The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean
Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRI...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Izumo, Takeshi [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2005 |
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| Schlagwörter: |
El Niño Southern Oscillation (ENSO) Shallow subtropical/tropical meridional overturning cells (STCs/TCs) |
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| Anmerkung: |
© Springer-Verlag 2005 |
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| Übergeordnetes Werk: |
Enthalten in: Ocean dynamics - Springer-Verlag, 2001, 55(2005), 2 vom: 21. Juli, Seite 110-123 |
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| Übergeordnetes Werk: |
volume:55 ; year:2005 ; number:2 ; day:21 ; month:07 ; pages:110-123 |
| Links: |
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| DOI / URN: |
10.1007/s10236-005-0115-1 |
|---|
| Katalog-ID: |
OLC2070855899 |
|---|
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| 245 | 1 | 0 | |a The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean |
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| 520 | |a Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. | ||
| 650 | 4 | |a Equatorial undercurrent (EUC) | |
| 650 | 4 | |a El Niño Southern Oscillation (ENSO) | |
| 650 | 4 | |a Shallow subtropical/tropical meridional overturning cells (STCs/TCs) | |
| 650 | 4 | |a Equatorial upwelling | |
| 650 | 4 | |a Mass and heat transport | |
| 650 | 4 | |a Heat budget | |
| 650 | 4 | |a Recharge/discharge mechanism | |
| 650 | 4 | |a Interannual and decadal variations of the tropical Pacific | |
| 650 | 4 | |a Climate change | |
| 650 | 4 | |a TAO/TRITON moorings | |
| 650 | 4 | |a Ocean general circulation model (OGCM) | |
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10.1007/s10236-005-0115-1 doi (DE-627)OLC2070855899 (DE-He213)s10236-005-0115-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Izumo, Takeshi verfasserin aut The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. Equatorial undercurrent (EUC) El Niño Southern Oscillation (ENSO) Shallow subtropical/tropical meridional overturning cells (STCs/TCs) Equatorial upwelling Mass and heat transport Heat budget Recharge/discharge mechanism Interannual and decadal variations of the tropical Pacific Climate change TAO/TRITON moorings Ocean general circulation model (OGCM) Enthalten in Ocean dynamics Springer-Verlag, 2001 55(2005), 2 vom: 21. Juli, Seite 110-123 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:55 year:2005 number:2 day:21 month:07 pages:110-123 https://doi.org/10.1007/s10236-005-0115-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_183 GBV_ILN_600 GBV_ILN_602 GBV_ILN_608 GBV_ILN_2018 GBV_ILN_4028 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 55 2005 2 21 07 110-123 |
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10.1007/s10236-005-0115-1 doi (DE-627)OLC2070855899 (DE-He213)s10236-005-0115-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Izumo, Takeshi verfasserin aut The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. Equatorial undercurrent (EUC) El Niño Southern Oscillation (ENSO) Shallow subtropical/tropical meridional overturning cells (STCs/TCs) Equatorial upwelling Mass and heat transport Heat budget Recharge/discharge mechanism Interannual and decadal variations of the tropical Pacific Climate change TAO/TRITON moorings Ocean general circulation model (OGCM) Enthalten in Ocean dynamics Springer-Verlag, 2001 55(2005), 2 vom: 21. Juli, Seite 110-123 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:55 year:2005 number:2 day:21 month:07 pages:110-123 https://doi.org/10.1007/s10236-005-0115-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_183 GBV_ILN_600 GBV_ILN_602 GBV_ILN_608 GBV_ILN_2018 GBV_ILN_4028 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 55 2005 2 21 07 110-123 |
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10.1007/s10236-005-0115-1 doi (DE-627)OLC2070855899 (DE-He213)s10236-005-0115-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Izumo, Takeshi verfasserin aut The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. Equatorial undercurrent (EUC) El Niño Southern Oscillation (ENSO) Shallow subtropical/tropical meridional overturning cells (STCs/TCs) Equatorial upwelling Mass and heat transport Heat budget Recharge/discharge mechanism Interannual and decadal variations of the tropical Pacific Climate change TAO/TRITON moorings Ocean general circulation model (OGCM) Enthalten in Ocean dynamics Springer-Verlag, 2001 55(2005), 2 vom: 21. Juli, Seite 110-123 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:55 year:2005 number:2 day:21 month:07 pages:110-123 https://doi.org/10.1007/s10236-005-0115-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_183 GBV_ILN_600 GBV_ILN_602 GBV_ILN_608 GBV_ILN_2018 GBV_ILN_4028 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 55 2005 2 21 07 110-123 |
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10.1007/s10236-005-0115-1 doi (DE-627)OLC2070855899 (DE-He213)s10236-005-0115-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Izumo, Takeshi verfasserin aut The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. Equatorial undercurrent (EUC) El Niño Southern Oscillation (ENSO) Shallow subtropical/tropical meridional overturning cells (STCs/TCs) Equatorial upwelling Mass and heat transport Heat budget Recharge/discharge mechanism Interannual and decadal variations of the tropical Pacific Climate change TAO/TRITON moorings Ocean general circulation model (OGCM) Enthalten in Ocean dynamics Springer-Verlag, 2001 55(2005), 2 vom: 21. Juli, Seite 110-123 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:55 year:2005 number:2 day:21 month:07 pages:110-123 https://doi.org/10.1007/s10236-005-0115-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_183 GBV_ILN_600 GBV_ILN_602 GBV_ILN_608 GBV_ILN_2018 GBV_ILN_4028 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 55 2005 2 21 07 110-123 |
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10.1007/s10236-005-0115-1 doi (DE-627)OLC2070855899 (DE-He213)s10236-005-0115-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Izumo, Takeshi verfasserin aut The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2005 Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. Equatorial undercurrent (EUC) El Niño Southern Oscillation (ENSO) Shallow subtropical/tropical meridional overturning cells (STCs/TCs) Equatorial upwelling Mass and heat transport Heat budget Recharge/discharge mechanism Interannual and decadal variations of the tropical Pacific Climate change TAO/TRITON moorings Ocean general circulation model (OGCM) Enthalten in Ocean dynamics Springer-Verlag, 2001 55(2005), 2 vom: 21. Juli, Seite 110-123 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:55 year:2005 number:2 day:21 month:07 pages:110-123 https://doi.org/10.1007/s10236-005-0115-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_183 GBV_ILN_600 GBV_ILN_602 GBV_ILN_608 GBV_ILN_2018 GBV_ILN_4028 GBV_ILN_4046 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 55 2005 2 21 07 110-123 |
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Equatorial undercurrent (EUC) El Niño Southern Oscillation (ENSO) Shallow subtropical/tropical meridional overturning cells (STCs/TCs) Equatorial upwelling Mass and heat transport Heat budget Recharge/discharge mechanism Interannual and decadal variations of the tropical Pacific Climate change TAO/TRITON moorings Ocean general circulation model (OGCM) |
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The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean |
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the equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during el niño events in the tropical pacific ocean |
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The equatorial undercurrent, meridional overturning circulation, and their roles in mass and heat exchanges during El Niño events in the tropical Pacific ocean |
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Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. © Springer-Verlag 2005 |
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Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. © Springer-Verlag 2005 |
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Abstract The equatorial undercurrent (EUC), the shallow meridional overturning cells feeding it, and their role in El Niño and decadal variability in the equatorial Pacific are studied using both in situ data and an ocean general circulation model. Using temperature and current data from the TAO/TRITON moorings at the equator, their data gaps are filled and it was shown that continuous time series of mass transport, temperature, depth, and kinetic energy of the EUC could be constructed for the period 1980–2002 with an excellent accuracy. This dataset was analysed and used to validate the output from an oceanic general circulation model (OGCM). The OGCM was then used to find that variations in the strength of the EUC, shallow meridional overturning (pycnocline convergence and surface divergence), and equatorial upwelling had the same variations in mass transport on interannual and longer time scales within the period 1951–1999. These variations are all caused by variations of the zonal wind stress zonally integrated, in agreement with simple linear and steady dynamics theories. Impact of these mass transport variations and of temperature variations on heat budgets in the entire equatorial band of the Pacific and in its eastern part are quantified. © Springer-Verlag 2005 |
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