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Antarctic Glacier Caught in Act of 'Ice Piracy,' Stealing Ice from Neighbor

15 hours ago

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Executive Summary

  • Kohler East Glacier in West Antarctica is rapidly siphoning ice from the slower-moving Kohler West Glacier, a process termed 'ice piracy'.
  • Satellite data from 2005 to 2022 reveals this phenomenon is occurring within 18 years, much faster than previously understood.
  • The 'ice piracy' contributes to faster glacial flow in Kohler East, slower glacial flow in Kohler West, altered ice mass flux into Dotson and Crosson Ice Shelves, and adds to the ongoing acceleration of sea-level rise.

Event Overview

A new study has revealed that the Kohler East Glacier in West Antarctica is stealing ice from its neighbor, Kohler West, in a process termed 'ice piracy'. This phenomenon, observed using satellite data between 2005 and 2022, is happening at an unexpectedly rapid pace – within 18 years – challenging previous understanding of glacial dynamics. The study, led by the University of Leeds, analyzed satellite imagery and ice-thinning data to measure the speed changes in the Pope, Smith, and Kohler region, revealing significant acceleration in most ice streams but a slowdown in Kohler West, attributed to the redirection of ice flow towards its faster-moving neighbor. This 'ice piracy' has implications for ice sheet stability, sea-level rise, and understanding the complex interactions between glaciers and ice shelves.

Media Coverage Comparison

Source Key Angle / Focus Unique Details Mentioned Tone
ESA Highlighting the role of Copernicus Sentinel-1 satellite data in discovering the ice piracy and understanding glacial dynamics. Mentions that the research was partly funded by the Science for Society element of ESA’s FutureEO programme. Details about CryoSat mission data usage. Focus on grounding line retreat. Informative and emphasizing the importance of satellite technology for polar research.
Discover Magazine Framing the event as 'ice piracy' and highlighting the implications for sea-level rise and at-risk populations. Provides the equivalent speed of the accelerated ice streams in terms of 'football fields' per year. Includes a statistic about global sea-level rise and at-risk populations by 2100. Engaging and emphasizing the broader impact on global communities.
British Antarctic Survey Underscoring the significance of the findings in challenging scientific understanding of Antarctica’s ice dynamics and potential sea-level rise contributions. Features a quote from Dr. Pierre Dutrieux (BAS) and highlights collaboration between Leeds, BAS, and the UK Centre for Polar Observation and Modelling. Authoritative and emphasizing the collaborative nature of the research.

Key Details & Data Points

  • What: The Kohler East Glacier is 'stealing' ice from the Kohler West Glacier due to differential thinning rates and redirection of ice flow. This is observed as an acceleration of Kohler East and a deceleration of Kohler West.
  • Who: Key individuals involved are Dr. Heather Selley and Professor Anna Hogg (University of Leeds), Dr. Pierre Dutrieux (British Antarctic Survey), and Dr. Martin Wearing (ESA). Key organizations include the University of Leeds, British Antarctic Survey, ESA, and NASA.
  • When: The 'ice piracy' was observed between 2005 and 2022.
  • Where: The event is occurring in the Pope, Smith, and Kohler (PSK) region of West Antarctica, specifically affecting the Dotson and Crosson Ice Shelves.

Key Statistics:

  • Glaciers in the Pope-Smith-Kohler region have sped up by an average of 51% since 2005.
  • Six of the ice streams reached average speeds of over 700 m (2200 feet) per year in 2022 alone.
  • Kohler West glacier slowed by 10% over the study period (2005-2022).

Analysis & Context

The 'ice piracy' phenomenon reveals a complex interplay between adjacent glaciers and their response to climate change. The faster-thinning Kohler East Glacier is drawing ice from the slower-moving Kohler West Glacier, leading to an altered ice mass flux into the Dotson and Crosson Ice Shelves. This process, occurring at an accelerated rate compared to previous understanding, highlights the dynamic nature of Antarctic ice sheets and the importance of continuous monitoring using satellite data. The implications extend to sea-level rise projections, emphasizing the need to incorporate such interactions into future climate models. The grounding line retreat and increased instability in the region contribute to further concerns about ice sheet stability.

Notable Quotes

We think that the observed slowdown on Kohler West Glacier is due to the redirection of ice flow towards its neighbour – Kohler East. This is due to the large change in Kohler West’s surface slope, likely caused by the vastly different thinning rates on its neighbouring glaciers. This is effectively an act of ‘ice piracy’, where ice flow is redirected from one glacier to another, and the accelerating glacier is essentially ‘thieving’ ice from its slowing neighbour.
— Dr Heather Selley (British Antarctic Survey)
This study provides an interesting demonstration of ice piracy, where flow into one glacier gradually switches to flow into another glacier, as the ocean melts the grounding zone and re-configures ice flow.
— Dr Pierre Dutrieux, climate researcher at the British Antarctic Survey (BAS) (British Antarctic Survey)
This suggests that ice flow redirection is an important new process in contemporary ice sheet dynamics, which is required to understand present-day structural change in glaciers and the future evolution of these systems.
— Professor Anna Hogg from the University of Leeds (British Antarctic Survey)

Conclusion

The discovery of 'ice piracy' in West Antarctica underscores the accelerating changes occurring in polar regions and the need for ongoing monitoring and research. The rapid pace of this phenomenon challenges previous assumptions about glacial dynamics and has implications for understanding and predicting sea-level rise. The interplay between adjacent glaciers, driven by climate change and differential thinning rates, requires further investigation to refine climate models and assess the future stability of Antarctic ice sheets. Satellite data will continue to play a crucial role in tracking these developments and informing mitigation strategies.

Disclaimer: This article was generated by an AI system that synthesizes information from multiple news sources. While efforts are made to ensure accuracy and objectivity, reporting nuances, potential biases, or errors from original sources may be reflected. The information presented here is for informational purposes and should be verified with primary sources, especially for critical decisions.