Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011
Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood d...
Ausführliche Beschreibung
Autor*in: |
Semenov, E. K. [verfasserIn] Platonov, V. S. [verfasserIn] Sokolikhina, E. V. [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2012 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Russian meteorology and hydrology - New York, NY : Allerton Press, 2007, 37(2012), 2 vom: Feb., Seite 90-97 |
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Übergeordnetes Werk: |
volume:37 ; year:2012 ; number:2 ; month:02 ; pages:90-97 |
Links: |
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DOI / URN: |
10.3103/S1068373912020033 |
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Katalog-ID: |
SPR023458054 |
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520 | |a Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. | ||
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650 | 4 | |a Pacific Ocean |7 (dpeaa)DE-He213 | |
650 | 4 | |a Tropical Cyclone |7 (dpeaa)DE-He213 | |
650 | 4 | |a RUSSIAN Meteorology |7 (dpeaa)DE-He213 | |
650 | 4 | |a Tropical Atmosphere |7 (dpeaa)DE-He213 | |
700 | 1 | |a Platonov, V. S. |e verfasserin |4 aut | |
700 | 1 | |a Sokolikhina, E. V. |e verfasserin |4 aut | |
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2012 |
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10.3103/S1068373912020033 doi (DE-627)SPR023458054 (SPR)S1068373912020033-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Semenov, E. K. verfasserin aut Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. Indian Ocean (dpeaa)DE-He213 Pacific Ocean (dpeaa)DE-He213 Tropical Cyclone (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Tropical Atmosphere (dpeaa)DE-He213 Platonov, V. S. verfasserin aut Sokolikhina, E. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 2 vom: Feb., Seite 90-97 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:2 month:02 pages:90-97 https://dx.doi.org/10.3103/S1068373912020033 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 37 2012 2 02 90-97 |
spelling |
10.3103/S1068373912020033 doi (DE-627)SPR023458054 (SPR)S1068373912020033-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Semenov, E. K. verfasserin aut Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. Indian Ocean (dpeaa)DE-He213 Pacific Ocean (dpeaa)DE-He213 Tropical Cyclone (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Tropical Atmosphere (dpeaa)DE-He213 Platonov, V. S. verfasserin aut Sokolikhina, E. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 2 vom: Feb., Seite 90-97 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:2 month:02 pages:90-97 https://dx.doi.org/10.3103/S1068373912020033 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 37 2012 2 02 90-97 |
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10.3103/S1068373912020033 doi (DE-627)SPR023458054 (SPR)S1068373912020033-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Semenov, E. K. verfasserin aut Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. Indian Ocean (dpeaa)DE-He213 Pacific Ocean (dpeaa)DE-He213 Tropical Cyclone (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Tropical Atmosphere (dpeaa)DE-He213 Platonov, V. S. verfasserin aut Sokolikhina, E. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 2 vom: Feb., Seite 90-97 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:2 month:02 pages:90-97 https://dx.doi.org/10.3103/S1068373912020033 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 37 2012 2 02 90-97 |
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10.3103/S1068373912020033 doi (DE-627)SPR023458054 (SPR)S1068373912020033-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Semenov, E. K. verfasserin aut Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. Indian Ocean (dpeaa)DE-He213 Pacific Ocean (dpeaa)DE-He213 Tropical Cyclone (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Tropical Atmosphere (dpeaa)DE-He213 Platonov, V. S. verfasserin aut Sokolikhina, E. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 2 vom: Feb., Seite 90-97 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:2 month:02 pages:90-97 https://dx.doi.org/10.3103/S1068373912020033 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 37 2012 2 02 90-97 |
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10.3103/S1068373912020033 doi (DE-627)SPR023458054 (SPR)S1068373912020033-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Semenov, E. K. verfasserin aut Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. Indian Ocean (dpeaa)DE-He213 Pacific Ocean (dpeaa)DE-He213 Tropical Cyclone (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Tropical Atmosphere (dpeaa)DE-He213 Platonov, V. S. verfasserin aut Sokolikhina, E. V. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 37(2012), 2 vom: Feb., Seite 90-97 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:37 year:2012 number:2 month:02 pages:90-97 https://dx.doi.org/10.3103/S1068373912020033 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 37 2012 2 02 90-97 |
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Enthalten in Russian meteorology and hydrology 37(2012), 2 vom: Feb., Seite 90-97 volume:37 year:2012 number:2 month:02 pages:90-97 |
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Enthalten in Russian meteorology and hydrology 37(2012), 2 vom: Feb., Seite 90-97 volume:37 year:2012 number:2 month:02 pages:90-97 |
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Russian meteorology and hydrology |
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Semenov, E. K. @@aut@@ Platonov, V. S. @@aut@@ Sokolikhina, E. V. @@aut@@ |
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author |
Semenov, E. K. |
spellingShingle |
Semenov, E. K. ddc 550 bkl 38.80 bkl 38.85 misc Indian Ocean misc Pacific Ocean misc Tropical Cyclone misc RUSSIAN Meteorology misc Tropical Atmosphere Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 |
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550 ASE 38.80 bkl 38.85 bkl Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 Indian Ocean (dpeaa)DE-He213 Pacific Ocean (dpeaa)DE-He213 Tropical Cyclone (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Tropical Atmosphere (dpeaa)DE-He213 |
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ddc 550 bkl 38.80 bkl 38.85 misc Indian Ocean misc Pacific Ocean misc Tropical Cyclone misc RUSSIAN Meteorology misc Tropical Atmosphere |
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ddc 550 bkl 38.80 bkl 38.85 misc Indian Ocean misc Pacific Ocean misc Tropical Cyclone misc RUSSIAN Meteorology misc Tropical Atmosphere |
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Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 |
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Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 |
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Semenov, E. K. |
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Russian meteorology and hydrology |
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Semenov, E. K. Platonov, V. S. Sokolikhina, E. V. |
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Semenov, E. K. |
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synoptic aspects of the catastrophic flood formation in the northeast of australia during extreme la niña 2010–2011 |
title_auth |
Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 |
abstract |
Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. |
abstractGer |
Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. |
abstract_unstemmed |
Abstract A synoptic mechanism of the formation of atmospheric circulation anomalies over the tropics of the Indian and Pacific oceans observed during the La Niña 2010–2011 culmination is considered using the daily data of the NCEP/NCAR reanalysis. It was established that the most destructive flood during the whole modern history of Australia was caused by the unprecedented activity of the tropical cyclogenesis in the circulation system of the Australian summer monsoon. The tropical cyclones affected in turn the monsoon regions of Australia both from the Indian Ocean through the system of the equatorial zone of westerlies and from the Pacific Ocean through the system of the eastern trade wind. The Pacific trade wind during the Australian flood was maximally developed and the South Pacific high was shifted considerably from the coast of Peru and Chile to the center of the ocean. It is demonstrated that the maximum values of negative SST anomalies were observed not in the east of the Pacific Ocean as in the case of the “canonical” La Niña but they were shifted significantly to the west to the line of the date change. All this enables to refer the extreme La Niña 2010–2011 to La Niña of Modoki type. |
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container_issue |
2 |
title_short |
Synoptic aspects of the catastrophic flood formation in the northeast of Australia during extreme La Niña 2010–2011 |
url |
https://dx.doi.org/10.3103/S1068373912020033 |
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author2 |
Platonov, V. S. Sokolikhina, E. V. |
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Platonov, V. S. Sokolikhina, E. V. |
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doi_str |
10.3103/S1068373912020033 |
up_date |
2024-07-03T19:03:29.462Z |
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score |
7.3977556 |