Transient convection in upper lake sediments produced by internal seiching
Transient convection in upper lake sediments produced by internal seiching
About this item
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Author / Creator
Publisher
Washington, DC: Blackwell Publishing Ltd
Journal title
Language
English
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Publisher
Washington, DC: Blackwell Publishing Ltd
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Scope and Contents
Contents
We present the first evidence of free convection development in lake sediments caused by seiche oscillations. Appearance of the pore water convection is manifested by increase in the upward heat flux during periodical seiche‐driven upwelling of cold deep water over the bottom slope. The dimensionless convective heat flux scales favorably with the s...
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Full title
Transient convection in upper lake sediments produced by internal seiching
Authors, Artists and Contributors
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Record Identifier
TN_cdi_proquest_miscellaneous_1671582141
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1671582141
Other Identifiers
ISSN
0094-8276
E-ISSN
1944-8007
DOI
10.1029/2009GL040064
