Thwaites Glacier (Antarctic glacier flowing into Pine Island Bay, part of the Amundsen Sea, east of Mount Murphy, on the Walgreen Coast of Marie Byrd Land. Its surface speeds exceed 2 km/yr near its grounding line, and its fastest flowing grounded ice is centred between 50 and 100 km east of Mount Murphy. It was named by ACAN for Fredrik T. Thwaites, a glacial geologist, geomorphologist and professor emeritus at the University of Wisconsin–Madison. Thwaits Glacier drains into West Antarctica’s Amundsen Sea and is being closely watched for its potential to raise global sea levels.) is an unusually broad and fast
Along with Pine Island Glacier, Thwaites Glacier has been described as part of the "weak underbelly" of the West Antarctic Ice Sheet, due to its apparent vulnerability to significant retreat. This hypothesis is based on both theoretical studies of the stability of marine ice sheets and recent observations of large changes on both of these glaciers. In recent years, the flow of both of these glaciers has accelerated, their surfaces have lowered, and their grounding lines have retreated.
In 2011, using geophysical data collected from flights over Thwaites Glacier (data collected under NASA's Ice Bridge campaign), a study by scientists at Columbia University’s Lamont-Doherty Earth Observatory showed a rock feature, a ridge 700 meters tall helps anchor the glacier and actually helped slow the glacier's slide into the sea. The study also confirms the importance of seafloor topography in predicting how these glaciers will behave in the near future.
Thwaites Glacier Tongue
The Thwaites Glacier Tongue, or Thwaites Ice Tongue (ice calving, based on the observational record. It was initially delineated from aerial photographs collected during Operation Highjump in January 1947.), is about 50 km wide and has progressively shortened due to
On 15 March 2002, the National Ice Center reported that an iceberg named B-22 broke off from the ice tongue. This iceberg was about 85 km long by 65 km wide, with a total area of some 5,490 km². As of 2003, B-22 had broken into five pieces, with B-22A still in the vicinity of the tongue, while the other smaller pieces had drifted farther west.
Thwaites Iceberg Tongue
The Thwaites Iceberg Tongue (Bear Peninsula. The feature was about 112 km long and 32 km wide, and in January 1966 its southern extent was only 5 km north of Thwaites Glacier Tongue. It consisted of icebergs which had broken off from the Thwaites Ice Tongue and ran aground, and should not be confused with the latter, which is still attached to the grounded ice. It was delineated by the USGS from aerial photographs collected during Operation Highjump and Operation Deepfreeze. It was first noted in the 1930s, but finally detached from the ice tongue off and broke up in the late 1980s.) was a large iceberg tongue which was aground in the Amundsen Sea, about 32 km northeast of
Water drainage beneath the glacier
Swamp like areas and streams underlie the glacier. The upstream swamps feed streams with dry areas between the streams which retard flow of the glacier. Due to this friction the glacier is considered stable in the short term.
- "Thwaites Glacier Tongue". Geographic Names Information System. United States Geological Survey. Retrieved 23 October 2011.
- "Thwaites Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 23 October 2011.
- "Thwaites Iceberg Tongue". Geographic Names Information System. United States Geological Survey. Retrieved 23 October 2011.
- Reynolds, Larry (4 March 2000). "Where a cold tongue isn't". Teachers Experiencing Antarctica. Retrieved 16 June 2009.
- Lucchitta, B.K.; Smith, C.E.; Bowel, J.; Mullins, K.F. (1994). "Velocities and mass balance of Pine Island Glacier, West Antarctica, derived from ERS-1 SAR". Pub. SP-361, 2nd ERS-1 Symposium, Space at the Service of Our Environment, Hamburg, Germany, 11–14, Oct. 1993 Proceedings. pp. 147–151.
- "Scientists Image Vast Subglacial Water System Underpinning West Antarctica’s Thwaites Glacier". University of Texas. July 9, 2013. Retrieved July 9, 2013.