FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4286321376> ?p ?o ?g. }

• W4286321376 abstract "Abstract Over the last two decades, Trinity, Wykeham, Ekblaw, and Cadogan glaciers have retreated and been identified as the primary sources of iceberg flux from Prince of Wales (POW) Icefield, Ellesmere Island, accounting for ∼83% of total solid ice discharge. In this study, we used a total of 167 Radarsat‐2 Synthetic Aperture Radar scene pairs collected between 2009 and 2019 to derive winter surface velocities of these four major basins of the POW Icefield. Over this period both Cadogan and Ekblaw glaciers underwent multiyear acceleration and deceleration limited to their lower parts, consistent with characteristics of “pulse‐type” glaciers. Trinity and Wykeham glaciers are currently the fastest flowing glaciers in the CAA and are grounded below sea level for ∼40 km up‐glacier from their termini. Both glaciers underwent multiyear repeating periods of velocity acceleration between 2009 and 2019 which coincided with significant thinning at their termini. As of 2017, Trinity and Wykeham were each within ∼10 m of flotation over their lowermost 4 km. We also identified a shift in flow since 2014 on Trinity and Wykeham, after which winter flow rates began to propagate up‐glacier and were nearly identical to flow rates observed throughout the rest of the year, indicating that seasonal variability in flow has become less apparent in recent years. Our findings suggest that Trinity and Wykeham glaciers have transitioned to a flow type dominated by dynamic thinning, which is strongly influenced by subglacial topography and may be susceptible to instability of the glacier front and large‐scale collapse." @default.
• W4286321376 created "2022-07-21" @default.
• W4286321376 creator A5001903581 @default.
• W4286321376 creator A5025898965 @default.
• W4286321376 creator A5028080549 @default.
• W4286321376 creator A5070252251 @default.
• W4286321376 creator A5082605601 @default.
• W4286321376 date "2022-04-01" @default.
• W4286321376 modified "2023-10-16" @default.
• W4286321376 title "Seasonal and Multiyear Flow Variability on the Prince of Wales Icefield, Ellesmere Island: 2009–2019" @default.
• W4286321376 cites W131631189 @default.
• W4286321376 cites W1858207246 @default.
• W4286321376 cites W1973320638 @default.
• W4286321376 cites W1987361392 @default.
• W4286321376 cites W1998150864 @default.
• W4286321376 cites W2002529950 @default.
• W4286321376 cites W2003888558 @default.
• W4286321376 cites W2011894267 @default.
• W4286321376 cites W2012092742 @default.
• W4286321376 cites W2019518940 @default.
• W4286321376 cites W2022459931 @default.
• W4286321376 cites W2024978468 @default.
• W4286321376 cites W2030492714 @default.
• W4286321376 cites W2038697952 @default.
• W4286321376 cites W2060035819 @default.
• W4286321376 cites W2090266865 @default.
• W4286321376 cites W2114727579 @default.
• W4286321376 cites W2120925500 @default.
• W4286321376 cites W2131847138 @default.
• W4286321376 cites W2138618655 @default.
• W4286321376 cites W2153709735 @default.
• W4286321376 cites W2154852185 @default.
• W4286321376 cites W2154868551 @default.
• W4286321376 cites W2161823728 @default.
• W4286321376 cites W2162669540 @default.
• W4286321376 cites W2163451218 @default.
• W4286321376 cites W2170210609 @default.
• W4286321376 cites W2279185263 @default.
• W4286321376 cites W2322340310 @default.
• W4286321376 cites W2476382257 @default.
• W4286321376 cites W2555828444 @default.
• W4286321376 cites W2588908043 @default.
• W4286321376 cites W2611570425 @default.
• W4286321376 cites W2627733492 @default.
• W4286321376 cites W2770405948 @default.
• W4286321376 cites W2785384847 @default.
• W4286321376 cites W2787532384 @default.
• W4286321376 cites W2803368100 @default.
• W4286321376 cites W2809202542 @default.
• W4286321376 cites W2921547444 @default.
• W4286321376 cites W2944929577 @default.
• W4286321376 cites W2951206943 @default.
• W4286321376 cites W2971351124 @default.
• W4286321376 cites W2971392059 @default.
• W4286321376 cites W3088969138 @default.
• W4286321376 cites W3119214240 @default.
• W4286321376 cites W3158099307 @default.
• W4286321376 cites W3215965912 @default.
• W4286321376 cites W4253380776 @default.
• W4286321376 cites W4254162371 @default.
• W4286321376 cites W4254975498 @default.
• W4286321376 doi "https://doi.org/10.1029/2021jf006501" @default.
• W4286321376 hasPublicationYear "2022" @default.
• W4286321376 type Work @default.
• W4286321376 citedByCount "0" @default.
• W4286321376 crossrefType "journal-article" @default.
• W4286321376 hasAuthorship W4286321376A5001903581 @default.
• W4286321376 hasAuthorship W4286321376A5025898965 @default.
• W4286321376 hasAuthorship W4286321376A5028080549 @default.
• W4286321376 hasAuthorship W4286321376A5070252251 @default.
• W4286321376 hasAuthorship W4286321376A5082605601 @default.
• W4286321376 hasConcept C100834320 @default.
• W4286321376 hasConcept C100970517 @default.
• W4286321376 hasConcept C104932425 @default.
• W4286321376 hasConcept C111368507 @default.
• W4286321376 hasConcept C114793014 @default.
• W4286321376 hasConcept C127045886 @default.
• W4286321376 hasConcept C127313418 @default.
• W4286321376 hasConcept C136894858 @default.
• W4286321376 hasConcept C154108245 @default.
• W4286321376 hasConcept C197435368 @default.
• W4286321376 hasConcept C205649164 @default.
• W4286321376 hasConcept C49204034 @default.
• W4286321376 hasConcept C65748596 @default.
• W4286321376 hasConcept C81820708 @default.
• W4286321376 hasConceptScore W4286321376C100834320 @default.
• W4286321376 hasConceptScore W4286321376C100970517 @default.
• W4286321376 hasConceptScore W4286321376C104932425 @default.
• W4286321376 hasConceptScore W4286321376C111368507 @default.
• W4286321376 hasConceptScore W4286321376C114793014 @default.
• W4286321376 hasConceptScore W4286321376C127045886 @default.
• W4286321376 hasConceptScore W4286321376C127313418 @default.
• W4286321376 hasConceptScore W4286321376C136894858 @default.
• W4286321376 hasConceptScore W4286321376C154108245 @default.
• W4286321376 hasConceptScore W4286321376C197435368 @default.
• W4286321376 hasConceptScore W4286321376C205649164 @default.
• W4286321376 hasConceptScore W4286321376C49204034 @default.
• W4286321376 hasConceptScore W4286321376C65748596 @default.
• W4286321376 hasConceptScore W4286321376C81820708 @default.
• W4286321376 hasIssue "4" @default.

• next