The Lofoten Vortex of the Nordic Seas
The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influ...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Raj, Roshin P. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015transfer abstract |
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| Umfang: |
14 |
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| Übergeordnetes Werk: |
Enthalten in: Seasonal factitious increase in serum potassium: Still a problem and should be recognised - Davis, Kayleigh R. ELSEVIER, 2014, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:96 ; year:2015 ; pages:1-14 ; extent:14 |
| Links: |
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| DOI / URN: |
10.1016/j.dsr.2014.10.011 |
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| 245 | 1 | 4 | |a The Lofoten Vortex of the Nordic Seas |
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| 520 | |a The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. | ||
| 520 | |a The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. | ||
| 650 | 7 | |a Norwegian Atlantic Current |2 Elsevier | |
| 650 | 7 | |a Eddy kinetic energy |2 Elsevier | |
| 650 | 7 | |a Lofoten Vortex |2 Elsevier | |
| 650 | 7 | |a Heat loss |2 Elsevier | |
| 650 | 7 | |a Convection |2 Elsevier | |
| 650 | 7 | |a Lofoten Basin |2 Elsevier | |
| 700 | 1 | |a Chafik, Léon |4 oth | |
| 700 | 1 | |a Nilsen, J. Even Ø. |4 oth | |
| 700 | 1 | |a Eldevik, Tor |4 oth | |
| 700 | 1 | |a Halo, Issufo |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Davis, Kayleigh R. ELSEVIER |t Seasonal factitious increase in serum potassium: Still a problem and should be recognised |d 2014 |g Amsterdam [u.a.] |w (DE-627)ELV023027428 |
| 773 | 1 | 8 | |g volume:96 |g year:2015 |g pages:1-14 |g extent:14 |
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10.1016/j.dsr.2014.10.011 doi GBVA2015017000022.pica (DE-627)ELV039875806 (ELSEVIER)S0967-0637(14)00194-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 540 VZ 35.40 bkl Raj, Roshin P. verfasserin aut The Lofoten Vortex of the Nordic Seas 2015transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. Norwegian Atlantic Current Elsevier Eddy kinetic energy Elsevier Lofoten Vortex Elsevier Heat loss Elsevier Convection Elsevier Lofoten Basin Elsevier Chafik, Léon oth Nilsen, J. Even Ø. oth Eldevik, Tor oth Halo, Issufo oth Enthalten in Elsevier Science Davis, Kayleigh R. ELSEVIER Seasonal factitious increase in serum potassium: Still a problem and should be recognised 2014 Amsterdam [u.a.] (DE-627)ELV023027428 volume:96 year:2015 pages:1-14 extent:14 https://doi.org/10.1016/j.dsr.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.40 Anorganische Chemie: Allgemeines VZ AR 96 2015 1-14 14 045F 550 |
| spelling |
10.1016/j.dsr.2014.10.011 doi GBVA2015017000022.pica (DE-627)ELV039875806 (ELSEVIER)S0967-0637(14)00194-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 540 VZ 35.40 bkl Raj, Roshin P. verfasserin aut The Lofoten Vortex of the Nordic Seas 2015transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. Norwegian Atlantic Current Elsevier Eddy kinetic energy Elsevier Lofoten Vortex Elsevier Heat loss Elsevier Convection Elsevier Lofoten Basin Elsevier Chafik, Léon oth Nilsen, J. Even Ø. oth Eldevik, Tor oth Halo, Issufo oth Enthalten in Elsevier Science Davis, Kayleigh R. ELSEVIER Seasonal factitious increase in serum potassium: Still a problem and should be recognised 2014 Amsterdam [u.a.] (DE-627)ELV023027428 volume:96 year:2015 pages:1-14 extent:14 https://doi.org/10.1016/j.dsr.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.40 Anorganische Chemie: Allgemeines VZ AR 96 2015 1-14 14 045F 550 |
| allfields_unstemmed |
10.1016/j.dsr.2014.10.011 doi GBVA2015017000022.pica (DE-627)ELV039875806 (ELSEVIER)S0967-0637(14)00194-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 540 VZ 35.40 bkl Raj, Roshin P. verfasserin aut The Lofoten Vortex of the Nordic Seas 2015transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. Norwegian Atlantic Current Elsevier Eddy kinetic energy Elsevier Lofoten Vortex Elsevier Heat loss Elsevier Convection Elsevier Lofoten Basin Elsevier Chafik, Léon oth Nilsen, J. Even Ø. oth Eldevik, Tor oth Halo, Issufo oth Enthalten in Elsevier Science Davis, Kayleigh R. ELSEVIER Seasonal factitious increase in serum potassium: Still a problem and should be recognised 2014 Amsterdam [u.a.] (DE-627)ELV023027428 volume:96 year:2015 pages:1-14 extent:14 https://doi.org/10.1016/j.dsr.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.40 Anorganische Chemie: Allgemeines VZ AR 96 2015 1-14 14 045F 550 |
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10.1016/j.dsr.2014.10.011 doi GBVA2015017000022.pica (DE-627)ELV039875806 (ELSEVIER)S0967-0637(14)00194-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 540 VZ 35.40 bkl Raj, Roshin P. verfasserin aut The Lofoten Vortex of the Nordic Seas 2015transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. Norwegian Atlantic Current Elsevier Eddy kinetic energy Elsevier Lofoten Vortex Elsevier Heat loss Elsevier Convection Elsevier Lofoten Basin Elsevier Chafik, Léon oth Nilsen, J. Even Ø. oth Eldevik, Tor oth Halo, Issufo oth Enthalten in Elsevier Science Davis, Kayleigh R. ELSEVIER Seasonal factitious increase in serum potassium: Still a problem and should be recognised 2014 Amsterdam [u.a.] (DE-627)ELV023027428 volume:96 year:2015 pages:1-14 extent:14 https://doi.org/10.1016/j.dsr.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.40 Anorganische Chemie: Allgemeines VZ AR 96 2015 1-14 14 045F 550 |
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10.1016/j.dsr.2014.10.011 doi GBVA2015017000022.pica (DE-627)ELV039875806 (ELSEVIER)S0967-0637(14)00194-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 540 VZ 35.40 bkl Raj, Roshin P. verfasserin aut The Lofoten Vortex of the Nordic Seas 2015transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. Norwegian Atlantic Current Elsevier Eddy kinetic energy Elsevier Lofoten Vortex Elsevier Heat loss Elsevier Convection Elsevier Lofoten Basin Elsevier Chafik, Léon oth Nilsen, J. Even Ø. oth Eldevik, Tor oth Halo, Issufo oth Enthalten in Elsevier Science Davis, Kayleigh R. ELSEVIER Seasonal factitious increase in serum potassium: Still a problem and should be recognised 2014 Amsterdam [u.a.] (DE-627)ELV023027428 volume:96 year:2015 pages:1-14 extent:14 https://doi.org/10.1016/j.dsr.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.40 Anorganische Chemie: Allgemeines VZ AR 96 2015 1-14 14 045F 550 |
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Enthalten in Seasonal factitious increase in serum potassium: Still a problem and should be recognised Amsterdam [u.a.] volume:96 year:2015 pages:1-14 extent:14 |
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Seasonal factitious increase in serum potassium: Still a problem and should be recognised |
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Raj, Roshin P. @@aut@@ Chafik, Léon @@oth@@ Nilsen, J. Even Ø. @@oth@@ Eldevik, Tor @@oth@@ Halo, Issufo @@oth@@ |
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Seasonal factitious increase in serum potassium: Still a problem and should be recognised |
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The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. |
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The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. |
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The Lofoten Basin is the largest reservoir of ocean heat in the Nordic Seas. A particular feature of the basin is ‘the Lofoten Vortex’, a most anomalous mesoscale structure in the Nordic Seas. The vortex resides in one of the major winter convection sites in the Norwegian Sea, and is likely to influence the dense water formation of the region. Here, we document this quasi-permanent anticyclonic vortex using hydrographic and satellite observations. The vortex’ uniqueness in the Nordic Seas, its surface characteristics on seasonal, inter-annual, and climatological time-scales, are examined together with the main forcing mechanisms acting on it. The influence of the vortex on the hydrography of the Lofoten Basin is also shown. We show that the Atlantic Water in the Nordic Seas penetrate the deepest inside the Lofoten Vortex, and confirm the persistent existence of the vortex in the deepest part of the Lofoten Basin, its dominant cyclonic drift and reveal seasonality in its eddy intensity with maximum during late winter and minimum during late autumn. Eddy merging processes are studied in detail, and mergers by eddies from the slope current are found to provide anticyclonic vorticity to the Lofoten Vortex. |
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