Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone

Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statist...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Dzyuba, A. V. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2009

Schlagwörter:	North Atlantic Oscillation RUSSIAN Meteorology North Atlantic Oscillation Index North Pacific Oscil Interannual Change

Übergeordnetes Werk:	Enthalten in: Russian meteorology and hydrology - New York, NY : Allerton Press, 2007, 34(2009), 5 vom: Mai, Seite 274-284
Übergeordnetes Werk:	volume:34 ; year:2009 ; number:5 ; month:05 ; pages:274-284

Links:	Volltext

DOI / URN:	10.3103/S1068373909050021

Katalog-ID:	SPR023454725

Internformat


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520			\|a Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region.
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650		4	\|a North Pacific Oscil \|7 (dpeaa)DE-He213
650		4	\|a Interannual Change \|7 (dpeaa)DE-He213
773	0	8	\|i Enthalten in \|t Russian meteorology and hydrology \|d New York, NY : Allerton Press, 2007 \|g 34(2009), 5 vom: Mai, Seite 274-284 \|w (DE-627)531203581 \|w (DE-600)2324879-8 \|x 1934-8096 \|7 nnns
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912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
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912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
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912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
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912			\|a GBV_ILN_602
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912			\|a GBV_ILN_702
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912			\|a GBV_ILN_2005
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912			\|a GBV_ILN_2007
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912			\|a GBV_ILN_2009
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912			\|a GBV_ILN_2015
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912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
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Indexfelder

author_variant	a v d av avd
matchkey_str	article:19348096:2009----::omlztooteeeoncinfhnrhtatcsiltoadeprtrrgmit
hierarchy_sort_str	2009
bklnumber	38.80 38.85
publishDate	2009
allfields	10.3103/S1068373909050021 doi (DE-627)SPR023454725 (SPR)S1068373909050021-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Dzyuba, A. V. verfasserin aut Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region. North Atlantic Oscillation (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 North Atlantic Oscillation Index (dpeaa)DE-He213 North Pacific Oscil (dpeaa)DE-He213 Interannual Change (dpeaa)DE-He213 Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 34(2009), 5 vom: Mai, Seite 274-284 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:34 year:2009 number:5 month:05 pages:274-284 https://dx.doi.org/10.3103/S1068373909050021 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_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 38.80 ASE 38.85 ASE AR 34 2009 5 05 274-284
spelling	10.3103/S1068373909050021 doi (DE-627)SPR023454725 (SPR)S1068373909050021-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Dzyuba, A. V. verfasserin aut Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region. North Atlantic Oscillation (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 North Atlantic Oscillation Index (dpeaa)DE-He213 North Pacific Oscil (dpeaa)DE-He213 Interannual Change (dpeaa)DE-He213 Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 34(2009), 5 vom: Mai, Seite 274-284 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:34 year:2009 number:5 month:05 pages:274-284 https://dx.doi.org/10.3103/S1068373909050021 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_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 38.80 ASE 38.85 ASE AR 34 2009 5 05 274-284
allfields_unstemmed	10.3103/S1068373909050021 doi (DE-627)SPR023454725 (SPR)S1068373909050021-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Dzyuba, A. V. verfasserin aut Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region. North Atlantic Oscillation (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 North Atlantic Oscillation Index (dpeaa)DE-He213 North Pacific Oscil (dpeaa)DE-He213 Interannual Change (dpeaa)DE-He213 Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 34(2009), 5 vom: Mai, Seite 274-284 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:34 year:2009 number:5 month:05 pages:274-284 https://dx.doi.org/10.3103/S1068373909050021 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_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 38.80 ASE 38.85 ASE AR 34 2009 5 05 274-284
allfieldsGer	10.3103/S1068373909050021 doi (DE-627)SPR023454725 (SPR)S1068373909050021-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Dzyuba, A. V. verfasserin aut Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region. North Atlantic Oscillation (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 North Atlantic Oscillation Index (dpeaa)DE-He213 North Pacific Oscil (dpeaa)DE-He213 Interannual Change (dpeaa)DE-He213 Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 34(2009), 5 vom: Mai, Seite 274-284 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:34 year:2009 number:5 month:05 pages:274-284 https://dx.doi.org/10.3103/S1068373909050021 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_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 38.80 ASE 38.85 ASE AR 34 2009 5 05 274-284
allfieldsSound	10.3103/S1068373909050021 doi (DE-627)SPR023454725 (SPR)S1068373909050021-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Dzyuba, A. V. verfasserin aut Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region. North Atlantic Oscillation (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 North Atlantic Oscillation Index (dpeaa)DE-He213 North Pacific Oscil (dpeaa)DE-He213 Interannual Change (dpeaa)DE-He213 Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 34(2009), 5 vom: Mai, Seite 274-284 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:34 year:2009 number:5 month:05 pages:274-284 https://dx.doi.org/10.3103/S1068373909050021 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_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 38.80 ASE 38.85 ASE AR 34 2009 5 05 274-284
language	English
source	Enthalten in Russian meteorology and hydrology 34(2009), 5 vom: Mai, Seite 274-284 volume:34 year:2009 number:5 month:05 pages:274-284
sourceStr	Enthalten in Russian meteorology and hydrology 34(2009), 5 vom: Mai, Seite 274-284 volume:34 year:2009 number:5 month:05 pages:274-284
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	North Atlantic Oscillation RUSSIAN Meteorology North Atlantic Oscillation Index North Pacific Oscil Interannual Change
dewey-raw	550
isfreeaccess_bool	false
container_title	Russian meteorology and hydrology
authorswithroles_txt_mv	Dzyuba, A. V. @@aut@@
publishDateDaySort_date	2009-05-01T00:00:00Z
hierarchy_top_id	531203581
dewey-sort	3550
id	SPR023454725
language_de	englisch
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author	Dzyuba, A. V.
spellingShingle	Dzyuba, A. V. ddc 550 bkl 38.80 bkl 38.85 misc North Atlantic Oscillation misc RUSSIAN Meteorology misc North Atlantic Oscillation Index misc North Pacific Oscil misc Interannual Change Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone
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topic_title	550 ASE 38.80 bkl 38.85 bkl Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone North Atlantic Oscillation (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 North Atlantic Oscillation Index (dpeaa)DE-He213 North Pacific Oscil (dpeaa)DE-He213 Interannual Change (dpeaa)DE-He213
topic	ddc 550 bkl 38.80 bkl 38.85 misc North Atlantic Oscillation misc RUSSIAN Meteorology misc North Atlantic Oscillation Index misc North Pacific Oscil misc Interannual Change
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title	Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone
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title_full	Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone
author_sort	Dzyuba, A. V.
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title_sort	formalization of the teleconnection of the north atlantic oscillation and temperature regime in the atlantic-eurasian subpolar zone
title_auth	Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone
abstract	Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region.
abstractGer	Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region.
abstract_unstemmed	Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. A statistical formalization is carried out, and a possible mechanism is described of teleconnection between low-frequency oscillations of the pressure field in the North Atlantic and climatic parameters in the northwestern part of the Atlantic-Eurasian region.
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title_short	Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone
url	https://dx.doi.org/10.3103/S1068373909050021
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up_date	2024-07-03T19:02:11.239Z
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fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR023454725</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220111102524.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201006s2009 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3103/S1068373909050021</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR023454725</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)S1068373909050021-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.80</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.85</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Dzyuba, A. V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2009</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="520" ind1=" " ind2=" "><subfield code="a">Abstract Statistical analysis is performed of long-term changes in surface air temperature in the western part of the subpolar zone, in the greenhouse gas content of the atmosphere, and in atmospheric pressure oscillations in the North Atlantic atmospheric centers of action. Stability of the statistics for the next decades is considered with allowance for a possible increase in the greenhouse gas concentration in the atmosphere of the north polar zone. 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Formalization of the teleconnection of the North Atlantic oscillation and temperature regime in the Atlantic-Eurasian subpolar zone

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