Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex
Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are consider...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhmur, V. V. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. |
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| Übergeordnetes Werk: |
Enthalten in: Izvestiya - Moscow : MAIK Nauka/Interperiodica Publ., 2006, 57(2021), 6 vom: Nov., Seite 632-641 |
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| Übergeordnetes Werk: |
volume:57 ; year:2021 ; number:6 ; month:11 ; pages:632-641 |
| Links: |
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| DOI / URN: |
10.1134/S0001433821050157 |
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| Katalog-ID: |
SPR050392778 |
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| 520 | |a Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). | ||
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| 700 | 1 | |a Belonenko, T. V. |4 aut | |
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10.1134/S0001433821050157 doi (DE-627)SPR050392778 (SPR)S0001433821050157-e DE-627 ger DE-627 rakwb eng Zhmur, V. V. verfasserin aut Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). Novoselova, E. V. aut Belonenko, T. V. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 57(2021), 6 vom: Nov., Seite 632-641 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:57 year:2021 number:6 month:11 pages:632-641 https://dx.doi.org/10.1134/S0001433821050157 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 57 2021 6 11 632-641 |
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10.1134/S0001433821050157 doi (DE-627)SPR050392778 (SPR)S0001433821050157-e DE-627 ger DE-627 rakwb eng Zhmur, V. V. verfasserin aut Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). Novoselova, E. V. aut Belonenko, T. V. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 57(2021), 6 vom: Nov., Seite 632-641 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:57 year:2021 number:6 month:11 pages:632-641 https://dx.doi.org/10.1134/S0001433821050157 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 57 2021 6 11 632-641 |
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10.1134/S0001433821050157 doi (DE-627)SPR050392778 (SPR)S0001433821050157-e DE-627 ger DE-627 rakwb eng Zhmur, V. V. verfasserin aut Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). Novoselova, E. V. aut Belonenko, T. V. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 57(2021), 6 vom: Nov., Seite 632-641 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:57 year:2021 number:6 month:11 pages:632-641 https://dx.doi.org/10.1134/S0001433821050157 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 57 2021 6 11 632-641 |
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10.1134/S0001433821050157 doi (DE-627)SPR050392778 (SPR)S0001433821050157-e DE-627 ger DE-627 rakwb eng Zhmur, V. V. verfasserin aut Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). Novoselova, E. V. aut Belonenko, T. V. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 57(2021), 6 vom: Nov., Seite 632-641 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:57 year:2021 number:6 month:11 pages:632-641 https://dx.doi.org/10.1134/S0001433821050157 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 57 2021 6 11 632-641 |
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10.1134/S0001433821050157 doi (DE-627)SPR050392778 (SPR)S0001433821050157-e DE-627 ger DE-627 rakwb eng Zhmur, V. V. verfasserin aut Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). Novoselova, E. V. aut Belonenko, T. V. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 57(2021), 6 vom: Nov., Seite 632-641 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:57 year:2021 number:6 month:11 pages:632-641 https://dx.doi.org/10.1134/S0001433821050157 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 57 2021 6 11 632-641 |
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V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2021</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. 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Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex |
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potential vorticity in the ocean: ertel and rossby approaches with estimates for the lofoten vortex |
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Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex |
| abstract |
Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. |
| abstractGer |
Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. |
| abstract_unstemmed |
Abstract The potential vorticity (PV) in the ocean is considered, including the history of the term. Various aspects and basic formulas used to calculate the PV in practice are discussed; the conditions for the fulfillment of its conservation law are considered. Two approaches to the PV are considered: by Ertel and by Rossby. To illustrate the main conclusions, we estimate the PV for the quasi-permanent anticyclonic Lofoten vortex in the Norwegian Sea. We use the data of GLORYS12V1 global oceanic reanalysis for calculations of the PV. The PV by Ertel is ascertained to be a kinematic characteristic. It determines the vortex core, where its typical values are zero, while they can attain %$ - 1.0 \times {{10}^{{ - 10}}}%$ $ m^{–1} %$ s^{–1} $ at the core-periphery, where isopycnic lines thicken. The vertical and horizontal sections of the relative and potential vorticities are constructed. It is found that the horizontal components mainly contribute to the PV, while vertical components are much less significant. In contrast to the PV by Ertel, the PV by Rossby is a dynamic characteristic in the quasi-geostrophic approximation. The main contributor to it is the relative vorticity, which characterizes the rotation of particles. The volumetric PV characterizes the vortex power. The PV maximum is –1.3 × $ 10^{–5} $ $ s^{–1} $ and corresponds to a level of 500 m; the PV does not exceed 1.0 × $ 10^{–5} $ $ s^{–1} $ below 1000 m, and it is ~0.5 × $ 10^{–5} $ $ s^{–1} $ at a level of 3000 m. The volumetric PV for the Lofoten vortex is –9.82 × $ 10^{6} $ $ s^{–1} $. It is –2.28 × $ 10^{8} $ $ s^{–1} $ in the core (up to 1000 m). © Pleiades Publishing, Ltd. 2021. ISSN 0001-4338, Izvestiya, Atmospheric and Oceanic Physics, 2021, Vol. 57, No. 6, pp. 632–641. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Izvestiya Rossiiskoi Akademii Nauk, Fizika Atmosfery i Okeana, 2021, Vol. 57, No. 6, pp. 721–732. |
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Potential Vorticity in the Ocean: Ertel and Rossby Approaches with Estimates for the Lofoten Vortex |
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Novoselova, E. V. Belonenko, T. V. |
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| score |
7.3985195 |