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Basal conditions of Denman Glacier from glacier hydrology and ice dynamics modeling. The Cryosphere, 2023 (Ref: 17133)
Category 1: Peer-reviewed literature

Basal sliding in Antarctic glaciers is often modeled using a friction law that relates basal shear stresses to the effective pressure. As few ice sheet models are dynamically coupled to subglacial hydrology models…

Evaluating the 20th Century Reanalysis Version 3 with synoptic typing and an East Antarctic ice core accumulation record Climate of the Past, 2025 (Ref: 17306)
Category 1: Peer-reviewed literature

Weather systems in the southern Indian Ocean influence East Antarctic precipitation variability and surface mass balance. However…

A Novel Method for Using Small Unoccupied Aerial Vehicles to Survey Wildlife Species and Model Their Density Distribution Frontiers in Marine Science, 2021 (Ref: 16720)
Category 1: Peer-reviewed literature

There is growing interest from research and conservation groups in the potential for using small unoccupied aerial vehicles (UAVs; <2 kg) to conduct wildlife surveys because they are affordable, easy to use, readily available and reliable. However, limitations such as short flight endurance…

Under the sea ice: Exploring the relationship between sea ice and the foraging behaviour of southern elephant seals in East Antarctica Progress in Oceanography, 2017 (Ref: 17050)
Category 1: Peer-reviewed literature

Investigating ecological relationships between predators and their environment is essential to understand the response of marine ecosystems to climate variability and change. This is particularly true in polar regions, where sea ice (a sensitive climate variable)…

Identifying atmospheric processes favouring the formation of bubble-free layers in the Law Dome ice core, East Antarctica The Cryosphere, 2023 (Ref: 17028)
Category 1: Peer-reviewed literature

Physical features preserved in ice cores may provide unique records about past atmospheric variability. Linking the formation and preservation of these features and the atmospheric processes causing them is key to their interpretation as palaeoclimate proxies. We imaged ice cores from Law Dome…

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