Helicopters track warm ocean water melting Totten Glacier ice shelf

Publicly released:
Australia; International; TAS

Probes measuring temperature and salinity were dropped from helicopters through ice cracks in East Antarctica to reveal warm ocean water flowing towards the Totten Glacier Ice Shelf. With a catchment holding the equivalent of about 3.5 metres of global sea-level rise, the Totten Glacier hosts the most rapidly thinning ice in East Antarctica, due to rapid melt of the ice shelf where warm ocean water flows into cavities underneath.

Media release

From: University of Tasmania

Probes dropped from helicopters through ice cracks help reveal that warm ocean water is melting the largest glacier ice shelf in East Antarctica from below.

With its catchment holding the equivalent ice volume of about 3.5 metres of global sea-level rise, the Totten Glacier is the most rapidly thinning in East Antarctica.

The results of six days of helicopter surveys off the Totten Glacier Ice Shelf during the 61st Japanese Antarctic Research Expedition in 2019 are published today in Geophysical Research Letters.

A co-second author, Dr Pat Wongpan of the Australian Antarctic Program Partnership, said their study was able to investigate a broader area of the continental shelf than previously covered by ships.

“To understand the pathways and mechanisms of warm water inflow, ocean observations across entire continental shelf regions are necessary, but ships are often obstructed by sea ice and icebergs.”

“This study uses probes dropped from helicopters through cracks in landfast ice to measure the temperature and salinity of the ocean to a depth of 1000 metres,” he said.

In total, 74 AXCTD (Airborne eXpendable Conductivity, Temperature, and Depth) and AXBT (Airborne Bathy-Thermograph) probes were deployed. These expendable instruments were launched from a helicopter into ice cracks between 15 and 540 m wide to float on the ocean surface. The floating portion releases a probe, which sinks toward the seabed, and transmits data back to the helicopter.

Intrusions of warm ocean water (0.5–1°C) were found uniformly over a large previously unsampled area of the continental shelf region below 550-600 metres.

Glacial meltwater outflow from the Totten Ice Shelf cavity was also identified, which is direct evidence of the ice shelf melting from beneath.

The authors write that their results “emphasise the capability and effectiveness of helicopter-based oceanographic observations for efficient and broad surveys of Antarctic coastal regions, especially for tracing pathways of ocean heat intrusions toward Antarctic ice shelves.”

Dr Wongpan said that helicopters are unaffected by sea-ice conditions, travel faster than a ship, can conduct measurement through small ice cracks, and are cheaper to operate than an icebreaker.

“By combining ship-based and helicopter-based approaches we may be able to enhance the efficiency of future polar oceanographic observations.”

“This will be crucial for intensifying our research to urgently improve projections of sea level rise,” Dr Wongpan said.

Multimedia

Deployment of probe from helicopter through ice crack
Icescape in front of Totten Glacier showing probe deployment and antenna
researchers prepare for helicopter deployment
researchers prepare for helicopter deployment
researcher with probe
researcher with probe
probe release
probe release
Totten Glacier ice shelf
Totten Glacier ice shelf
icescape from helicopter
icescape from helicopter
Journal/
conference:
Geophysical Research Letters
Research:Paper
Organisation/s: University of Tasmania, Institute for Marine and Antarctic Studies (IMAS), Australian Antarctic Program Partnership (AAPP), Hokkaido University Japan, Scripps Institution of Oceanography USA, National Institute for Polar Research Japan, Marine Works Japan, Tomakomai College Japan, University of Texas at Austin USA
Funder: Science Program of Japanese Antarctic Research Expedition (JARE); National Institute of Polar Research (NIPR); Ministry of Education, Culture, Sports, Science, and Technology in Japan; National Science Foundation (NSF); Australian Antarctic Program Partnership; Japan Society for the Promotion of Science; NASA’s Cryosphere Program
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