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Seasonality of density currents induced by differential cooling

Seasonality of density currents induced by differential cooling

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_ef61efc39aa843eb886ae0b1c73960c2

Seasonality of density currents induced by differential cooling

About this item

Full title

Seasonality of density currents induced by differential cooling

Publisher

Katlenburg-Lindau: Copernicus GmbH

Journal title

Hydrology and earth system sciences, 2022-01, Vol.26 (2), p.331-353

Language

English

Formats

Publication information

Publisher

Katlenburg-Lindau: Copernicus GmbH

More information

Scope and Contents

Contents

When lakes experience surface cooling, the shallow littoral region cools faster than the deep pelagic waters. The lateral density gradient resulting from this differential cooling can trigger a cold downslope density current that intrudes at the base of the mixed layer during stratified conditions. This process is known as a thermal siphon (TS). TS...

Alternative Titles

Full title

Seasonality of density currents induced by differential cooling

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_ef61efc39aa843eb886ae0b1c73960c2

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_ef61efc39aa843eb886ae0b1c73960c2

Other Identifiers

ISSN

1607-7938,1027-5606

E-ISSN

1607-7938

DOI

10.5194/hess-26-331-2022

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