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Influence of the grounding zone on the internal structure of ice shelves Nature Communications, 2025 (Ref: 17318)
Category 1: Peer-reviewed literature

Antarctic ice shelves typically comprise continental meteoric ice, in situ-accumulated meteoric ice, and marine ice accumulated at the shelf base. Using borehole optical televiewer logs from across Larsen C Ice Shelf, Antarctic Peninsula, we identify and report an intermediate ice unit…

Imaging Brine Infiltration and Basal Marine Ice in Larsen C Ice Shelf, Antarctic Peninsula, From Borehole Measurements and Transient Electromagnetics Geophysical Research Letters, 2025 (Ref: 17440)
Category 1: Peer-reviewed literature

The presence and nature of marine ice in ice shelves is important, yet difficult to determine. We present transient electromagnetic results spanning 10 km across a suture zone of Larsen C Ice Shelf (LCIS), Antarctica, supported by central borehole measurements.

Imaging Brine Infiltration and Basal Marine Ice in Larsen C Ice Shelf, Antarctic Peninsula, From Borehole Measurements and Transient Electromagnetics Geophysical Research Letters, 2025 (Ref: 17474)
Category 1: Peer-reviewed literature

The presence and nature of marine ice in ice shelves is important, yet difficult to determine. We present transient electromagnetic results spanning 10 km across a suture zone of Larsen C Ice Shelf (LCIS), Antarctica, supported by central borehole measurements.

Influence of the grounding zone on the internal structure of ice shelves Nature Communications, 2025 (Ref: 17338)
Category 1: Peer-reviewed literature

Antarctic ice shelves typically comprise continental meteoric ice, in situ-accumulated meteoric ice, and marine ice accumulated at the shelf base. Using borehole optical televiewer logs from across Larsen C Ice Shelf, Antarctic Peninsula, we identify and report an intermediate ice unit…

High-resolution elevation models of Larsen B glaciers extracted from 1960s imagery Scientific Reports, 2024 (Ref: 17265)
Category 1: Peer-reviewed literature

Accelerated warming since the 1950s has caused dramatic change to ice shelves and outlet glaciers on the Antarctic Peninsula. Long observational records of ice loss in Antarctica are rare but essential to accurately inform mass balance estimates of glaciers. Here…

Monitoring the Polar Stratospheric Clouds Evolution in Antarctica by Combining Lidar Measurements, the Lagrangian MATCH Approach, and Microphysical Modelling International Polar Year Conference (OSC-2010, Oslo Norway June 8-12 2010), 2010 (Ref: 14178)
Category 3: Poster

As part of the global project ORACLE-O3 selected for the IPY, LOLITA-PSC (“Lagrangian Observations with Lidar Investigations and Trajectories in Antarctica and Arctic, of PSC”) is devoted to Polar Stratospheric Clouds (PSCs) studies. Indeed…

Model derived dynamics, basal melt and time evolution of The Mertz Glacier Tongue, East Antarctica Abstracts of the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12571)
Category 3: Abstract

Recent research indicates extensive basal melting near the deep grounding lines of major … Antarctic outlet glaciers. Further…

East Antarctic ice shelves: Status quo or decline? Abstracts of the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12498)
Category 3: Poster

The collapse of the Larsen A and B and other ice shelves fringing the Antarctic Peninsula … coastline raises questions about the status of ice shelves in other parts of the continent. Are … the large ice shelves along the East Antarctic coast also in danger of permanent collapse…

Arsenic speciation in estuarine and oceanic waters by hydride generation - atomic fluorescence spectroscopy , 1999 (Ref: 9187)
Category 3: Thesis, higher degree

A method has been developed for the routine determination of four arsenic species (arsenite, arsenate, monomethylarsenic and dimethylarsenic) in natural water, and has been applied to a study of arsenic cycling in open ocean (Atlantic and Southern Ocean) and estuarine (Huon Estuary, Tasmania)…

Breakup and conditions for stability of the northern Larsen Ice Shelf, Antarctica. Nature, 1998 (Ref: 8317)
Category 1: Peer-reviewed literature

Break-up of ice shelves has been regarded as an indicator of climate change1. Observations around the Antarctic Peninsula have shown a pattern of gradual retreat, associated with a regional atmospheric warming and increased summer melt and fracturing processes2-9.

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