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Geothermal heat flux of Ridge B region in Antarctica inferred from basal dry–wet distribution

Geothermal heat flux of Ridge B region in Antarctica inferred from basal dry–wet distribution

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_cf18c9dadfb44709b9986ce5a870ecce

Geothermal heat flux of Ridge B region in Antarctica inferred from basal dry–wet distribution

About this item

Full title

Geothermal heat flux of Ridge B region in Antarctica inferred from basal dry–wet distribution

Publisher

Cambridge, UK: Cambridge University Press

Journal title

Journal of glaciology, 2025-01, Vol.71, Article e12

Language

English

Formats

Publication information

Publisher

Cambridge, UK: Cambridge University Press

More information

Scope and Contents

Contents

Ridge B is one of the least studied areas in Antarctica but has been considered to be a potential location for the oldest ice on Earth. Among important parameters for calculating where very old ice may exist, geothermal heat flux (GHF) is critical but poorly understood. Here, GHF is determined by quantifying the transitions between dry and wet basa...

Alternative Titles

Full title

Geothermal heat flux of Ridge B region in Antarctica inferred from basal dry–wet distribution

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_cf18c9dadfb44709b9986ce5a870ecce

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_cf18c9dadfb44709b9986ce5a870ecce

Other Identifiers

ISSN

0022-1430

E-ISSN

1727-5652

DOI

10.1017/jog.2024.85

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