Dep Science Leader of Palaeo Environments IMP 3
International Thwaites Glacier Collaboration
International Thwaites Glacier Collaboration
- Start date:
- 1 April, 2018
- End date:
- 1 December, 2026
What this project does
The International Thwaites Glacier Collaboration (ITGC) studies Antarctica’s most vulnerable and rapidly changing large glacier.
It investigates how West Antarctica’s Thwaites Glacier is changing, what controls its stability and how quickly it might retreat.
Researchers use field observations, measurements of the ice and ocean, evidence of how it has changed over centuries and millennia and advanced modelling to improve predictions of its impact on global sea-level rise.
Why this matters
ITGC helps us to:
- determine whether loss of Thwaites Glacier will occur over decades or centuries
- assess how its retreat will accelerate global sea-level rise
- improve knowledge of how ice, ocean, and climate processes interact in West Antarctica
- provide robust data for climate models and sea-level forecasts used by scientists and policymakers worldwide
Thwaites Glacier, sometimes referred to as the ‘Doomsday Glacier’, drains an area the size of Great Britain It already accounts for about 4% of global sea-level rise – a rate that has trebled since the mid-1990s. Its entire loss will eventually raise sea level by 65cm and lead to further ice loss from adjacent glaciers. Understanding its future is critical for planning and adapting to climate change.
Who is involved
ITGC is a joint UK–US programme funded by the Natural Environment Research Council (NERC) and the National Science Foundation (NSF).
It is the largest UK–US Antarctic research collaboration in over 70 years.
The programme brings together around 100 scientists from leading institutions in the UK, US, South Korea, Germany and Sweden.
What did this project discover
Over the past seven years, research on the glacier has unveiled a complex and rapidly changing environment.
Thwaites Glacier’s retreat has accelerated considerably over the past 30 years. Although a full disintegration is unlikely to occur in the next few decades, our findings indicate it is set to retreat further, and faster, through the 21st and 22nd centuries, and general disintegration of the West Antarctic Ice Sheet over this timeframe cannot be ruled out.
Further research is urgently needed to refine this timeline.
Immediate and sustained climate change mitigation (decarbonisation) offers the best hope of delaying this ice loss and avoiding initiation of similar unstable retreat in marine-based sectors of East Antarctica.
Read the findings of the ITGC report.
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Fieldwork starts on Thwaites Glacier
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Underwater robot reveals how Thwaites Glacier is melting
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Deep channels link ocean to Antarctic glacier
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Plans for International Thwaites Glacier Collaboration in response to COVID-19
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Scientists drill for first time on remote Antarctic Glacier
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Scientists head to Antarctica’s Thwaites Glacier
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2019/20 Antarctic field season begins
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Seals to act as sentinels of remote Antarctic glacier
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