Smith Glacier (Antarctica)

E154230

Smith Glacier is a major Antarctic glacier that drains part of the West Antarctic Ice Sheet into the Amundsen Sea, contributing to regional ice loss and sea-level rise.

All labels observed (1)

Label Occurrences
Smith Glacier (Antarctica) canonical 1

How this entity was disambiguated

Statements (39)

Predicate Object
instanceOf Antarctic glacier
glacier
continent Antarctica
contributesTo global sea-level rise
regional ice mass loss
drainsInto Amundsen Sea
flowsFrom interior of West Antarctic Ice Sheet
hasProcess basal melting
dynamic thinning
ice discharge to ocean
hasProperty fast-flowing
marine-terminating
retreating terminus
thinning
hasRelevanceTo Antarctic ice-sheet stability
ocean–ice interactions
sea-level projections
hasRisk contribution to future sea-level rise
potential dynamic instability
influencedBy climate change
ocean-driven melting
warm Circumpolar Deep Water
locatedIn Marie Byrd Land
West Antarctica
locatedOn West Antarctica
surface form: West Antarctic Ice Sheet
monitoredBy gravity missions (e.g., GRACE)
satellite altimetry
satellite interferometric SAR
partOf Amundsen Sea Embayment glacial system
Amundsen Sea
surface form: Amundsen Sea sector

West Antarctic outlet glaciers
global cryosphere
studiedBy climate scientists
glaciologists
subjectOf glaciological research
ice-flow modeling studies
remote sensing studies
terminusIn Amundsen Sea
terminusType ice shelf front

How these facts were elicited

Referenced by (1)

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

Amundsen Sea hasGlacier Smith Glacier (Antarctica)