Ice-flow Velocity Derivation of the Confluence Zone of the Amery Ice Shelf Using Offset-tracking Method
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Abstract
ThreepairsofEnvisatASARimagesata35daysintervalwereutilizedtomaptheiceveloci tyintheconfluencezoneoftheAmeryiceshelfintheEastAntarcticausinganoffset trackingmeth od.Accuracyassessmentandcomparativeanalysiswereconducted,whichconfirmedthereliabilityofourresults.Theicevelocityreachedashighas800m/aattheconfluencezoneoftheLambert,Mel lor,andFisherGlaciers.Therewerecertainvariationcharacteristicsoficevelocitynearthegroundingline,whichprovidedimportantreferenceswhendeterminingthepositionofthegroundingline.犓犲狔狑狅狉犱狊:ameryiceshelf;iceflowvelocity;offsettracking;groundingline
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