However, there are a few small isolated islands, most of which are currently facing the combined pressures of climate change and introduced species.

Holocene climate and ecosystem variability on sub-Antarctic Campbell, Macquarie and Marion Islands. SCAR Biology-EBA Workshop: Antarctic biodiversity: status and trends, University of Liège, Belgium, 31 May 2011, 2011 (Ref: 14854)
Category 3: Poster

The sub-Antarctic region between 45-60 °S is primarily ocean. However, there are a few small isolated islands, most of which are currently facing the combined pressures of climate change and introduced species.

Origin and evolution of the sub-Antarctic islands: the Foundation The sub-Antarctic. Papers and Proceedings of the Royal Society of Tasmania, 2007 (Ref: 13527)
Authors:
Category 1: Peer-reviewed literature

Sub-Antarctic islands have a diversity of origins in detail but most are volcanic and very young suggesting that they are short-lived and that the distribution would have been very different a few million years ago. They contrast with the common tourist brochure concept of oceanic islands.

Report by the Taxonomy Working Group to the fourth meeting of the ACAP Advisory Committee - Cape Town, South Africa 2007. AC4 Doc12 Fourth Meeting of the ACAP Advisory Committee. Agreement on the Conservation of Albatrosses and Petrels (ACAP), 2008 (Ref: 13539)
Category 2: International meeting papers

This report presents the application of the taxonomic guidelines developed by the … Taxonomy Working Group to three pairs of taxa currently listed under Annex 1 … (Attachment 1) of the Agreement on the Conservation of Albatrosses and Petrels … (ACAP): 1. Amsterdam and Wandering Albatross…

Fronts and transport variability of the Antarctic Circumpolar Current south of New Zealand. Abstracts from the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12604)
Category 3: Poster

Twenty one XBT sections across the Antarctic Circumpolar Current (ACC) between New … Zealand and Antarctica, collected in the frame of the Italian CLIMA project (1994-2006), are … used to study the upper ocean thermal structure and to infer the baroclinic transport. The … Subantarctic Front (SAF)…

Fonts and upper ocean thermal variability couth of New Zealand. Antarctic Science, 2003 (Ref: 12070)
Category 1: Peer-reviewed literature

Abstract: The structure and variability of Southern Ocean fronts south of New Zealand are described based … on fifteen summer expendable bathythermograph (XBT) sections obtained between 1994 and 2001.

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