AustralieFrV1, PascalFrancis, Checkpoint, bibRecord, 003136

Internal tides and vertical mixing over the Kerguelen Plateau

Identifieur interne : 003136 ( PascalFrancis/Checkpoint ); précédent : 003135; suivant : 003137

Internal tides and vertical mixing over the Kerguelen Plateau

Auteurs : Young-Hyang Park [France] ; Jean-Luc Fuda [France] ; Isabelle Durand [France] ; Alberto C. Naveira Garabato [Royaume-Uni]

Source :

Deep-sea research. Part 2. Topical studies in oceanography [ 0967-0645 ] ; 2008.

RBID : Pascal:08-0300455

Descripteurs français

Pascal (Inist)
- Onde interne, Mixage, Mélangeage, Fer, Fertilisation, Série temporelle, Phytoplancton, Déplacement, Thermocline, Diffusion tourbillonnaire, Interaction onde, Théorie, Diffusivité, Méthode spectrale, Cisaillement, Déformation sous contrainte, Circulation océanique, Préconditionnement, Dynamique, Plateau Kerguelen.
Wicri :
- topic : Fer, Préconditionnement.

English descriptors

KwdEn :
- Eddy diffusion, Kerguelen Plateau, Mixing, Preconditioning, Spectral method, Time series, Wave interaction, diffusivity, displacements, dynamics, fertilization, internal waves, iron, mixing, ocean circulation, phytoplankton, shear, strain, theory, thermocline.

Abstract

Within the context of the natural iron-fertilization study KEOPS, time series measurements of CTD and LADCP profiles at a site (50,6°S, 72°E; 528m) coinciding with an annual phytoplankton bloom over the Kerguelen Plateau were made during the January-February 2005 KEOPS cruise. An important activity of highly nonlinear semidiurnal internal tides having peak-to-peak isopycnal displacements of up to 80m is identified. These internal tides appear to be a principal agent for promoting elevated vertical mixing indispensable for upward transfer of iron within the seasonal thermocline. We estimate local vertical eddy diffusivities of the order of 4 × 10^-4 m² s^-1 using a Thorpe scale analysis. Although this estimate is higher by an order of magnitude than the canonical value O (0.1 x 10^-4m²s^-1) in the open ocean away from boundaries, it is consistent with nonlinear internal wave/wave interaction theories, as verified by independent diffusivity estimates using the vertical wavenumber spectral methods for shear and strain. It is also suggested that the general ocean circulation may play an important role in preconditioning the bloom in that the relatively sluggish circulation over the shallow plateau (compared to the much more dynamic neighbouring deep ocean) may foster the bloom's observed annual recurrence over the plateau.

Affiliations:

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Le document en format XML

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<term>Wave interaction</term>
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<front><div type="abstract" xml:lang="en">Within the context of the natural iron-fertilization study KEOPS, time series measurements of CTD and LADCP profiles at a site (50,6°S, 72°E; 528m) coinciding with an annual phytoplankton bloom over the Kerguelen Plateau were made during the January-February 2005 KEOPS cruise. An important activity of highly nonlinear semidiurnal internal tides having peak-to-peak isopycnal displacements of up to 80m is identified. These internal tides appear to be a principal agent for promoting elevated vertical mixing indispensable for upward transfer of iron within the seasonal thermocline. We estimate local vertical eddy diffusivities of the order of 4 × 10<sup>-4</sup>
 m<sup>2</sup>
 s<sup>-1</sup>
 using a Thorpe scale analysis. Although this estimate is higher by an order of magnitude than the canonical value O (0.1 x 10<sup>-4</sup>
m<sup>2</sup>
s<sup>-1</sup>
) in the open ocean away from boundaries, it is consistent with nonlinear internal wave/wave interaction theories, as verified by independent diffusivity estimates using the vertical wavenumber spectral methods for shear and strain. It is also suggested that the general ocean circulation may play an important role in preconditioning the bloom in that the relatively sluggish circulation over the shallow plateau (compared to the much more dynamic neighbouring deep ocean) may foster the bloom's observed annual recurrence over the plateau.</div>
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 m<sup>2</sup>
 s<sup>-1</sup>
 using a Thorpe scale analysis. Although this estimate is higher by an order of magnitude than the canonical value O (0.1 x 10<sup>-4</sup>
m<sup>2</sup>
s<sup>-1</sup>
) in the open ocean away from boundaries, it is consistent with nonlinear internal wave/wave interaction theories, as verified by independent diffusivity estimates using the vertical wavenumber spectral methods for shear and strain. It is also suggested that the general ocean circulation may play an important role in preconditioning the bloom in that the relatively sluggish circulation over the shallow plateau (compared to the much more dynamic neighbouring deep ocean) may foster the bloom's observed annual recurrence over the plateau.</s0>
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<fC03 i1="15" i2="2" l="ENG"><s0>shear</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Cizalladura</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Déformation sous contrainte</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>strain</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Deformación bajo tensión</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Circulation océanique</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>ocean circulation</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Circulación oceánica</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="X" l="FRE"><s0>Préconditionnement</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="ENG"><s0>Preconditioning</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="SPA"><s0>Precondicionamiento</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Dynamique</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>dynamics</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Dinámica</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Plateau Kerguelen</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>Kerguelen Plateau</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Plancton</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>plankton</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Plancton</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Océan Indien</s0>
<s2>564</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Indian Ocean</s0>
<s2>564</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Océano Indico</s0>
<s2>564</s2>
</fC07>
<fN21><s1>189</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
<affiliations><list><country><li>France</li>
<li>Royaume-Uni</li>
</country>
<region><li>Provence-Alpes-Côte d'Azur</li>
<li>Île-de-France</li>
</region>
<settlement><li>Marseille</li>
<li>Paris</li>
</settlement>
</list>
<tree><country name="France"><region name="Île-de-France"><name sortKey="Park, Young Hyang" sort="Park, Young Hyang" uniqKey="Park Y" first="Young-Hyang" last="Park">Young-Hyang Park</name>
</region>
<name sortKey="Durand, Isabelle" sort="Durand, Isabelle" uniqKey="Durand I" first="Isabelle" last="Durand">Isabelle Durand</name>
<name sortKey="Fuda, Jean Luc" sort="Fuda, Jean Luc" uniqKey="Fuda J" first="Jean-Luc" last="Fuda">Jean-Luc Fuda</name>
</country>
<country name="Royaume-Uni"><noRegion><name sortKey="Naveira Garabato, Alberto C" sort="Naveira Garabato, Alberto C" uniqKey="Naveira Garabato A" first="Alberto C." last="Naveira Garabato">Alberto C. Naveira Garabato</name>
</noRegion>
</country>
</tree>
</affiliations>
</record>

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   |texte=   Internal tides and vertical mixing over the Kerguelen Plateau
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This area was generated with Dilib version V0.6.33.
Data generation: Tue Dec 5 10:43:12 2017. Site generation: Tue Mar 5 14:07:20 2024

	Serveur d'exploration sur les relations entre la France et l'Australie
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Serveur d'exploration sur les relations entre la France et l'Australie

Internal tides and vertical mixing over the Kerguelen Plateau

Internal tides and vertical mixing over the Kerguelen Plateau

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