The Response of the Water Surface Layer to Internal Turbulence and Surface Forcing
We have carried out an experimental study of the turbulence kinetic energy dissipation rate (<inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula>), temperature dissipation rate (<inline-formula&g...
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Language: | English |
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MDPI AG
2021-02-01
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Series: | Journal of Marine Science and Engineering |
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Online Access: | https://www.mdpi.com/2077-1312/9/2/217 |
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record_format |
Article |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Mohammad Barzegar Darek Bogucki Brian K. Haus Mingming Shao |
spellingShingle |
Mohammad Barzegar Darek Bogucki Brian K. Haus Mingming Shao The Response of the Water Surface Layer to Internal Turbulence and Surface Forcing Journal of Marine Science and Engineering turbulence non-breaking wave water surface layer convection |
author_facet |
Mohammad Barzegar Darek Bogucki Brian K. Haus Mingming Shao |
author_sort |
Mohammad Barzegar |
title |
The Response of the Water Surface Layer to Internal Turbulence and Surface Forcing |
title_short |
The Response of the Water Surface Layer to Internal Turbulence and Surface Forcing |
title_full |
The Response of the Water Surface Layer to Internal Turbulence and Surface Forcing |
title_fullStr |
The Response of the Water Surface Layer to Internal Turbulence and Surface Forcing |
title_full_unstemmed |
The Response of the Water Surface Layer to Internal Turbulence and Surface Forcing |
title_sort |
response of the water surface layer to internal turbulence and surface forcing |
publisher |
MDPI AG |
series |
Journal of Marine Science and Engineering |
issn |
2077-1312 |
publishDate |
2021-02-01 |
description |
We have carried out an experimental study of the turbulence kinetic energy dissipation rate (<inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula>), temperature dissipation rate (<inline-formula><math display="inline"><semantics><mi>χ</mi></semantics></math></inline-formula>), and turbulent heat flux (THF) within the water surface layer in the presence of non-breaking wave, surface convection, and horizontal heat and eddy fluxes that play a prominent role in the front. We noted that the non-breaking wave dominates <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> values within the surface layer. While analyzing the vertical <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> variability, the presence of a wave-affected layer from the water surface to a depth of <inline-formula><math display="inline"><semantics><mrow><mi>z</mi><mo>≈</mo><mn>1.25</mn><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></mrow></semantics></math></inline-formula> is observed, where <inline-formula><math display="inline"><semantics><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></semantics></math></inline-formula> is the wavelength. <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> associated with non-breaking waves ranged to <inline-formula><math display="inline"><semantics><mrow><mn>4.9</mn><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>6</mn></mrow></msup></mrow></semantics></math></inline-formula>–<inline-formula><math display="inline"><semantics><mrow><mn>7</mn><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>6</mn></mrow></msup></mrow></semantics></math></inline-formula> m<sup>2</sup>/s<sup>3</sup> for the wavelength range of 0.038 m < <inline-formula><math display="inline"><semantics><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></semantics></math></inline-formula> < 0.098 m categorized as the gravity and gravity-capillary wave regimes. <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> values increase for longer <inline-formula><math display="inline"><semantics><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></semantics></math></inline-formula> and non-breaking wave <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> values represent their significant contribution to the ocean energy budget and dynamic of surface layer considering that the non-breaking wave covers the large fraction of ocean surface. We also found that the surface mean square slope (MSS) and wave generated <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> have the same order of magnitude, i.e., MSS <inline-formula><math display="inline"><semantics><mrow><mo>∼</mo><mi>ϵ</mi></mrow></semantics></math></inline-formula>. Besides, we have documented that the small-scale temperature fluctuation change (i.e., <inline-formula><math display="inline"><semantics><mi>χ</mi></semantics></math></inline-formula>) is consistent with the large-scale temperature gradient change (i.e., <inline-formula><math display="inline"><semantics><mrow><mi>d</mi><mo><</mo><mi>T</mi><mo>></mo><mo>/</mo><mi>d</mi><mi>z</mi></mrow></semantics></math></inline-formula>). The value of the THF is approximately constant within the surface layer. It represents that the measured THF near the water surface can be considered a surface water THF, challenging to measure directly. |
topic |
turbulence non-breaking wave water surface layer convection |
url |
https://www.mdpi.com/2077-1312/9/2/217 |
work_keys_str_mv |
AT mohammadbarzegar theresponseofthewatersurfacelayertointernalturbulenceandsurfaceforcing AT darekbogucki theresponseofthewatersurfacelayertointernalturbulenceandsurfaceforcing AT briankhaus theresponseofthewatersurfacelayertointernalturbulenceandsurfaceforcing AT mingmingshao theresponseofthewatersurfacelayertointernalturbulenceandsurfaceforcing AT mohammadbarzegar responseofthewatersurfacelayertointernalturbulenceandsurfaceforcing AT darekbogucki responseofthewatersurfacelayertointernalturbulenceandsurfaceforcing AT briankhaus responseofthewatersurfacelayertointernalturbulenceandsurfaceforcing AT mingmingshao responseofthewatersurfacelayertointernalturbulenceandsurfaceforcing |
_version_ |
1721548634475986944 |
spelling |
doaj-c1b4ea4a3ee84afc902ce352fa532c452021-04-02T19:32:55ZengMDPI AGJournal of Marine Science and Engineering2077-13122021-02-01921721710.3390/jmse9020217The Response of the Water Surface Layer to Internal Turbulence and Surface ForcingMohammad Barzegar0Darek Bogucki1Brian K. Haus2Mingming Shao3Department of Physical and Environmental Sciences, Texas A&M University, Corpus Christi, TX 78412, USADepartment of Physical and Environmental Sciences, Texas A&M University, Corpus Christi, TX 78412, USARosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL 33149, USARosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL 33149, USAWe have carried out an experimental study of the turbulence kinetic energy dissipation rate (<inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula>), temperature dissipation rate (<inline-formula><math display="inline"><semantics><mi>χ</mi></semantics></math></inline-formula>), and turbulent heat flux (THF) within the water surface layer in the presence of non-breaking wave, surface convection, and horizontal heat and eddy fluxes that play a prominent role in the front. We noted that the non-breaking wave dominates <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> values within the surface layer. While analyzing the vertical <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> variability, the presence of a wave-affected layer from the water surface to a depth of <inline-formula><math display="inline"><semantics><mrow><mi>z</mi><mo>≈</mo><mn>1.25</mn><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></mrow></semantics></math></inline-formula> is observed, where <inline-formula><math display="inline"><semantics><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></semantics></math></inline-formula> is the wavelength. <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> associated with non-breaking waves ranged to <inline-formula><math display="inline"><semantics><mrow><mn>4.9</mn><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>6</mn></mrow></msup></mrow></semantics></math></inline-formula>–<inline-formula><math display="inline"><semantics><mrow><mn>7</mn><mo>×</mo><msup><mn>10</mn><mrow><mo>−</mo><mn>6</mn></mrow></msup></mrow></semantics></math></inline-formula> m<sup>2</sup>/s<sup>3</sup> for the wavelength range of 0.038 m < <inline-formula><math display="inline"><semantics><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></semantics></math></inline-formula> < 0.098 m categorized as the gravity and gravity-capillary wave regimes. <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> values increase for longer <inline-formula><math display="inline"><semantics><msub><mi>λ</mi><mi mathvariant="normal">w</mi></msub></semantics></math></inline-formula> and non-breaking wave <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> values represent their significant contribution to the ocean energy budget and dynamic of surface layer considering that the non-breaking wave covers the large fraction of ocean surface. We also found that the surface mean square slope (MSS) and wave generated <inline-formula><math display="inline"><semantics><mi>ϵ</mi></semantics></math></inline-formula> have the same order of magnitude, i.e., MSS <inline-formula><math display="inline"><semantics><mrow><mo>∼</mo><mi>ϵ</mi></mrow></semantics></math></inline-formula>. Besides, we have documented that the small-scale temperature fluctuation change (i.e., <inline-formula><math display="inline"><semantics><mi>χ</mi></semantics></math></inline-formula>) is consistent with the large-scale temperature gradient change (i.e., <inline-formula><math display="inline"><semantics><mrow><mi>d</mi><mo><</mo><mi>T</mi><mo>></mo><mo>/</mo><mi>d</mi><mi>z</mi></mrow></semantics></math></inline-formula>). The value of the THF is approximately constant within the surface layer. It represents that the measured THF near the water surface can be considered a surface water THF, challenging to measure directly.https://www.mdpi.com/2077-1312/9/2/217turbulencenon-breaking wavewater surface layerconvection |