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Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the...

Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_0d43b962c3314e44833892b987b3c39b

Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the European Alps

About this item

Full title

Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the European Alps

Publisher

Katlenburg-Lindau: Copernicus GmbH

Journal title

Climate of the past, 2023-09, Vol.19 (9), p.1805-1823

Language

English

Formats

Publication information

Publisher

Katlenburg-Lindau: Copernicus GmbH

More information

Scope and Contents

Contents

Evidence that during the Last Glacial Maximum (LGM) glaciers extended well into the piedmont plains is still identifiable in the alpine foreland as a system of well-preserved moraines. Glaciers are strongly controlled by temperature and precipitation, and therefore, they are excellent indicators of climate change. Here, we use a regional climate mo...

Alternative Titles

Full title

Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the European Alps

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_0d43b962c3314e44833892b987b3c39b

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_0d43b962c3314e44833892b987b3c39b

Other Identifiers

ISSN

1814-9332,1814-9324

E-ISSN

1814-9332

DOI

10.5194/cp-19-1805-2023

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