West Antarctic outlet glaciers

E615705

West Antarctic outlet glaciers are fast-flowing ice streams that drain the West Antarctic Ice Sheet into the surrounding oceans, playing a critical role in regional ice loss and global sea-level rise.

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Observed surface forms (1)

Surface form Occurrences
Amundsen Sea outlet glaciers 1

Statements (50)

Predicate Object
instanceOf glacier system
ice stream
outlet glacier
bedBelow sea level
contributesTo Antarctic ice mass loss
global sea-level rise
controls drainage of West Antarctic Ice Sheet
drainInto Amundsen Sea NERFINISHED
Bellingshausen Sea NERFINISHED
Ross Sea NERFINISHED
Southern Ocean NERFINISHED
exhibits dynamic thinning
grounding-line retreat
ice-flow acceleration
flowDirection toward coast
flowsOver marine-based bedrock
flowType fast-flowing ice
hasPart Crosson Ice Shelf outlet glaciers NERFINISHED
Dotson Ice Shelf outlet glaciers
Getz outlet glaciers NERFINISHED
Haynes Glacier NERFINISHED
Kohler Glacier NERFINISHED
Mercer Ice Stream NERFINISHED
Pine Island Glacier NERFINISHED
Rutford Ice Stream NERFINISHED
Smith Glacier NERFINISHED
Thwaites Glacier NERFINISHED
Whillans Ice Stream NERFINISHED
influencedBy Circumpolar Deep Water intrusions
bed topography
ice-shelf thinning
subglacial hydrology
locatedIn West Antarctica NERFINISHED
monitoredBy GPS measurements
airborne radar surveys
satellite altimetry
satellite interferometric SAR
partOf West Antarctic Ice Sheet NERFINISHED
roleIn future sea-level projections
potential marine ice-sheet instability
sensitiveTo basal melting
changes in ice-shelf buttressing
grounding-line retreat
ocean warming
studiedIn climate change research
cryospheric science
glaciology
terminusForm grounding line
ice shelf
ice tongue

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Smith Glacier (Antarctica) partOf West Antarctic outlet glaciers
Smith Glacier partOf West Antarctic outlet glaciers
this entity surface form: Amundsen Sea outlet glaciers