gptkbp:instanceOf
|
gptkb:lake
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gptkbp:adjacentTo
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gptkb:Pine_Island_Glacier
gptkb:Haynes_Glacier
gptkb:Smith_Glacier
|
gptkbp:area
|
about 192,000 km²
|
gptkbp:claimedBy
|
unclaimed territory
|
gptkbp:connectedTo
|
gptkb:Pine_Island_Glacier
|
gptkbp:coordinates
|
75°30′S 106°45′W
|
gptkbp:dam
|
outlet glacier
|
gptkbp:discoveredBy
|
gptkb:British_Graham_Land_Expedition
|
gptkbp:discoveredIn
|
1930s
|
gptkbp:endDate
|
gptkb:Amundsen_Sea
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gptkbp:firstMapped
|
gptkb:US_Geological_Survey
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gptkbp:firstMappedInYear
|
1960s
|
https://www.w3.org/2000/01/rdf-schema#label
|
Thwaites Glacier
|
gptkbp:iceDischarge
|
one of the largest in Antarctica
|
gptkbp:iceFlowDirection
|
northwest
|
gptkbp:iceFrontRetreat
|
significant since 1990s
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gptkbp:iceLoss
|
over 50 billion tons per year (as of 2020s)
|
gptkbp:iceLossAcceleration
|
observed since 2000s
|
gptkbp:iceLossRate
|
gptkb:fire
|
gptkbp:iceShelfCollapseRisk
|
high
|
gptkbp:iceShelfPresent
|
yes
|
gptkbp:iceShelfStatus
|
unstable
|
gptkbp:iceStream
|
yes
|
gptkbp:length
|
about 120 km
|
gptkbp:locatedIn
|
gptkb:Amundsen_Sea_sector
gptkb:West_Antarctica
|
gptkbp:mediaAttention
|
high due to sea level rise risk
|
gptkbp:meltingCause
|
warm ocean water intrusion
|
gptkbp:monitors
|
gptkb:International_Thwaites_Glacier_Collaboration
satellite observations
field expeditions
|
gptkbp:namedAfter
|
gptkb:Fredrik_T._Thwaites
|
gptkbp:nickname
|
gptkb:Doomsday_Glacier
|
gptkbp:partOf
|
gptkb:West_Antarctic_Ice_Sheet
|
gptkbp:potentialSeaLevelRise
|
up to 65 cm if fully melted
|
gptkbp:researchStationsNearby
|
none
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gptkbp:riskFactor
|
collapse could destabilize West Antarctic Ice Sheet
|
gptkbp:significance
|
major contributor to global sea level rise
subject of international scientific study
|
gptkbp:studiedBy
|
gptkb:NASA
gptkb:UK_Natural_Environment_Research_Council
gptkb:US_National_Science_Foundation
British Antarctic Survey
|
gptkbp:thickness
|
up to 1200 m
|
gptkbp:threats
|
high
|
gptkbp:width
|
about 120 km
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gptkbp:bfsParent
|
gptkb:lake
|
gptkbp:bfsLayer
|
4
|