Variability of Atlantic Ocean heat transport and its effects on the atmosphere
The variability of the Atlantic meridional Ocean Heat Transport (OHT) has been diagnosed from a simulation of a coupled ocean-atmosphere general circulation model, and the mechanisms responsible for this variability have been elucidated. It has been demonstrated that the interannual variability in A...
Ausführliche Beschreibung
Autor*in: |
R. T. Sutton [verfasserIn] B. Dong [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
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2003 |
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Übergeordnetes Werk: |
In: Annals of Geophysics - Istituto Nazionale di Geofisica e Vulcanologia (INGV), 2010, 46(2003), 1 |
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Übergeordnetes Werk: |
volume:46 ; year:2003 ; number:1 |
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Link aufrufen |
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DOI / URN: |
10.4401/ag-3391 |
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Katalog-ID: |
DOAJ033447519 |
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520 | |a The variability of the Atlantic meridional Ocean Heat Transport (OHT) has been diagnosed from a simulation of a coupled ocean-atmosphere general circulation model, and the mechanisms responsible for this variability have been elucidated. It has been demonstrated that the interannual variability in Atlantic OHT is dominated by windstress-driven Ekman fluctuations. In contrast, the decadal and multidecadal variability is associated with the fluctuations of the Thermohaline Circulation (THC), driven by the fluctuations in deep convection over the Greenland-Iceland-Norwegian (GIN) Sea. The fluctuations of OHT induce Ocean Heat Content (OHC), and Sea Surface Temperature (SST) anomalies over the tropical and subtropical North Atlantic. The SST anomalies, in turn, have an impact on the atmosphere. The lead-lag relationships between the fluctuations of THC-related OHT and those of OHC and SST raise the possibility that a knowledge of OHT fluctuations could be used to predict variations in Atlantic Sea surface temperatures, and perhaps aspects of climate, several years in advance. A comparison of results from a second, independent, coupled model simulation is also presented, and similar conclusions reached. | ||
650 | 4 | |a climate variability | |
650 | 4 | |a North Atlantic Oscillation (NAO) | |
650 | 4 | |a Ocean Heat Transport (OHT) | |
650 | 4 | |a Sea Surface Temperature (SST) | |
650 | 4 | |a ThermohalineCirculation (THC) | |
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10.4401/ag-3391 doi (DE-627)DOAJ033447519 (DE-599)DOAJa98d1eecb49b4238b2bdddaafe433943 DE-627 ger DE-627 rakwb eng QC851-999 QC801-809 R. T. Sutton verfasserin aut Variability of Atlantic Ocean heat transport and its effects on the atmosphere 2003 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The variability of the Atlantic meridional Ocean Heat Transport (OHT) has been diagnosed from a simulation of a coupled ocean-atmosphere general circulation model, and the mechanisms responsible for this variability have been elucidated. It has been demonstrated that the interannual variability in Atlantic OHT is dominated by windstress-driven Ekman fluctuations. In contrast, the decadal and multidecadal variability is associated with the fluctuations of the Thermohaline Circulation (THC), driven by the fluctuations in deep convection over the Greenland-Iceland-Norwegian (GIN) Sea. The fluctuations of OHT induce Ocean Heat Content (OHC), and Sea Surface Temperature (SST) anomalies over the tropical and subtropical North Atlantic. The SST anomalies, in turn, have an impact on the atmosphere. The lead-lag relationships between the fluctuations of THC-related OHT and those of OHC and SST raise the possibility that a knowledge of OHT fluctuations could be used to predict variations in Atlantic Sea surface temperatures, and perhaps aspects of climate, several years in advance. A comparison of results from a second, independent, coupled model simulation is also presented, and similar conclusions reached. climate variability North Atlantic Oscillation (NAO) Ocean Heat Transport (OHT) Sea Surface Temperature (SST) ThermohalineCirculation (THC) Meteorology. Climatology Geophysics. Cosmic physics B. Dong verfasserin aut In Annals of Geophysics Istituto Nazionale di Geofisica e Vulcanologia (INGV), 2010 46(2003), 1 (DE-627)559075804 (DE-600)2410939-3 2037416X nnns volume:46 year:2003 number:1 https://doi.org/10.4401/ag-3391 kostenfrei https://doaj.org/article/a98d1eecb49b4238b2bdddaafe433943 kostenfrei http://www.annalsofgeophysics.eu/index.php/annals/article/view/3391 kostenfrei https://doaj.org/toc/1593-5213 Journal toc kostenfrei https://doaj.org/toc/2037-416X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 46 2003 1 |
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QC851-999 QC801-809 Variability of Atlantic Ocean heat transport and its effects on the atmosphere climate variability North Atlantic Oscillation (NAO) Ocean Heat Transport (OHT) Sea Surface Temperature (SST) ThermohalineCirculation (THC) |
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misc QC851-999 misc QC801-809 misc climate variability misc North Atlantic Oscillation (NAO) misc Ocean Heat Transport (OHT) misc Sea Surface Temperature (SST) misc ThermohalineCirculation (THC) misc Meteorology. Climatology misc Geophysics. Cosmic physics |
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Variability of Atlantic Ocean heat transport and its effects on the atmosphere |
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The variability of the Atlantic meridional Ocean Heat Transport (OHT) has been diagnosed from a simulation of a coupled ocean-atmosphere general circulation model, and the mechanisms responsible for this variability have been elucidated. It has been demonstrated that the interannual variability in Atlantic OHT is dominated by windstress-driven Ekman fluctuations. In contrast, the decadal and multidecadal variability is associated with the fluctuations of the Thermohaline Circulation (THC), driven by the fluctuations in deep convection over the Greenland-Iceland-Norwegian (GIN) Sea. The fluctuations of OHT induce Ocean Heat Content (OHC), and Sea Surface Temperature (SST) anomalies over the tropical and subtropical North Atlantic. The SST anomalies, in turn, have an impact on the atmosphere. The lead-lag relationships between the fluctuations of THC-related OHT and those of OHC and SST raise the possibility that a knowledge of OHT fluctuations could be used to predict variations in Atlantic Sea surface temperatures, and perhaps aspects of climate, several years in advance. A comparison of results from a second, independent, coupled model simulation is also presented, and similar conclusions reached. |
abstractGer |
The variability of the Atlantic meridional Ocean Heat Transport (OHT) has been diagnosed from a simulation of a coupled ocean-atmosphere general circulation model, and the mechanisms responsible for this variability have been elucidated. It has been demonstrated that the interannual variability in Atlantic OHT is dominated by windstress-driven Ekman fluctuations. In contrast, the decadal and multidecadal variability is associated with the fluctuations of the Thermohaline Circulation (THC), driven by the fluctuations in deep convection over the Greenland-Iceland-Norwegian (GIN) Sea. The fluctuations of OHT induce Ocean Heat Content (OHC), and Sea Surface Temperature (SST) anomalies over the tropical and subtropical North Atlantic. The SST anomalies, in turn, have an impact on the atmosphere. The lead-lag relationships between the fluctuations of THC-related OHT and those of OHC and SST raise the possibility that a knowledge of OHT fluctuations could be used to predict variations in Atlantic Sea surface temperatures, and perhaps aspects of climate, several years in advance. A comparison of results from a second, independent, coupled model simulation is also presented, and similar conclusions reached. |
abstract_unstemmed |
The variability of the Atlantic meridional Ocean Heat Transport (OHT) has been diagnosed from a simulation of a coupled ocean-atmosphere general circulation model, and the mechanisms responsible for this variability have been elucidated. It has been demonstrated that the interannual variability in Atlantic OHT is dominated by windstress-driven Ekman fluctuations. In contrast, the decadal and multidecadal variability is associated with the fluctuations of the Thermohaline Circulation (THC), driven by the fluctuations in deep convection over the Greenland-Iceland-Norwegian (GIN) Sea. The fluctuations of OHT induce Ocean Heat Content (OHC), and Sea Surface Temperature (SST) anomalies over the tropical and subtropical North Atlantic. The SST anomalies, in turn, have an impact on the atmosphere. The lead-lag relationships between the fluctuations of THC-related OHT and those of OHC and SST raise the possibility that a knowledge of OHT fluctuations could be used to predict variations in Atlantic Sea surface temperatures, and perhaps aspects of climate, several years in advance. A comparison of results from a second, independent, coupled model simulation is also presented, and similar conclusions reached. |
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Variability of Atlantic Ocean heat transport and its effects on the atmosphere |
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