Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations

Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index,...
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Autor*in:	Semenov, V. A. [verfasserIn] Shelekhova, E. A. Mokhov, I. I. Zuev, V. V. Koltermann, K. P.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	Heat Flux Atmospheric General Circulation Model Turbulent Heat Flux Mixed Ocean Layer Oceanic Heat Transport

Anmerkung:	© Pleiades Publishing, Ltd. 2014

Übergeordnetes Werk:	Enthalten in: Atmospheric and oceanic optics - Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009, 27(2014), 3 vom: Mai, Seite 253-261
Übergeordnetes Werk:	volume:27 ; year:2014 ; number:3 ; month:05 ; pages:253-261

Links:	Volltext

DOI / URN:	10.1134/S1024856014030087

Katalog-ID:	SPR026320479

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520			\|a Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies.
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allfields	10.1134/S1024856014030087 doi (DE-627)SPR026320479 (SPR)S1024856014030087-e DE-627 ger DE-627 rakwb eng Semenov, V. A. verfasserin aut Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. Heat Flux (dpeaa)DE-He213 Atmospheric General Circulation Model (dpeaa)DE-He213 Turbulent Heat Flux (dpeaa)DE-He213 Mixed Ocean Layer (dpeaa)DE-He213 Oceanic Heat Transport (dpeaa)DE-He213 Shelekhova, E. A. aut Mokhov, I. I. aut Zuev, V. V. aut Koltermann, K. P. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 27(2014), 3 vom: Mai, Seite 253-261 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:27 year:2014 number:3 month:05 pages:253-261 https://dx.doi.org/10.1134/S1024856014030087 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_101 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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2014 3 05 253-261
spelling	10.1134/S1024856014030087 doi (DE-627)SPR026320479 (SPR)S1024856014030087-e DE-627 ger DE-627 rakwb eng Semenov, V. A. verfasserin aut Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. Heat Flux (dpeaa)DE-He213 Atmospheric General Circulation Model (dpeaa)DE-He213 Turbulent Heat Flux (dpeaa)DE-He213 Mixed Ocean Layer (dpeaa)DE-He213 Oceanic Heat Transport (dpeaa)DE-He213 Shelekhova, E. A. aut Mokhov, I. I. aut Zuev, V. V. aut Koltermann, K. P. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 27(2014), 3 vom: Mai, Seite 253-261 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:27 year:2014 number:3 month:05 pages:253-261 https://dx.doi.org/10.1134/S1024856014030087 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_101 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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2014 3 05 253-261
allfields_unstemmed	10.1134/S1024856014030087 doi (DE-627)SPR026320479 (SPR)S1024856014030087-e DE-627 ger DE-627 rakwb eng Semenov, V. A. verfasserin aut Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. Heat Flux (dpeaa)DE-He213 Atmospheric General Circulation Model (dpeaa)DE-He213 Turbulent Heat Flux (dpeaa)DE-He213 Mixed Ocean Layer (dpeaa)DE-He213 Oceanic Heat Transport (dpeaa)DE-He213 Shelekhova, E. A. aut Mokhov, I. I. aut Zuev, V. V. aut Koltermann, K. P. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 27(2014), 3 vom: Mai, Seite 253-261 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:27 year:2014 number:3 month:05 pages:253-261 https://dx.doi.org/10.1134/S1024856014030087 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_101 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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2014 3 05 253-261
allfieldsGer	10.1134/S1024856014030087 doi (DE-627)SPR026320479 (SPR)S1024856014030087-e DE-627 ger DE-627 rakwb eng Semenov, V. A. verfasserin aut Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. Heat Flux (dpeaa)DE-He213 Atmospheric General Circulation Model (dpeaa)DE-He213 Turbulent Heat Flux (dpeaa)DE-He213 Mixed Ocean Layer (dpeaa)DE-He213 Oceanic Heat Transport (dpeaa)DE-He213 Shelekhova, E. A. aut Mokhov, I. I. aut Zuev, V. V. aut Koltermann, K. P. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 27(2014), 3 vom: Mai, Seite 253-261 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:27 year:2014 number:3 month:05 pages:253-261 https://dx.doi.org/10.1134/S1024856014030087 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_101 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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2014 3 05 253-261
allfieldsSound	10.1134/S1024856014030087 doi (DE-627)SPR026320479 (SPR)S1024856014030087-e DE-627 ger DE-627 rakwb eng Semenov, V. A. verfasserin aut Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2014 Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. Heat Flux (dpeaa)DE-He213 Atmospheric General Circulation Model (dpeaa)DE-He213 Turbulent Heat Flux (dpeaa)DE-He213 Mixed Ocean Layer (dpeaa)DE-He213 Oceanic Heat Transport (dpeaa)DE-He213 Shelekhova, E. A. aut Mokhov, I. I. aut Zuev, V. V. aut Koltermann, K. P. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 27(2014), 3 vom: Mai, Seite 253-261 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:27 year:2014 number:3 month:05 pages:253-261 https://dx.doi.org/10.1134/S1024856014030087 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_101 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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2014 3 05 253-261
language	English
source	Enthalten in Atmospheric and oceanic optics 27(2014), 3 vom: Mai, Seite 253-261 volume:27 year:2014 number:3 month:05 pages:253-261
sourceStr	Enthalten in Atmospheric and oceanic optics 27(2014), 3 vom: Mai, Seite 253-261 volume:27 year:2014 number:3 month:05 pages:253-261
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Heat Flux Atmospheric General Circulation Model Turbulent Heat Flux Mixed Ocean Layer Oceanic Heat Transport
isfreeaccess_bool	false
container_title	Atmospheric and oceanic optics
authorswithroles_txt_mv	Semenov, V. A. @@aut@@ Shelekhova, E. A. @@aut@@ Mokhov, I. I. @@aut@@ Zuev, V. V. @@aut@@ Koltermann, K. P. @@aut@@
publishDateDaySort_date	2014-05-01T00:00:00Z
hierarchy_top_id	599674695
id	SPR026320479
language_de	englisch
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author	Semenov, V. A.
spellingShingle	Semenov, V. A. misc Heat Flux misc Atmospheric General Circulation Model misc Turbulent Heat Flux misc Mixed Ocean Layer misc Oceanic Heat Transport Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations
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topic_title	Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations Heat Flux (dpeaa)DE-He213 Atmospheric General Circulation Model (dpeaa)DE-He213 Turbulent Heat Flux (dpeaa)DE-He213 Mixed Ocean Layer (dpeaa)DE-He213 Oceanic Heat Transport (dpeaa)DE-He213
topic	misc Heat Flux misc Atmospheric General Circulation Model misc Turbulent Heat Flux misc Mixed Ocean Layer misc Oceanic Heat Transport
topic_unstemmed	misc Heat Flux misc Atmospheric General Circulation Model misc Turbulent Heat Flux misc Mixed Ocean Layer misc Oceanic Heat Transport
topic_browse	misc Heat Flux misc Atmospheric General Circulation Model misc Turbulent Heat Flux misc Mixed Ocean Layer misc Oceanic Heat Transport
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title	Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations
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title_full	Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations
author_sort	Semenov, V. A.
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author_browse	Semenov, V. A. Shelekhova, E. A. Mokhov, I. I. Zuev, V. V. Koltermann, K. P.
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author-letter	Semenov, V. A.
doi_str_mv	10.1134/S1024856014030087
title_sort	role of the atlantic multidecadal oscillation in formation of seasonal air temperature anomalies in the northern hemisphere according to model calculations
title_auth	Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations
abstract	Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. © Pleiades Publishing, Ltd. 2014
abstractGer	Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. © Pleiades Publishing, Ltd. 2014
abstract_unstemmed	Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. The results obtained indicate an important role of AMO in the formation of weather and climate anomalies. © Pleiades Publishing, Ltd. 2014
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title_short	Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations
url	https://dx.doi.org/10.1134/S1024856014030087
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author2	Shelekhova, E. A. Mokhov, I. I. Zuev, V. V. Koltermann, K. P.
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up_date	2024-07-03T20:14:11.628Z
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A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2014</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. 2014</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Atlantic Multidecadal Oscillation (AMO), associated with variations in oceanic heat transport in the North Atlantic and the Atlantic sector of the Arctic, influences appreciably the climate of the Northern Hemisphere (NH). From the 1970s to early 2000s, there was a growth in the AMO index, coinciding with the trend of global warming. To estimate the AMO contribution to the NH seasonal temperature changes, we analyzed the numerical experiments with the atmospheric general circulation model (ECHAM5) coupled to the thermodynamic model of the upper mixed ocean layer using anomalous ocean heat convergence fluxes associated with the AMO. As part of the research, we studied the relative contribution of anomalous heat fluxes in the Atlantic and the Arctic. It is shown that AMO can explain about 40% of the observed winter and summer temperature changes over the last three decades. The vertical structure of the AMO-related temperature changes has also much in common with empirical estimates. In particular, the model reproduces the Arctic amplification with maximum temperature trends near the surface at high NH latitudes. AMO in the model leads to more probable anomalously cold temperature regimes in February on the territory of Russia, despite the rise of the mean February temperature. Also, we indicated more a probable development of anomalously hot Julys, particularly in European Russia. It is shown that an important contribution to the seasonal variations comes from anomalous heat fluxes in the Arctic, which are generally disregarded when the effect of North Atlantic Multidecadal Oscillation in the Northern Atlantic is modeled. 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A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mokhov, I. I.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zuev, V. V.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Koltermann, K. 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Role of the Atlantic Multidecadal Oscillation in formation of seasonal air temperature anomalies in the Northern Hemisphere according to model calculations

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