Amundsen Sea

Coordinates: 73°S 112°W / 73°S 112°W / -73; -112
Source: Wikipedia, the free encyclopedia.
Not to be confused with the Amundsen Gulf.
The Amundsen Sea area of Antarctica
Antarctic iceberg floating in the Amundsen Sea water, October 2009.

The Amundsen Sea is an arm of the

marginal sea of the Southern Ocean between the Amundsen and Ross Seas. The Norwegian expedition of 1928–1929 under Captain Nils Larsen named the body of water for the Norwegian polar explorer Roald Amundsen while exploring this area in February 1929.[1]

The sea is mostly ice-covered, and the Thwaites Ice Tongue protrudes into it. The ice sheet which drains into the Amundsen Sea averages about 3 km (1.9 mi) in thickness; roughly the size of the state of Texas, this area is known as the Amundsen Sea Embayment (ASE); it forms one of the three major ice-drainage basins of the West Antarctic Ice Sheet.

Embayment

See also: Rossby wave § Oceanic waves
Large B-22 iceberg breaking off from Thwaites Glacier and remnants of the B-21 iceberg from Pine Island Glacier in Pine Island Bay to the right of the image

The ice sheet that drains into the Amundsen Sea averages about 3 km (1.9 mi) in thickness. It is roughly the size of the state of Texas and is known as the Amundsen Sea Embayment (ASE); it forms one of the three major ice drainage basins of the

Embayment and the Weddell Sea
Embayment.

Some scientists proposed that this region may be a weak underbelly of the

rise by about 0.9–1.9 meters (3.0–6.2 feet). Other researchers suggested that the loss of these glaciers would destabilise the entire West Antarctic ice sheet and possibly sections of the East Antarctic Ice Sheet.[2]

A 2004 study suggested that because the ice in the Amundsen Sea had been melting rapidly and was riven with cracks, the offshore ice shelf was set to collapse "within five years". The study projected a sea level rise of 1.3 m (4.3 ft) from the West Antarctic Ice Sheet if all the sea ice in the Amundsen Sea melted.[3]

Measurements made by the British Antarctic Survey in 2005 showed that the ice discharge rate into the Amundsen Sea embayment was about 250 km3 per year. Assuming a steady rate of discharge, this alone was sufficient to raise global sea levels by 0.2 mm per year.[4]

A subglacial

global warming.[10]

Amundsen Sea as part of the Southern Ocean

In January 2010, a modelling study suggested that the "tipping point" for Pine Island Glacier may have been passed in 1996, with a retreat of 200 kilometers (120 miles) possible by 2100, producing a corresponding 24 cm (0.79 ft) of sea level rise. It was suggested that these estimates were conservative.[11] The modelling study also stated that "Given the complex, three-dimensional nature of the real Pine Island glacier ... it should be clear that the [...] model is a very crude representation of reality."[12]

A 2023 study estimated that the area lost 3.3 trillion tons of ice between 1996 and 2021, raising sea levels by 9 millimeters.

Pine Island Bay

Pine Island Bay (74°50′S 102°40′W / 74.833°S 102.667°W / -74.833; -102.667) is a bay about 40 miles (64 km) long and 30 miles (48 km) wide, into which flows the ice of the

USS Pine Island, seaplane tender and flagship of the eastern task group of USN Operation HIGHJUMP which explored this area.[13]

Russell Bay

Russell Bay (73°27′S 123°54′W / 73.450°S 123.900°W / -73.450; -123.900) is a rather open bay in southwestern Amundsen Sea, extending along the north sides of

Carney Island, from Pranke Island to Cape Gates. It was mapped by the United States Geological Survey from surveys and USN air photos, 1959–66, and named by the Advisory Committee on Antarctic Names for Admiral James S. Russell, Vice Chief of Naval Operations during the post 1957–58 IGY period.[14]

Climate engineering

This section is an excerpt from Thwaites Glacier § Engineering options for stabilization.[edit]
A proposed "underwater sill" blocking 50% of warm water flows heading for the glacier could have the potential to delay its collapse and the resultant sea level rise by many centuries.[15]

Some engineering interventions have been proposed for Thwaites Glacier and the nearby

greenhouse gas emission reductions.[15]

In 2023, a modified proposal was tabled: it was proposed that an installation of underwater "curtains", made out of a flexible material and anchored to Amundsen Sea floor would be able to interrupt warm water flow while reducing costs and increasing their longevity (conservatively estimated at 25 years for curtain elements and up to 100 years for the foundations) relative to more rigid structures. With them in place, Thwaites Ice Shelf and Pine Island Ice Shelf would presumably be able to regrow to a state they last had a century ago, thus stabilizing these glaciers.[19][20][17] To achieve this, the curtains would have to be placed at a depth of around 600 metres (0.37 miles) (to avoid damage from icebergs which would be regularly drifting above) and be 80 km (50 mi) long. The authors acknowledged that while work on this scale would be unprecedented and face many challenges in the Antarctic (including polar night and the currently insufficient numbers of specialized polar ships and underwater vessels), it would also not require any new technology and there is already experience of laying down pipelines at such depths.[19][20]

Diagram of a proposed "curtain".[19]
The authors estimated that this project would take a decade to construct, at $40–80 billion initial cost, while the ongoing maintenance would cost $1–2 billion a year.[19][20] Yet, a single seawall capable of protecting the entire New York City may cost twice as much on its own,[17] and the global costs of adaptation to sea level rise caused by the glaciers' collapse are estimated to reach $40 billion annually:[19][20] The authors also suggested that their proposal would be competitive with the other "climate engineering" proposals like stratospheric aerosol injection (SAI) or carbon dioxide removal (CDR), as while those would stop a much larger spectrum of climate change impacts, their estimated annual costs range from $7–70 billion for SAI to $160–4500 billion for CDR powerful enough to help meet the 1.5 °C (2.7 °F) Paris Agreement target.[19][20]

References

  1. ^ "Amundsen Sea". Geographic Names Information System. United States Geological Survey. Retrieved 23 October 2011.
  2. ^ Pearce, Fred (2007). With Speed and Violence: Why scientists fear tipping points in climate change. Beacon Press Books.
    ISBN 978-0-8070-8576-9
    .
  3. ^ Flannery, Tim F. (2006). The Weather Makers: How man is changing the climate and what it means for life on Earth. HarperCollins. pp. 356.
    ISBN 978-0-00-200751-1
    .
  4. ^ Strom, Robert (2007). "The Melting Earth". Hot House: Global Climate Change and the Human Condition. Coprenicus Books. p. 302.
  5. ^ Black, Richard (20 January 2008). "Ancient Antarctic eruption noted".
    BBC
    . Retrieved 22 October 2011.
  6. ^ Corr, H. F. J.; Vaughan, D. G. (2008). "A recent volcanic eruption beneath the West Antarctic ice sheet".
    doi:10.1038/ngeo106
    .
  7. ^ Mosher, Dave (20 January 2008). "Buried Volcano Discovered in Antarctica". Imaginova Corp. LiveScience.com. Retrieved 11 April 2009.
  8. ^ Payne, A. J.; Vieli, A.; Shepherd, A. P.; Wingham, D. J.; Rignot, E. (2004). "Recent dramatic thinning of largest West Antarctic ice stream triggered by oceans".
    S2CID 4891690
    .
  9. ^ Shepherd, A. P.; Wingham, D. J.; Rignot, E. (2004). "Warm ocean is eroding West Antarctic Ice Sheet" (PDF).
    doi:10.1029/2004GL021106
    .
  10. ^ Thoma, M.; Jenkins, A.; Holland, D.; Jacobs, S. (2008). "Modelling Circumpolar Deep Water intrusions on the Amundsen Sea continental shelf, Antarctica" (PDF).
    S2CID 55937812
    .
  11. ^ Barley, Shanta (13 January 2010). "Major Antarctic glacier is 'past its tipping point'". Reed Business Information Ltd. New Scientist. Archived from the original on 16 January 2010. Retrieved 17 January 2010.
  12. ^ Katz, R. F.; Worster, M.G. (2010). "Stability of ice sheet grounding lines".
    doi:10.1098/rspa.2009.0434
    .
  13. ^ "Pine Island Bay". Geographic Names Information System. United States Geological Survey. Retrieved 23 October 2011.
  14. ^ "Russell Bay". Geographic Names Information System. United States Geological Survey. Retrieved 23 October 2011.
  15. ^
    S2CID 52969664
    .
  16. S2CID 206554077
    .
  17. ^ a b c d James Temple (14 January 2022). "The radical intervention that might save the "doomsday" glacier". MIT Technology Review. Retrieved 19 July 2023.
  18. PMID 29695853
    .
  19. ^
    PMID 37007716
    .
  20. ^
    PMID 37091546
    .

External links

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