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Nonlinear Dynamics of Deep Open-Ocean Convection : An Analytical Approach. / Kovalevsky, Dmitry V.; Bashmachnikov, Igor L.

The Many Facets of Complexity Science. Springer Nature, 2021. стр. 161-183 (Nonlinear Physical Science).

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › глава/раздел › научная › Рецензирование

Harvard

Kovalevsky, DV & Bashmachnikov, IL 2021, Nonlinear Dynamics of Deep Open-Ocean Convection: An Analytical Approach. в The Many Facets of Complexity Science. Nonlinear Physical Science, Springer Nature, стр. 161-183. https://doi.org/10.1007/978-981-16-2853-5_10

APA

Kovalevsky, D. V., & Bashmachnikov, I. L. (2021). Nonlinear Dynamics of Deep Open-Ocean Convection: An Analytical Approach. в The Many Facets of Complexity Science (стр. 161-183). (Nonlinear Physical Science). Springer Nature. https://doi.org/10.1007/978-981-16-2853-5_10

Vancouver

Kovalevsky DV, Bashmachnikov IL. Nonlinear Dynamics of Deep Open-Ocean Convection: An Analytical Approach. в The Many Facets of Complexity Science. Springer Nature. 2021. стр. 161-183. (Nonlinear Physical Science). https://doi.org/10.1007/978-981-16-2853-5_10

Author

Kovalevsky, Dmitry V. ; Bashmachnikov, Igor L. / Nonlinear Dynamics of Deep Open-Ocean Convection : An Analytical Approach. The Many Facets of Complexity Science. Springer Nature, 2021. стр. 161-183 (Nonlinear Physical Science).

BibTeX

@inbook{0b48318737114eecbfb61fde1cf9d58e,
title = "Nonlinear Dynamics of Deep Open-Ocean Convection: An Analytical Approach",
abstract = "Deep open-ocean convection is a complex multiscale nonlinear dynamical phenomenon observed in few localized regions of the World Ocean. The results of Whitehead{\textquoteright}s {\textquoteleft}tank model{\textquoteright} [Whitehead, Stratified convection with multiple states, Ocean Modelling, 2(3–4), 109–121, 2000] show that the dynamic system, that includes a deep convection in a localized convective site and water exchange with a neighboring ocean basin, can exist in multiple steady states. We generalize this {\textquoteleft}tank model{\textquoteright} for the case of non-zero salinity of the upper layer, which brings the model closer to the real ocean conditions. We then derive exact analytical solutions of the nonlinear transitional dynamics for different model dynamic regimes, and discuss oceanographic implications of the modified model.",
author = "Kovalevsky, {Dmitry V.} and Bashmachnikov, {Igor L.}",
note = "Publisher Copyright: {\textcopyright} 2021, Higher Education Press.",
year = "2021",
doi = "10.1007/978-981-16-2853-5_10",
language = "English",
series = "Nonlinear Physical Science",
publisher = "Springer Nature",
pages = "161--183",
booktitle = "The Many Facets of Complexity Science",
address = "Germany",

}

RIS

TY - CHAP

T1 - Nonlinear Dynamics of Deep Open-Ocean Convection

T2 - An Analytical Approach

AU - Kovalevsky, Dmitry V.

AU - Bashmachnikov, Igor L.

N1 - Publisher Copyright: © 2021, Higher Education Press.

PY - 2021

Y1 - 2021

N2 - Deep open-ocean convection is a complex multiscale nonlinear dynamical phenomenon observed in few localized regions of the World Ocean. The results of Whitehead’s ‘tank model’ [Whitehead, Stratified convection with multiple states, Ocean Modelling, 2(3–4), 109–121, 2000] show that the dynamic system, that includes a deep convection in a localized convective site and water exchange with a neighboring ocean basin, can exist in multiple steady states. We generalize this ‘tank model’ for the case of non-zero salinity of the upper layer, which brings the model closer to the real ocean conditions. We then derive exact analytical solutions of the nonlinear transitional dynamics for different model dynamic regimes, and discuss oceanographic implications of the modified model.

AB - Deep open-ocean convection is a complex multiscale nonlinear dynamical phenomenon observed in few localized regions of the World Ocean. The results of Whitehead’s ‘tank model’ [Whitehead, Stratified convection with multiple states, Ocean Modelling, 2(3–4), 109–121, 2000] show that the dynamic system, that includes a deep convection in a localized convective site and water exchange with a neighboring ocean basin, can exist in multiple steady states. We generalize this ‘tank model’ for the case of non-zero salinity of the upper layer, which brings the model closer to the real ocean conditions. We then derive exact analytical solutions of the nonlinear transitional dynamics for different model dynamic regimes, and discuss oceanographic implications of the modified model.

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UR - https://www.mendeley.com/catalogue/96715ff9-ba69-3abc-8f9f-c2e43a80b6aa/

U2 - 10.1007/978-981-16-2853-5_10

DO - 10.1007/978-981-16-2853-5_10

M3 - Chapter

AN - SCOPUS:85114337227

T3 - Nonlinear Physical Science

SP - 161

EP - 183

BT - The Many Facets of Complexity Science

PB - Springer Nature

ER -

ID: 85481614