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Control of the temperature signal in Antarctic proxies by snowfall dynamics

Control of the temperature signal in Antarctic proxies by snowfall dynamics

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_7f1b9e3b16024ec5a011de6b24d51c27

Control of the temperature signal in Antarctic proxies by snowfall dynamics

About this item

Full title

Control of the temperature signal in Antarctic proxies by snowfall dynamics

Publisher

Katlenburg-Lindau: Copernicus GmbH

Journal title

The cryosphere, 2023-12, Vol.17 (12), p.5373-5389

Language

English

Formats

Publication information

Publisher

Katlenburg-Lindau: Copernicus GmbH

More information

Scope and Contents

Contents

Antarctica, the coldest and driest continent, is home to the largest ice sheet, whose mass is predominantly recharged by snowfall. A common feature of polar regions is the warming associated with snowfall, as moist oceanic air and cloud cover increase the surface temperature. Consequently, snow that accumulates on the ice sheet is deposited under u...

Alternative Titles

Full title

Control of the temperature signal in Antarctic proxies by snowfall dynamics

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_7f1b9e3b16024ec5a011de6b24d51c27

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_7f1b9e3b16024ec5a011de6b24d51c27

Other Identifiers

ISSN

1994-0424,1994-0416

E-ISSN

1994-0424,1994-0416

DOI

10.5194/tc-17-5373-2023

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