https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&feed=atom&action=history
Internal Tide Energy Conversion - Revision history
2024-03-28T16:30:27Z
Revision history for this page on the wiki
MediaWiki 1.38.1
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=405&oldid=prev
Taylorgasher: categorical
2019-05-20T11:58:12Z
<p>categorical</p>
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Taylorgasher
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=269&oldid=prev
Taylorgasher: added version tag
2019-02-07T15:30:55Z
<p>added version tag</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:30, 7 February 2019</td>
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<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">{{ADC version|version=53.01|relation=ge}} </ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Internal tide energy conversion refers to the energy conversion from barotropic to baroclinic modes as surface tides flow over steep and rough topography in the deep ocean generating internal tides. The "lost" barotropic tidal energy is often accounted for through a linear friction term in large-scale numerical models that are barotropic or not fine-scaled enough to resolve the energy conversion. It is implemented in ADCIRC through a spatially varying nodal attribute called [[fort.13_file#Internal_Tide_Energy_Conversion|internal_tide_friction]], in the [[fort.13 file]].</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Internal tide energy conversion refers to the energy conversion from barotropic to baroclinic modes as surface tides flow over steep and rough topography in the deep ocean generating internal tides. The "lost" barotropic tidal energy is often accounted for through a linear friction term in large-scale numerical models that are barotropic or not fine-scaled enough to resolve the energy conversion. It is implemented in ADCIRC through a spatially varying nodal attribute called [[fort.13_file#Internal_Tide_Energy_Conversion|internal_tide_friction]], in the [[fort.13 file]].</div></td></tr>
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Taylorgasher
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=242&oldid=prev
Taylorgasher: Modified link
2019-02-02T21:03:38Z
<p>Modified link</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 17:03, 2 February 2019</td>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Internal tide energy conversion refers to the energy conversion from barotropic to baroclinic modes as surface tides flow over steep and rough topography in the deep ocean generating internal tides. The "lost" barotropic tidal energy is often accounted for through a linear friction term in large-scale numerical models that are barotropic or not fine-scaled enough to resolve the energy conversion. It is implemented in ADCIRC through a spatially varying nodal attribute called [[internal_tide_friction]], in the [[fort.13 file]].</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Internal tide energy conversion refers to the energy conversion from barotropic to baroclinic modes as surface tides flow over steep and rough topography in the deep ocean generating internal tides. The "lost" barotropic tidal energy is often accounted for through a linear friction term in large-scale numerical models that are barotropic or not fine-scaled enough to resolve the energy conversion. It is implemented in ADCIRC through a spatially varying nodal attribute called [[<ins style="font-weight: bold; text-decoration: none;">fort.13_file#Internal_Tide_Energy_Conversion|</ins>internal_tide_friction]], in the [[fort.13 file]].</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td></tr>
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Taylorgasher
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=238&oldid=prev
Taylorgasher: Grammar and some language fixes
2019-02-02T20:43:12Z
<p>Grammar and some language fixes</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:43, 2 February 2019</td>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Internal tide energy conversion refers to the energy conversion from barotropic to baroclinic modes as surface tides flow over steep and rough topography in the deep ocean generating internal tides. The "lost" barotropic tidal energy is often accounted for through a linear friction term in large-scale numerical models that are barotropic or not fine-scaled enough to resolve the energy conversion. It is implemented in ADCIRC through a spatially varying <del style="font-weight: bold; text-decoration: none;">[[</del>nodal attribute<del style="font-weight: bold; text-decoration: none;">]] </del>called [[internal_tide_friction]], in the [[fort.13 file]].</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Internal tide energy conversion refers to the energy conversion from barotropic to baroclinic modes as surface tides flow over steep and rough topography in the deep ocean generating internal tides. The "lost" barotropic tidal energy is often accounted for through a linear friction term in large-scale numerical models that are barotropic or not fine-scaled enough to resolve the energy conversion. It is implemented in ADCIRC through a spatially varying nodal attribute called [[internal_tide_friction]], in the [[fort.13 file]].</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Attribute Summary ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Attribute Summary ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>In a computational domain covering a large portion of the deep ocean <del style="font-weight: bold; text-decoration: none;">it is critical to include </del>the effect of internal tide energy conversion to obtain more accurate tidal solutions. The user should only elect to use the internal_tide_friction nodal attribute when tides are included in the simulation through tidal boundary conditions and tidal potential functions. The attribute <del style="font-weight: bold; text-decoration: none;">is unnecessary </del>for domains that are small in size and/or do not cover a significant portion of the deep ocean (<del style="font-weight: bold; text-decoration: none;">taken here to mean </del>the portion of the ocean excluding the continental shelf). </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>In a computational domain covering a large portion of the deep ocean<ins style="font-weight: bold; text-decoration: none;">, </ins>the effect of internal tide energy conversion <ins style="font-weight: bold; text-decoration: none;">may be needed </ins>to obtain more accurate tidal solutions. The user should only elect to use the internal_tide_friction nodal attribute when tides are included in the simulation through tidal boundary conditions and tidal potential functions. The attribute <ins style="font-weight: bold; text-decoration: none;">may not be important </ins>for domains that are small in size and/or do not cover a significant portion of the <ins style="font-weight: bold; text-decoration: none;">"</ins>deep ocean<ins style="font-weight: bold; text-decoration: none;">" </ins>(the portion of the ocean excluding the continental shelf). </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>ADCIRC reads the internal_tide_friction attribute in as the ''IT_Fric'' variable, which can have 1 (scalar) or 3 (tensor) dimensions. The attribute has dimensions of [1/time], meaning that it is a linear friction term which is multiplied by the velocity in the governing equations, and is normalized by the ocean depth prior to simulation. Hence, it ignores the water surface elevation portion of the total water depth, which is reasonable since the term and theory it is based on is only applicable to deep ocean. Typically, it is only applied to ocean depths greater than 100-500 m.<ref name="Pringle2018"></ref><ref name="Arbic2010"></ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>ADCIRC reads the internal_tide_friction attribute in as the ''IT_Fric'' variable, which can have 1 (scalar) or 3 (tensor) dimensions. The attribute has dimensions of [1/time], meaning that it is a linear friction term which is multiplied by the velocity in the governing equations, and is normalized by the ocean depth prior to simulation. Hence, it ignores the water surface elevation portion of the total water depth, which is reasonable since the term and theory it is based on is only applicable to deep ocean. Typically, it is only applied to ocean depths greater than 100-500 m.<ref name="Pringle2018"></ref><ref name="Arbic2010"></ref></div></td></tr>
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Taylorgasher
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=223&oldid=prev
Taylorgasher: /* Background and Theory */
2019-02-02T17:36:15Z
<p><span dir="auto"><span class="autocomment">Background and Theory</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:36, 2 February 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The basic theory for generation of internal tides in the deep ocean was established several decades ago.<ref name="Bell1975">T.H. Bell, Topographically generated internal waves in the open ocean, J. Geophys. Res. 80 (1975) 320–327. doi:10.1029/JC080i003p00320.</ref> However, it was not thought to be incredibly important to the global energy balance of the surface tides until the modern satellite era when it was discovered that internal tides are responsible for approximately 30% of the global barotropic tidal dissipation.<ref name="Garrett2007">C. Garrett, E. Kunze, Internal Tide Generation in the Deep Ocean, Annu. Rev. Fluid Mech. 39 (2007) 57–87. doi:10.1146/annurev.fluid.39.050905.110227.</ref><ref>G.D. Egbert, R.D. Ray, Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data, Nature. 405 (2000) 775–778. doi:10.1038/35015531</ref><ref>G.D. Egbert, R.D. Ray, Estimates of M2 tidal energy dissipation from TOPEX/Poseidon altimeter data, J. Geophys. Res. Ocean. 106 (2001) 22475–22502. doi:10.1029/2000JC000699.</ref> </div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The basic theory for generation of internal tides in the deep ocean was established several decades ago.<ref name="Bell1975">T.H. Bell, Topographically generated internal waves in the open ocean, J. Geophys. Res. 80 (1975) 320–327. doi:10.1029/JC080i003p00320.</ref> However, it was not thought to be incredibly important to the global energy balance of the surface tides until the modern satellite era when it was discovered that internal tides are responsible for approximately 30% of the global barotropic tidal dissipation.<ref name="Garrett2007">C. Garrett, E. Kunze, Internal Tide Generation in the Deep Ocean, Annu. Rev. Fluid Mech. 39 (2007) 57–87. doi:10.1146/annurev.fluid.39.050905.110227.</ref><ref>G.D. Egbert, R.D. Ray, Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data, Nature. 405 (2000) 775–778. doi:10.1038/35015531</ref><ref>G.D. Egbert, R.D. Ray, Estimates of M2 tidal energy dissipation from TOPEX/Poseidon altimeter data, J. Geophys. Res. Ocean. 106 (2001) 22475–22502. doi:10.1029/2000JC000699.</ref> </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Following this revelation the past two decades have been subject to a number of theoretical</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Following this revelation<ins style="font-weight: bold; text-decoration: none;">, </ins>the past two decades have been subject to a number of theoretical</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>A. Melet, M. Nikurashin, C. Muller, S. Falahat, J. Nycander, P.G. Timko, B.K. Arbic, J.A. Goff, Internal tide generation by abyssal hills using analytical theory, J. Geophys. Res. Ocean. 118 (2013) 6303–6318. doi:10.1002/2013JC009212.</ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>A. Melet, M. Nikurashin, C. Muller, S. Falahat, J. Nycander, P.G. Timko, B.K. Arbic, J.A. Goff, Internal tide generation by abyssal hills using analytical theory, J. Geophys. Res. Ocean. 118 (2013) 6303–6318. doi:10.1002/2013JC009212.</ref></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>F. Pétrélis, S.L. Smith, W.R. Young, F. Pétrélis, S.L. Smith, W.R. Young, Tidal Conversion at a Submarine Ridge, J. Phys. Oceanogr. 36 (2006) 1053–1071. doi:10.1175/JPO2879.1.</ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>F. Pétrélis, S.L. Smith, W.R. Young, F. Pétrélis, S.L. Smith, W.R. Young, Tidal Conversion at a Submarine Ridge, J. Phys. Oceanogr. 36 (2006) 1053–1071. doi:10.1175/JPO2879.1.</ref></div></td></tr>
</table>
Taylorgasher
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=218&oldid=prev
Wpringle at 22:37, 27 January 2019
2019-01-27T22:37:11Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 18:37, 27 January 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>A. Lefauve, C. Muller, A. Melet, A three-dimensional map of tidal dissipation over abyssal hills, J. Geophys. Res. C Ocean. 120 (2015) 4760–4777. doi:10.1002/2014JC010598.</ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>A. Lefauve, C. Muller, A. Melet, A three-dimensional map of tidal dissipation over abyssal hills, J. Geophys. Res. C Ocean. 120 (2015) 4760–4777. doi:10.1002/2014JC010598.</ref></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>M.H. Alford, T. Peacock, J. a MacKinnon, J.D. Nash, M.C. Buijsman, L.R. Centuroni, S.-Y. Chao, M.-H. Chang, D.M. Farmer, O.B. Fringer, K.-H. Fu, P.C. Gallacher, H.C. Graber, K.R. Helfrich, S.M. Jachec, C.R. Jackson, J.M. Klymak, D.S. Ko, S. Jan, T.M.S. Johnston, S. Legg, I.-H. Lee, R.-C. Lien, M.J. Mercier, J.N. Moum, R. Musgrave, J.-H. Park, A.I. Pickering, R. Pinkel, L. Rainville, S.R. Ramp, D.L. Rudnick, S. Sarkar, A. Scotti, H.L. Simmons, L.C. St Laurent, S.K. Venayagamoorthy, Y.-H. Wang, J. Wang, Y.J. Yang, T. Paluszkiewicz, T.-Y.D. Tang, The formation and fate of internal waves in the South China Sea., Nature. 521 (2015) 65–9. doi:10.1038/nature14399.</ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>M.H. Alford, T. Peacock, J. a MacKinnon, J.D. Nash, M.C. Buijsman, L.R. Centuroni, S.-Y. Chao, M.-H. Chang, D.M. Farmer, O.B. Fringer, K.-H. Fu, P.C. Gallacher, H.C. Graber, K.R. Helfrich, S.M. Jachec, C.R. Jackson, J.M. Klymak, D.S. Ko, S. Jan, T.M.S. Johnston, S. Legg, I.-H. Lee, R.-C. Lien, M.J. Mercier, J.N. Moum, R. Musgrave, J.-H. Park, A.I. Pickering, R. Pinkel, L. Rainville, S.R. Ramp, D.L. Rudnick, S. Sarkar, A. Scotti, H.L. Simmons, L.C. St Laurent, S.K. Venayagamoorthy, Y.-H. Wang, J. Wang, Y.J. Yang, T. Paluszkiewicz, T.-Y.D. Tang, The formation and fate of internal waves in the South China Sea., Nature. 521 (2015) 65–9. doi:10.1038/nature14399.</ref></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>investigations into internal tide generation and their effects on the surface tides through <del style="font-weight: bold; text-decoration: none;">parameterizations</del>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>investigations into internal tide generation and their effects on the surface tides through <ins style="font-weight: bold; text-decoration: none;">parameterization of the energy conversion in large-scale numerical tidal models</ins>.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>S.R. Jayne, L.C. St. Laurent, Parameterizing tidal dissipation over rough topography, Geophys. Res. Lett. 28 (2001) 811–814. doi:10.1029/2000GL012044.</ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>S.R. Jayne, L.C. St. Laurent, Parameterizing tidal dissipation over rough topography, Geophys. Res. Lett. 28 (2001) 811–814. doi:10.1029/2000GL012044.</ref></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>M.C. Buijsman, B.K. Arbic, J.A.M. Green, R.W. Helber, J.G. Richman, J.F. Shriver, P.G. Timko, A. Wallcraft, Optimizing internal wave drag in a forward barotropic model with semidiurnal tides, Ocean Model. 85 (2015) 42–55. doi:10.1016/j.ocemod.2014.11.003.</ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div><ref>M.C. Buijsman, B.K. Arbic, J.A.M. Green, R.W. Helber, J.G. Richman, J.F. Shriver, P.G. Timko, A. Wallcraft, Optimizing internal wave drag in a forward barotropic model with semidiurnal tides, Ocean Model. 85 (2015) 42–55. doi:10.1016/j.ocemod.2014.11.003.</ref></div></td></tr>
</table>
Wpringle
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=217&oldid=prev
Wpringle at 22:35, 27 January 2019
2019-01-27T22:35:41Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 18:35, 27 January 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Specifying ''IT_Fric'' Values ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Specifying ''IT_Fric'' Values ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>''IT_Fric'' values are determined through analytical formulations based on Bell's linear theory<ref name="Bell1975"></ref>, valid in what is called sub-critical topography<ref name="Garrett2007"><<del style="font-weight: bold; text-decoration: none;">\</del>ref><del style="font-weight: bold; text-decoration: none;">. </del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>''IT_Fric'' values are determined through analytical formulations based on Bell's linear theory<ref name="Bell1975"></ref>, valid in what is called sub-critical topography<ins style="font-weight: bold; text-decoration: none;">.</ins><ref name="Garrett2007"><<ins style="font-weight: bold; text-decoration: none;">/</ins>ref> </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Recent publications using ADCIRC<ref name="Pringle2018"></ref><ref name="Pringle2018a"></ref> provide relevant formulation and implementation details. </div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Recent publications using ADCIRC<ref name="Pringle2018"></ref><ref name="Pringle2018a"></ref> provide relevant formulation and implementation details. </div></td></tr>
</table>
Wpringle
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=216&oldid=prev
Wpringle at 22:34, 27 January 2019
2019-01-27T22:34:36Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 18:34, 27 January 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The basic theory for generation of internal tides in the deep ocean was established several decades ago.<ref>C. Garrett, E. Kunze, Internal Tide Generation in the Deep Ocean, Annu. Rev. Fluid Mech. 39 (2007) 57–87. doi:10.1146/annurev.fluid.39.050905.110227.</ref></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>The basic theory for generation of internal tides in the deep ocean was established several decades ago.<ref <ins style="font-weight: bold; text-decoration: none;">name="Bell1975">T.H. Bell, Topographically generated internal waves in the open ocean, J. Geophys. Res. 80 (1975) 320–327. doi:10.1029/JC080i003p00320.</ref> However, it was not thought to be incredibly important to the global energy balance of the surface tides until the modern satellite era when it was discovered that internal tides are responsible for approximately 30% of the global barotropic tidal dissipation.<ref name="Garrett2007"</ins>>C. Garrett, E. Kunze, Internal Tide Generation in the Deep Ocean, Annu. Rev. Fluid Mech. 39 (2007) 57–87. doi:10.1146/annurev.fluid.39.050905.110227<ins style="font-weight: bold; text-decoration: none;">.</ref><ref>G.D. Egbert, R.D. Ray, Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data, Nature. 405 (2000) 775–778. doi:10.1038/35015531</ref><ref>G.D. Egbert, R.D. Ray, Estimates of M2 tidal energy dissipation from TOPEX/Poseidon altimeter data, J. Geophys. Res. Ocean. 106 (2001) 22475–22502. doi:10.1029/2000JC000699</ins>.</ref> </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">How it was known that internal energy conversion is important </del>to the <del style="font-weight: bold; text-decoration: none;">global energy balance </del>of the <del style="font-weight: bold; text-decoration: none;">surface </del>tides.<ref><del style="font-weight: bold; text-decoration: none;">G</del>.D. <del style="font-weight: bold; text-decoration: none;">Egbert</del>, R.D. <del style="font-weight: bold; text-decoration: none;">Ray</del>, <del style="font-weight: bold; text-decoration: none;">Significant dissipation </del>of <del style="font-weight: bold; text-decoration: none;">tidal energy </del>in the <del style="font-weight: bold; text-decoration: none;">deep ocean inferred from satellite altimeter data</del>, Nature. <del style="font-weight: bold; text-decoration: none;">405 </del>(<del style="font-weight: bold; text-decoration: none;">2000</del>) <del style="font-weight: bold; text-decoration: none;">775–778</del>. doi:10.1038/<del style="font-weight: bold; text-decoration: none;">35015531</del></ref><ref>G.D. <del style="font-weight: bold; text-decoration: none;">Egbert</del>, <del style="font-weight: bold; text-decoration: none;">R</del>.D. <del style="font-weight: bold; text-decoration: none;">Ray</del>, <del style="font-weight: bold; text-decoration: none;">Estimates </del>of <del style="font-weight: bold; text-decoration: none;">M2 </del>tidal <del style="font-weight: bold; text-decoration: none;">energy dissipation from TOPEX</del>/<del style="font-weight: bold; text-decoration: none;">Poseidon altimeter data</del>, J. <del style="font-weight: bold; text-decoration: none;">Geophys</del>. <del style="font-weight: bold; text-decoration: none;">Res</del>. <del style="font-weight: bold; text-decoration: none;">Ocean</del>. <del style="font-weight: bold; text-decoration: none;">106 </del>(<del style="font-weight: bold; text-decoration: none;">2001</del>) <del style="font-weight: bold; text-decoration: none;">22475–22502</del>. doi:10.<del style="font-weight: bold; text-decoration: none;">1029</del>/<del style="font-weight: bold; text-decoration: none;">2000JC000699</del>.</ref></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Following this revelation the past two decades have been subject </ins>to <ins style="font-weight: bold; text-decoration: none;">a number of theoretical</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>A. Melet, M. Nikurashin, C. Muller, S. Falahat, J. Nycander, P.G. Timko, B.K. Arbic, J.A. Goff, Internal tide generation by abyssal hills using analytical theory, J. Geophys. Res. Ocean. 118 (2013) 6303–6318. doi:10.1002/2013JC009212.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>F. Pétrélis, S.L. Smith, W.R. Young, F. Pétrélis, S.L. Smith, W.R. Young, Tidal Conversion at a Submarine Ridge, J. Phys. Oceanogr. 36 (2006) 1053–1071. doi:10.1175/JPO2879.1.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>L. St. Laurent, C. Garrett, The Role of Internal Tides in Mixing </ins>the <ins style="font-weight: bold; text-decoration: none;">Deep Ocean, J. Phys. Oceanogr. 32 (2002) 2882–2899. doi:10.1175/1520-0485(2002)032<2882:TROITI>2.0.CO;2.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>L. St. Laurent, S. Stringer, C. Garrett, D. Perrault-Joncas, The generation of internal tides at abrupt topography, Deep Sea Res. Part I Oceanogr. Res. Pap. 50 (2003) 987–1003. doi:10.1016/S0967-0637(03)00096-7.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">and numerical </ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>J. Nycander, Generation </ins>of <ins style="font-weight: bold; text-decoration: none;">internal waves in </ins>the <ins style="font-weight: bold; text-decoration: none;">deep ocean by </ins>tides<ins style="font-weight: bold; text-decoration: none;">, J. Geophys. Res. 110 (2005) C10028. doi:10.1029/2004JC002487.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>A. Lefauve, C. Muller, A. Melet, A three-dimensional map of tidal dissipation over abyssal hills, J. Geophys. Res. C Ocean. 120 (2015) 4760–4777. doi:10.1002/2014JC010598</ins>.<<ins style="font-weight: bold; text-decoration: none;">/</ins>ref></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>M.H. Alford, T. Peacock, J. a MacKinnon, J.D. Nash, M.C. Buijsman, L.R. Centuroni, S.-Y. Chao, M.-H. Chang, D.M. Farmer, O.B. Fringer, K.-H. Fu, P.C. Gallacher, H.C. Graber, K.R. Helfrich, S.M. Jachec, C.R. Jackson, J.M</ins>. <ins style="font-weight: bold; text-decoration: none;">Klymak, </ins>D.<ins style="font-weight: bold; text-decoration: none;">S. Ko, S. Jan, T.M.S. Johnston, S. Legg, I.-H. Lee, R.-C. Lien, M.J. Mercier, J.N. Moum, R. Musgrave, J.-H. Park, A.I. Pickering, R. Pinkel, L. Rainville</ins>, <ins style="font-weight: bold; text-decoration: none;">S.</ins>R<ins style="font-weight: bold; text-decoration: none;">. Ramp, D.L. Rudnick, S. Sarkar, A. Scotti, H.L. Simmons, L.C. St Laurent, S.K. Venayagamoorthy, Y.-H. Wang, J. Wang, Y.J. Yang, T. Paluszkiewicz, T.-Y</ins>.D. <ins style="font-weight: bold; text-decoration: none;">Tang</ins>, <ins style="font-weight: bold; text-decoration: none;">The formation and fate </ins>of <ins style="font-weight: bold; text-decoration: none;">internal waves </ins>in the <ins style="font-weight: bold; text-decoration: none;">South China Sea.</ins>, Nature. <ins style="font-weight: bold; text-decoration: none;">521 </ins>(<ins style="font-weight: bold; text-decoration: none;">2015</ins>) <ins style="font-weight: bold; text-decoration: none;">65–9</ins>. doi:10.1038/<ins style="font-weight: bold; text-decoration: none;">nature14399.</ins></ref></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">investigations into internal tide generation and their effects on the surface tides through parameterizations.</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ref><ins style="font-weight: bold; text-decoration: none;">S.R. Jayne, L.C. St. Laurent, Parameterizing tidal dissipation over rough topography, Geophys. Res. Lett. 28 (2001) 811–814. doi:10.1029/2000GL012044.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>M.C. Buijsman, B.K. Arbic, J.A.M. Green, R.W. Helber, J.</ins>G. <ins style="font-weight: bold; text-decoration: none;">Richman, J.F. Shriver, P.G. Timko, A. Wallcraft, Optimizing internal wave drag in a forward barotropic model with semidiurnal tides, Ocean Model. 85 (2015) 42–55. doi:10.1016/j.ocemod.2014.11.003.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref name="Pringle2018">W.J. Pringle, </ins>D. <ins style="font-weight: bold; text-decoration: none;">Wirasaet, A. Suhardjo, J. Meixner, J.J. Westerink, A.B. Kennedy, S. Nong, Finite-Element Barotropic Model for the Indian and Western Pacific Oceans: Tidal Model-Data Comparisons and Sensitivities, Ocean Model. 129 (2018) 13–38. doi:10.1016/j.ocemod.2018.07.003.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref name="Pringle2018a">W.J. Pringle, D. Wirasaet, J.J. Westerink, Modifications to Internal Tide Conversion Parameterizations and Implementation into Barotropic Ocean Models, EarthArXiv. (2018) 9. doi:10.31223/osf.io/84w53.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref name="Arbic2010">B.K. Arbic, A.J. Wallcraft, E.J. Metzger, Concurrent simulation of the eddying general circulation and tides in a global ocean model, Ocean Model. 32 (2010) 175–187. doi:10.1016/j.ocemod.2010.01.007.</ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>A. Schmittner</ins>, <ins style="font-weight: bold; text-decoration: none;">G</ins>.D. <ins style="font-weight: bold; text-decoration: none;">Egbert</ins>, <ins style="font-weight: bold; text-decoration: none;">An improved parameterization </ins>of tidal <ins style="font-weight: bold; text-decoration: none;">mixing for ocean models, Geosci. Model Dev. 7 (2014) 211–224. doi:10.5194/gmd-7-211-2014.<</ins>/<ins style="font-weight: bold; text-decoration: none;">ref></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><ref>J.A.M. Green</ins>, J. <ins style="font-weight: bold; text-decoration: none;">Nycander, A Comparison of Tidal Conversion Parameterizations for Tidal Models, J</ins>. <ins style="font-weight: bold; text-decoration: none;">Phys</ins>. <ins style="font-weight: bold; text-decoration: none;">Oceanogr</ins>. <ins style="font-weight: bold; text-decoration: none;">43 </ins>(<ins style="font-weight: bold; text-decoration: none;">2013</ins>) <ins style="font-weight: bold; text-decoration: none;">104–119</ins>. doi:10.<ins style="font-weight: bold; text-decoration: none;">1175</ins>/<ins style="font-weight: bold; text-decoration: none;">JPO-D-12-023.1</ins>.</ref></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Attribute Summary ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Attribute Summary ==</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>In a computational domain covering a large portion of the deep ocean it is critical to include the effect of internal tide energy conversion to obtain more accurate tidal solutions. The user should only elect to use the internal_tide_friction nodal attribute when tides are included in the simulation through tidal boundary conditions and tidal potential functions. The attribute is unnecessary for domains that are small in size and/or do not cover a significant portion of the deep ocean (taken here to mean the portion of the ocean excluding the continental shelf). </div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>In a computational domain covering a large portion of the deep ocean it is critical to include the effect of internal tide energy conversion to obtain more accurate tidal solutions. The user should only elect to use the internal_tide_friction nodal attribute when tides are included in the simulation through tidal boundary conditions and tidal potential functions. The attribute is unnecessary for domains that are small in size and/or do not cover a significant portion of the deep ocean (taken here to mean the portion of the ocean excluding the continental shelf). </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>ADCIRC reads the internal_tide_friction attribute in as the ''IT_Fric'' variable, which can have 1 (scalar) or 3 (tensor) dimensions. The attribute has dimensions of [1/time], meaning that it is a linear friction term which is multiplied by the velocity in the governing equations, and is normalized by the ocean depth prior to simulation. Hence, it ignores the water surface elevation portion of the total water depth, which is reasonable since the term and theory it is based on is only applicable to deep ocean. Typically, it is only applied to ocean depths greater than 100-500 m.<ref name="Pringle2018"><del style="font-weight: bold; text-decoration: none;">W.J. Pringle, D. Wirasaet, A. Suhardjo, J. Meixner, J.J. Westerink, A.B. Kennedy, S. Nong, Finite-Element Barotropic Model for the Indian and Western Pacific Oceans: Tidal Model-Data Comparisons and Sensitivities, Ocean Model. 129 (2018) 13–38. doi:10.1016/j.ocemod.2018.07.003.</del></ref><ref><del style="font-weight: bold; text-decoration: none;">B.K. Arbic, A.J. Wallcraft, E.J. Metzger, Concurrent simulation of the eddying general circulation and tides in a global ocean model, Ocean Model. 32 (2010) 175–187. doi:10.1016/j.ocemod.2010.01.007.</del></ref></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>ADCIRC reads the internal_tide_friction attribute in as the ''IT_Fric'' variable, which can have 1 (scalar) or 3 (tensor) dimensions. The attribute has dimensions of [1/time], meaning that it is a linear friction term which is multiplied by the velocity in the governing equations, and is normalized by the ocean depth prior to simulation. Hence, it ignores the water surface elevation portion of the total water depth, which is reasonable since the term and theory it is based on is only applicable to deep ocean. Typically, it is only applied to ocean depths greater than 100-500 m.<ref name="Pringle2018"></ref><ref <ins style="font-weight: bold; text-decoration: none;">name="Arbic2010"</ins>></ref></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Specifying ''IT_Fric'' Values ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Specifying ''IT_Fric'' Values ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>''IT_Fric'' values are determined through analytical formulations based on Bell's linear theory<ref name="Bell1975"><del style="font-weight: bold; text-decoration: none;">T.H. Bell, Topographically generated internal waves in the open ocean, J. Geophys. Res. 80 (1975) 320–327. doi:10.1029/JC080i003p00320.</del></ref>, valid in what is called sub-critical topography. </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>''IT_Fric'' values are determined through analytical formulations based on Bell's linear theory<ref name="Bell1975"></ref>, valid in what is called sub-critical topography<ins style="font-weight: bold; text-decoration: none;"><ref name="Garrett2007"><\ref></ins>. </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Recent publications using ADCIRC<ref name="Pringle2018"></ref><ref><del style="font-weight: bold; text-decoration: none;">W.J. Pringle, D. Wirasaet, J.J. Westerink, Modifications to Internal Tide Conversion Parameterizations and Implementation into Barotropic Ocean Models, EarthArXiv. (2018) 9. doi:10.31223/osf.io/84w53.</del></ref> provide relevant formulation and implementation details. </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Recent publications using ADCIRC<ref name="Pringle2018"></ref><ref <ins style="font-weight: bold; text-decoration: none;">name="Pringle2018a"</ins>></ref> provide relevant formulation and implementation details. </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td></tr>
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Wpringle
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=215&oldid=prev
Wpringle: /* Background and Theory */
2019-01-27T22:14:02Z
<p><span dir="auto"><span class="autocomment">Background and Theory</span></span></p>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Background and Theory ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">For a review</del>.<ref>C. Garrett, E. Kunze, Internal Tide Generation in the Deep Ocean, Annu. Rev. Fluid Mech. 39 (2007) 57–87. doi:10.1146/annurev.fluid.39.050905.110227.</ref></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">The basic theory for generation of internal tides in the deep ocean was established several decades ago</ins>.<ref>C. Garrett, E. Kunze, Internal Tide Generation in the Deep Ocean, Annu. Rev. Fluid Mech. 39 (2007) 57–87. doi:10.1146/annurev.fluid.39.050905.110227.</ref></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>How it was known that internal energy conversion is important to the global energy balance of the surface tides.<ref>G.D. Egbert, R.D. Ray, Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data, Nature. 405 (2000) 775–778. doi:10.1038/35015531</ref><ref>G.D. Egbert, R.D. Ray, Estimates of M2 tidal energy dissipation from TOPEX/Poseidon altimeter data, J. Geophys. Res. Ocean. 106 (2001) 22475–22502. doi:10.1029/2000JC000699.</ref></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>How it was known that internal energy conversion is important to the global energy balance of the surface tides.<ref>G.D. Egbert, R.D. Ray, Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data, Nature. 405 (2000) 775–778. doi:10.1038/35015531</ref><ref>G.D. Egbert, R.D. Ray, Estimates of M2 tidal energy dissipation from TOPEX/Poseidon altimeter data, J. Geophys. Res. Ocean. 106 (2001) 22475–22502. doi:10.1029/2000JC000699.</ref></div></td></tr>
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Wpringle
https://wiki.adcirc.org/index.php?title=Internal_Tide_Energy_Conversion&diff=214&oldid=prev
Wpringle at 22:10, 27 January 2019
2019-01-27T22:10:33Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 18:10, 27 January 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>In a computational domain covering a large portion of the deep ocean it is critical to include the effect of internal tide energy conversion to obtain more accurate tidal solutions. The user should only elect to use the internal_tide_friction nodal attribute when tides are included in the simulation through tidal boundary conditions and tidal potential functions. The attribute is unnecessary for domains that are small in size and/or do not cover a significant portion of the deep ocean (taken here to mean the portion of the ocean excluding the continental shelf). </div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>In a computational domain covering a large portion of the deep ocean it is critical to include the effect of internal tide energy conversion to obtain more accurate tidal solutions. The user should only elect to use the internal_tide_friction nodal attribute when tides are included in the simulation through tidal boundary conditions and tidal potential functions. The attribute is unnecessary for domains that are small in size and/or do not cover a significant portion of the deep ocean (taken here to mean the portion of the ocean excluding the continental shelf). </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>ADCIRC reads the internal_tide_friction attribute in as the ''IT_Fric'' variable, which can have 1 (scalar) or 3 (tensor) dimensions. The attribute has dimensions of [1/time], meaning that it is a linear friction term which is multiplied by the velocity in the governing equations, and is normalized by the ocean depth prior to simulation. Hence, it ignores the water surface elevation portion of the total water depth, which is reasonable since the term and theory it is based on is only applicable to deep ocean. Typically, it is only applied to ocean depths greater than 100-500 m.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>ADCIRC reads the internal_tide_friction attribute in as the ''IT_Fric'' variable, which can have 1 (scalar) or 3 (tensor) dimensions. The attribute has dimensions of [1/time], meaning that it is a linear friction term which is multiplied by the velocity in the governing equations, and is normalized by the ocean depth prior to simulation. Hence, it ignores the water surface elevation portion of the total water depth, which is reasonable since the term and theory it is based on is only applicable to deep ocean. Typically, it is only applied to ocean depths greater than 100-500 m.<ins style="font-weight: bold; text-decoration: none;"><ref name="Pringle2018">W.J. Pringle, D. Wirasaet, A. Suhardjo, J. Meixner, J.J. Westerink, A.B. Kennedy, S. Nong, Finite-Element Barotropic Model for the Indian and Western Pacific Oceans: Tidal Model-Data Comparisons and Sensitivities, Ocean Model. 129 (2018) 13–38. doi:10.1016/j.ocemod.2018.07.003.</ref><ref>B.K. Arbic, A.J. Wallcraft, E.J. Metzger, Concurrent simulation of the eddying general circulation and tides in a global ocean model, Ocean Model. 32 (2010) 175–187. doi:10.1016/j.ocemod.2010.01.007.</ref></ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Specifying ''IT_Fric'' Values ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Specifying ''IT_Fric'' Values ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>''IT_Fric'' values are determined through analytical formulations based on Bell's linear theory<ref name="Bell1975"><del style="font-weight: bold; text-decoration: none;">{{cite journal|last1=Bell|first1=</del>T.H.<del style="font-weight: bold; text-decoration: none;">|title=</del>Topographically generated internal waves in the open ocean<del style="font-weight: bold; text-decoration: none;">|journal=Journal of Geophysical Research|volume=</del>80<del style="font-weight: bold; text-decoration: none;">|year=</del>1975<del style="font-weight: bold; text-decoration: none;">|pages=</del>320–327<del style="font-weight: bold; text-decoration: none;">|</del>doi<del style="font-weight: bold; text-decoration: none;">=</del>10.1029/JC080i003p00320<del style="font-weight: bold; text-decoration: none;">}}</del></ref>, valid in what is called sub-critical topography. </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>''IT_Fric'' values are determined through analytical formulations based on Bell's linear theory<ref name="Bell1975">T.H. <ins style="font-weight: bold; text-decoration: none;">Bell, </ins>Topographically generated internal waves in the open ocean<ins style="font-weight: bold; text-decoration: none;">, J. Geophys. Res. </ins>80 <ins style="font-weight: bold; text-decoration: none;">(</ins>1975<ins style="font-weight: bold; text-decoration: none;">) </ins>320–327<ins style="font-weight: bold; text-decoration: none;">. </ins>doi<ins style="font-weight: bold; text-decoration: none;">:</ins>10.1029/JC080i003p00320<ins style="font-weight: bold; text-decoration: none;">.</ins></ref>, valid in what is called sub-critical topography. </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Recent publications using ADCIRC<ref><del style="font-weight: bold; text-decoration: none;">W.J. Pringle, D. Wirasaet, A. Suhardjo, J. Meixner, J.J. Westerink, A.B. Kennedy, S. Nong, Finite-Element Barotropic Model for the Indian and Western Pacific Oceans: Tidal Model-Data Comparisons and Sensitivities, Ocean Model. 129 (2018) 13–38. doi:10.1016/j.ocemod.2018.07.003.</del></ref><ref>W.J. Pringle, D. Wirasaet, J.J. Westerink, Modifications to Internal Tide Conversion Parameterizations and Implementation into Barotropic Ocean Models, EarthArXiv. (2018) 9. doi:10.31223/osf.io/84w53.</ref> provide relevant formulation and implementation details. </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Recent publications using ADCIRC<ref <ins style="font-weight: bold; text-decoration: none;">name="Pringle2018"</ins>></ref><ref>W.J. Pringle, D. Wirasaet, J.J. Westerink, Modifications to Internal Tide Conversion Parameterizations and Implementation into Barotropic Ocean Models, EarthArXiv. (2018) 9. doi:10.31223/osf.io/84w53.</ref> provide relevant formulation and implementation details. </div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td></tr>
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Wpringle