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Transition of flow regime along a marine-terminating outlet glacier in East Antarctica

Transition of flow regime along a marine-terminating outlet glacier in East Antarctica

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_10b4af6a4c14424bb748d91dfa629f48

Transition of flow regime along a marine-terminating outlet glacier in East Antarctica

About this item

Full title

Transition of flow regime along a marine-terminating outlet glacier in East Antarctica

Publisher

Copernicus GmbH

Journal title

The cryosphere, 2014-05, Vol.8 (3), p.867-875

Language

English

Formats

Publication information

Publisher

Copernicus GmbH

More information

Scope and Contents

Contents

We present results of a multi-methodological approach to characterize the flow regime of West Ragnhild Glacier, the widest glacier in Dronning Maud Land, Antarctica. A new airborne radar survey points to substantially thicker ice (>2000 m) than previously thought. With a discharge estimate of 13–14 Gt yr−1, West Ragnhild Glacier thus becomes of the...

Alternative Titles

Full title

Transition of flow regime along a marine-terminating outlet glacier in East Antarctica

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_10b4af6a4c14424bb748d91dfa629f48

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_10b4af6a4c14424bb748d91dfa629f48

Other Identifiers

ISSN

1994-0424,1994-0416

E-ISSN

1994-0424,1994-0416

DOI

10.5194/tc-8-867-2014

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