Thwaites Glacier
| Thwaites Glacier | |
|---|---|
| Doomsday Glacier | |
 Thwaites Glacier | |
| Type | tidewater valley |
| Location | Walgreen Coast, Marie Byrd Land, Antarctic |
| Coordinates | Coordinates: 75°30′S 106°45′W |
| Lowest elevation | below sea level |
| Terminus | Pine Island Bay, part of the Amundsen Sea |
| Status | receding |
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Thwaites Glacier, sometimes referred to as the Doomsday Glacier,[1] is an unusually broad and vast Antarctic glacier flowing into Pine Island Bay, part of the Amundsen Sea, east of Mount Murphy, on the Walgreen Coast of Marie Byrd Land.[2] Its surface speeds exceed 2 kilometres (1.2 miles) per year near its grounding line. Its fastest flowing grounded ice is centered between 50 and 100 kilometres (31 and 62 mi) east of Mount Murphy. In 1967, the Advisory Committee on Antarctic Names named the glacier after Fredrik T. Thwaites (1883–1961), a glacial geologist, geomorphologist and professor emeritus at the University of Wisconsin–Madison.[3][4] The historian Reuben Gold Thwaites was his father.[5]
Thwaites Glacier is closely watched for its potential to raise sea levels.[6] Along with the Pine Island Glacier, it 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 observations of large changes on these two glaciers. In recent years, the flow of both of these glaciers has accelerated, their surfaces have lowered, and their grounding lines have retreated.
Research[edit]
In 2001, a study of Thwaites Glacier using satellite radar interferometry data from the Earth Remote Sensing Satellite 1 and 2 revealed that the grounding line of Thwaites Glacier was retreating at 1 kilometer per year and that the glacier was significantly out of mass balance, hence confirming presumptions of collapse by Terence Hughes, University of Maine, in 1973. In 2002, a team of scientists from Chile and NASA on board an Orion P3 from the Chilean Navy collected the first radar sounding and laser altimetry survey of the glacier to reveal extensive thinning and acceleration in thinning. This discovery prompted an extensive airborne campaign in 2004 by the University of Texas, Austin, Texas, to be followed by subsequent airborne campaigns under NASA's IceBridge Campaign in 2009–2018.
In 2011, using geophysical data collected from flights over Thwaites Glacier (data collected under NASA's IceBridge campaign), a study by scientists at Columbia University's Lamont-Doherty Earth Observatory showed a rock feature, a ridge 700 meters tall that helps anchor the glacier and helped slow the glacier's slide into the sea. The study also confirmed the importance of seafloor topography in predicting how the glacier will behave in the near future.[7] However, the glacier has been considered to be the biggest threat on relevant time scales, for rising seas, current studies aim to better quantify retreat and possible impacts.[8] Since the 1980s, the glacier had a net loss of over 600 billion tons of ice though 2017.[9] In 2017, scientists discovered previously unknown volcanoes nearby.[10]
In 2020, scientists discovered warm water underneath the glacier for the first time.[11][12] The place where the glacier was in contact with the sea had been recorded as 2 degree Celsius above the freezing temperature.[13] The discovery was a part of the International Thwaites Glacier Collaboration, a partnership primarily between US and UK academic institutions. This study has raised alarm regarding the glacier collapse, which can lead to nearly 3 ft (0.9 m) rise in the sea level.[14]
Extensive calving at the marine terminus of Thwaites Glacier is monitored by remote sensing and seismological observations, with the largest events being seismically detectable at ranges up to 1600 km.[15]
Water drainage beneath the glacier[edit]
Swamp-like canal areas and streams underlie the glacier. The upstream swamp canals 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.[16]
Predictions[edit]
A 2014 University of Washington study, using satellite measurements and computer models, predicted that the Thwaites Glacier will gradually melt, leading to an irreversible collapse over the next 200 to 1000 years.[17][18][19][20][21][22] A 2021 study, suggested that the timeframe for collapse may be shorter, within 3-5 years leading to rapid process of releasing ice that would cause up to 65 centimeters of sea level rise.[23][24] According to Ted Scambos, a glaciologist at the University of Colorado Boulder and a leader of the International Thwaites Glacier Collaboration, in a late 2021 interview from McMurdo Station, "Things are evolving really rapidly here. It's daunting."[12]
Features and observation[edit]
Thwaites Glacier Tongue[edit]
The Thwaites Glacier Tongue, or Thwaites Ice Tongue (75°0′S 106°50′W), is about 50 km wide and has progressively shortened due to ice calving, based on the observational record. It was initially delineated from aerial photographs collected during Operation Highjump in January 1947.
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[edit]
The Thwaites Iceberg Tongue (74°0′S 108°30′W) was a large iceberg tongue which was aground in the Amundsen Sea, about 32 km northeast of 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.[25] It was first noted in the 1930s, but finally detached from the ice tongue and broke up in the late 1980s.[26][27]
Underwater cavity[edit]
In January 2019, NASA discovered an underwater cavity underneath the glacier, with an area two-thirds the size of Manhattan. The cavity formed mostly in the previous three years and is nearly a thousand feet tall, likely speeding up the glacier's decay. Thwaites currently contributes roughly 4% to global sea level rise.[28]
International Thwaites Glacier Collaboration (ITGC)[edit]
A 5-year international collaboration to study the Thwaites Glacier was established in 2018.[29][30][23]
At the beginning of 2020, researchers from the ITGC took measurements to develop scenarios for the future of the glacier and to predict the time frame for a possible collapse: The erosion of the glacier by warmed ocean water seems to be stronger than expected. The researchers noted with concern, that at the baseline of the glacier, the temperature of the water is already more than two degrees above freezing point. They confirm thawing of the Thwaites glacier contributes about four percent of global sea-level rise.[23] The collapse of this glacier alone would raise the sea level by about 65 centimetres (25 inches).[31]
See also[edit]
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