Diagnostics of isopycnal mixing in a circumpolar channel
• We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The d...
Ausführliche Beschreibung
Autor*in: |
Abernathey, Ryan [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2013 |
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Schlagwörter: |
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Umfang: |
16 |
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Übergeordnetes Werk: |
Enthalten in: Laser sharpening evaluation of diamond wheels based on 3D recognition - Zhou, Wei ELSEVIER, 2022, Amsterdam [u.a.] |
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Übergeordnetes Werk: |
volume:72 ; year:2013 ; pages:1-16 ; extent:16 |
Links: |
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DOI / URN: |
10.1016/j.ocemod.2013.07.004 |
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Katalog-ID: |
ELV038556227 |
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520 | |a • We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. | ||
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10.1016/j.ocemod.2013.07.004 doi GBVA2013003000013.pica (DE-627)ELV038556227 (ELSEVIER)S1463-5003(13)00120-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 550 670 VZ 51.79 bkl Abernathey, Ryan verfasserin aut Diagnostics of isopycnal mixing in a circumpolar channel 2013 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. Eddy diffusivity Elsevier Isopycnal mixing Elsevier Mesoscale eddies Elsevier Antarctic Circumpolar Current Elsevier Ferreira, David oth Klocker, Andreas oth Enthalten in Elsevier Science Zhou, Wei ELSEVIER Laser sharpening evaluation of diamond wheels based on 3D recognition 2022 Amsterdam [u.a.] (DE-627)ELV008583811 volume:72 year:2013 pages:1-16 extent:16 https://doi.org/10.1016/j.ocemod.2013.07.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 51.79 Sonstige Werkstoffe VZ AR 72 2013 1-16 16 045F 550 |
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10.1016/j.ocemod.2013.07.004 doi GBVA2013003000013.pica (DE-627)ELV038556227 (ELSEVIER)S1463-5003(13)00120-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 550 670 VZ 51.79 bkl Abernathey, Ryan verfasserin aut Diagnostics of isopycnal mixing in a circumpolar channel 2013 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. Eddy diffusivity Elsevier Isopycnal mixing Elsevier Mesoscale eddies Elsevier Antarctic Circumpolar Current Elsevier Ferreira, David oth Klocker, Andreas oth Enthalten in Elsevier Science Zhou, Wei ELSEVIER Laser sharpening evaluation of diamond wheels based on 3D recognition 2022 Amsterdam [u.a.] (DE-627)ELV008583811 volume:72 year:2013 pages:1-16 extent:16 https://doi.org/10.1016/j.ocemod.2013.07.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 51.79 Sonstige Werkstoffe VZ AR 72 2013 1-16 16 045F 550 |
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10.1016/j.ocemod.2013.07.004 doi GBVA2013003000013.pica (DE-627)ELV038556227 (ELSEVIER)S1463-5003(13)00120-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 550 670 VZ 51.79 bkl Abernathey, Ryan verfasserin aut Diagnostics of isopycnal mixing in a circumpolar channel 2013 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. Eddy diffusivity Elsevier Isopycnal mixing Elsevier Mesoscale eddies Elsevier Antarctic Circumpolar Current Elsevier Ferreira, David oth Klocker, Andreas oth Enthalten in Elsevier Science Zhou, Wei ELSEVIER Laser sharpening evaluation of diamond wheels based on 3D recognition 2022 Amsterdam [u.a.] (DE-627)ELV008583811 volume:72 year:2013 pages:1-16 extent:16 https://doi.org/10.1016/j.ocemod.2013.07.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 51.79 Sonstige Werkstoffe VZ AR 72 2013 1-16 16 045F 550 |
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10.1016/j.ocemod.2013.07.004 doi GBVA2013003000013.pica (DE-627)ELV038556227 (ELSEVIER)S1463-5003(13)00120-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 550 670 VZ 51.79 bkl Abernathey, Ryan verfasserin aut Diagnostics of isopycnal mixing in a circumpolar channel 2013 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. Eddy diffusivity Elsevier Isopycnal mixing Elsevier Mesoscale eddies Elsevier Antarctic Circumpolar Current Elsevier Ferreira, David oth Klocker, Andreas oth Enthalten in Elsevier Science Zhou, Wei ELSEVIER Laser sharpening evaluation of diamond wheels based on 3D recognition 2022 Amsterdam [u.a.] (DE-627)ELV008583811 volume:72 year:2013 pages:1-16 extent:16 https://doi.org/10.1016/j.ocemod.2013.07.004 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 51.79 Sonstige Werkstoffe VZ AR 72 2013 1-16 16 045F 550 |
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• We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. |
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• We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. |
abstract_unstemmed |
• We examine lateral mixing in an idealized model which resembles the Antarctic Circumpolar Current. • Diffusivities are computed for passive and active tracers, including potential vorticity and buoyancy. • Diffusivities are also estimated from simulated float and tracerrelease experiments. • The disparate methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient. |
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Diagnostics of isopycnal mixing in a circumpolar channel |
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methods agree, showing a strong mid-depth maximum in isopycnal mixing. • The isopycnal mixing rate is not the same as the Gent–McWilliams transfer coefficient.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Eddy diffusivity</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Isopycnal mixing</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Mesoscale eddies</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Antarctic Circumpolar Current</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ferreira, David</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Klocker, Andreas</subfield><subfield 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