Mid-depth temperature maximum in an estuarine lake

The mid-depth temperature maximum (TeM) was measured in an estuarine Bol’shoi Vilyui Lake (Kamchatka peninsula, Russia) in summer 2015. We applied 1D k –ε model LAKE to the case, and found it successfully simulating the phenomenon. We argue that the main prerequisite for mid-depth TeM development is...

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Published in:Environmental Research Letters
Main Authors: V M Stepanenko, I A Repina, A Yu Artamonov, S L Gorin, V N Lykossov, D V Kulyamin
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2018
Subjects:
Q
Online Access:https://doi.org/10.1088/1748-9326/aaad75
https://doaj.org/article/7369c3a70fdd410b9ef2f84757abd90a
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spelling ftdoajarticles:oai:doaj.org/article:7369c3a70fdd410b9ef2f84757abd90a 2023-09-05T13:20:46+02:00 Mid-depth temperature maximum in an estuarine lake V M Stepanenko I A Repina A Yu Artamonov S L Gorin V N Lykossov D V Kulyamin 2018-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/aaad75 https://doaj.org/article/7369c3a70fdd410b9ef2f84757abd90a EN eng IOP Publishing https://doi.org/10.1088/1748-9326/aaad75 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aaad75 1748-9326 https://doaj.org/article/7369c3a70fdd410b9ef2f84757abd90a Environmental Research Letters, Vol 13, Iss 3, p 035006 (2018) temperature maximum numerical modelling estuaries meromictic lakes Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2018 ftdoajarticles https://doi.org/10.1088/1748-9326/aaad75 2023-08-13T00:37:37Z The mid-depth temperature maximum (TeM) was measured in an estuarine Bol’shoi Vilyui Lake (Kamchatka peninsula, Russia) in summer 2015. We applied 1D k –ε model LAKE to the case, and found it successfully simulating the phenomenon. We argue that the main prerequisite for mid-depth TeM development is a salinity increase below the freshwater mixed layer, sharp enough in order to increase the temperature with depth not to cause convective mixing and double diffusion there. Given that this condition is satisfied, the TeM magnitude is controlled by physical factors which we identified as: radiation absorption below the mixed layer, mixed-layer temperature dynamics, vertical heat conduction and water-sediments heat exchange. In addition to these, we formulate the mechanism of temperature maximum ‘pumping’, resulting from the phase shift between diurnal cycles of mixed-layer depth and temperature maximum magnitude. Based on the LAKE model results we quantify the contribution of the above listed mechanisms and find their individual significance highly sensitive to water turbidity. Relying on physical mechanisms identified we define environmental conditions favouring the summertime TeM development in salinity-stratified lakes as: small-mixed layer depth (roughly, ~< 2 m), transparent water, daytime maximum of wind and cloudless weather. We exemplify the effect of mixed-layer depth on TeM by a set of selected lakes. Article in Journal/Newspaper Kamchatka Kamchatka Peninsula Directory of Open Access Journals: DOAJ Articles Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) Environmental Research Letters 13 3 035006
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic temperature maximum
numerical modelling
estuaries
meromictic lakes
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
spellingShingle temperature maximum
numerical modelling
estuaries
meromictic lakes
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
V M Stepanenko
I A Repina
A Yu Artamonov
S L Gorin
V N Lykossov
D V Kulyamin
Mid-depth temperature maximum in an estuarine lake
topic_facet temperature maximum
numerical modelling
estuaries
meromictic lakes
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
description The mid-depth temperature maximum (TeM) was measured in an estuarine Bol’shoi Vilyui Lake (Kamchatka peninsula, Russia) in summer 2015. We applied 1D k –ε model LAKE to the case, and found it successfully simulating the phenomenon. We argue that the main prerequisite for mid-depth TeM development is a salinity increase below the freshwater mixed layer, sharp enough in order to increase the temperature with depth not to cause convective mixing and double diffusion there. Given that this condition is satisfied, the TeM magnitude is controlled by physical factors which we identified as: radiation absorption below the mixed layer, mixed-layer temperature dynamics, vertical heat conduction and water-sediments heat exchange. In addition to these, we formulate the mechanism of temperature maximum ‘pumping’, resulting from the phase shift between diurnal cycles of mixed-layer depth and temperature maximum magnitude. Based on the LAKE model results we quantify the contribution of the above listed mechanisms and find their individual significance highly sensitive to water turbidity. Relying on physical mechanisms identified we define environmental conditions favouring the summertime TeM development in salinity-stratified lakes as: small-mixed layer depth (roughly, ~< 2 m), transparent water, daytime maximum of wind and cloudless weather. We exemplify the effect of mixed-layer depth on TeM by a set of selected lakes.
format Article in Journal/Newspaper
author V M Stepanenko
I A Repina
A Yu Artamonov
S L Gorin
V N Lykossov
D V Kulyamin
author_facet V M Stepanenko
I A Repina
A Yu Artamonov
S L Gorin
V N Lykossov
D V Kulyamin
author_sort V M Stepanenko
title Mid-depth temperature maximum in an estuarine lake
title_short Mid-depth temperature maximum in an estuarine lake
title_full Mid-depth temperature maximum in an estuarine lake
title_fullStr Mid-depth temperature maximum in an estuarine lake
title_full_unstemmed Mid-depth temperature maximum in an estuarine lake
title_sort mid-depth temperature maximum in an estuarine lake
publisher IOP Publishing
publishDate 2018
url https://doi.org/10.1088/1748-9326/aaad75
https://doaj.org/article/7369c3a70fdd410b9ef2f84757abd90a
long_lat ENVELOPE(160.000,160.000,56.000,56.000)
geographic Kamchatka Peninsula
geographic_facet Kamchatka Peninsula
genre Kamchatka
Kamchatka Peninsula
genre_facet Kamchatka
Kamchatka Peninsula
op_source Environmental Research Letters, Vol 13, Iss 3, p 035006 (2018)
op_relation https://doi.org/10.1088/1748-9326/aaad75
https://doaj.org/toc/1748-9326
doi:10.1088/1748-9326/aaad75
1748-9326
https://doaj.org/article/7369c3a70fdd410b9ef2f84757abd90a
op_doi https://doi.org/10.1088/1748-9326/aaad75
container_title Environmental Research Letters
container_volume 13
container_issue 3
container_start_page 035006
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