The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of Okhotsk

The properties and dynamics of internal waves in the ocean crucially depend on the vertical structure of water masses. We present detailed analysis of the impact of spatial and seasonal variations in the density-driven stratification in the Sea of Okhotsk on the properties of the classic kinematic a...

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Main Authors: Oxana E. Kurkina, Tatyana G. Talipova, Tarmo Soomere, Andrey A. Kurkin, Artem V. Rybin
Format: Article
Language:English
Published: Estonian Academy Publishers 2017-11-01
Series:Estonian Journal of Earth Sciences
Subjects:
Online Access:http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2017/issue_4/earth-2017-4-238-255.pdf
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author Oxana E. Kurkina
Tatyana G. Talipova
Tarmo Soomere
Andrey A. Kurkin
Artem V. Rybin
author_facet Oxana E. Kurkina
Tatyana G. Talipova
Tarmo Soomere
Andrey A. Kurkin
Artem V. Rybin
author_sort Oxana E. Kurkina
collection DOAJ
description The properties and dynamics of internal waves in the ocean crucially depend on the vertical structure of water masses. We present detailed analysis of the impact of spatial and seasonal variations in the density-driven stratification in the Sea of Okhotsk on the properties of the classic kinematic and nonlinear parameters of internal waves in this water body. The resulting maps of the phase speed of long internal waves and coefficients at various terms of the underlying Gardner’s equation make it possible to rapidly determine the main properties of internal solitary waves in the region and to choose an adequate set of parameters of the relevant numerical models. It is shown that the phase speed of long internal waves almost does not depend on the particular season. The coefficient at the quadratic term of the underlying evolution equation is predominantly negative in summer and winter and therefore internal solitons usually have negative polarity. Numerical simulations of the formation of internal solitons and solibores indicate that seasonal variations in the coefficient at the cubic term of Gardner’s equation lead to substantial variations in the shape of solibores.
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spelling doaj.art-53edd3294632451fb05cbed80be7c2552022-12-22T03:02:53ZengEstonian Academy PublishersEstonian Journal of Earth Sciences1736-47281736-75572017-11-0166423825510.3176/earth.2017.2010.3176/earth.2017.20The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of OkhotskOxana E. Kurkina0Tatyana G. Talipova1Tarmo Soomere2Andrey A. Kurkin3Artem V. Rybin4Nizhny Novgorod State Technical University n.a. R.E. Alekseev, 603950 Nizhny Novgorod, RussiaNizhny Novgorod State Technical University n.a. R.E. Alekseev, 603950 Nizhny Novgorod, Russia / Institute of Applied Physics, 603950 Nizhny Novgorod, RussiaDepartment of Cybernetics, School of Science, Tallinn University of Technology, 12618 Tallinn, Estonia; tarmo.soomere@cs.ioc.ee / Estonian Academy of Sciences, Kohtu 6, 10130 Tallinn, EstoniaNizhny Novgorod State Technical University n.a. R.E. Alekseev, 603950 Nizhny Novgorod, RussiaNizhny Novgorod State Technical University n.a. R.E. Alekseev, 603950 Nizhny Novgorod, RussiaThe properties and dynamics of internal waves in the ocean crucially depend on the vertical structure of water masses. We present detailed analysis of the impact of spatial and seasonal variations in the density-driven stratification in the Sea of Okhotsk on the properties of the classic kinematic and nonlinear parameters of internal waves in this water body. The resulting maps of the phase speed of long internal waves and coefficients at various terms of the underlying Gardner’s equation make it possible to rapidly determine the main properties of internal solitary waves in the region and to choose an adequate set of parameters of the relevant numerical models. It is shown that the phase speed of long internal waves almost does not depend on the particular season. The coefficient at the quadratic term of the underlying evolution equation is predominantly negative in summer and winter and therefore internal solitons usually have negative polarity. Numerical simulations of the formation of internal solitons and solibores indicate that seasonal variations in the coefficient at the cubic term of Gardner’s equation lead to substantial variations in the shape of solibores.http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2017/issue_4/earth-2017-4-238-255.pdfinternal wavesstratificationinternal solitonsGardner’s equationSea of Okhotsk.
spellingShingle Oxana E. Kurkina
Tatyana G. Talipova
Tarmo Soomere
Andrey A. Kurkin
Artem V. Rybin
The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of Okhotsk
Estonian Journal of Earth Sciences
internal waves
stratification
internal solitons
Gardner’s equation
Sea of Okhotsk.
title The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of Okhotsk
title_full The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of Okhotsk
title_fullStr The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of Okhotsk
title_full_unstemmed The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of Okhotsk
title_short The impact of seasonal changes in stratification on the dynamics of internal waves in the Sea of Okhotsk
title_sort impact of seasonal changes in stratification on the dynamics of internal waves in the sea of okhotsk
topic internal waves
stratification
internal solitons
Gardner’s equation
Sea of Okhotsk.
url http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2017/issue_4/earth-2017-4-238-255.pdf
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