On the vertical structure of Mediterranean explosive cyclones
Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evo...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kouroutzoglou, John [verfasserIn] Flocas, Helena A. [verfasserIn] Keay, Kevin [verfasserIn] Simmonds, Ian [verfasserIn] Hatzaki, Maria [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Wien [u.a.] : Springer, 1948, 110(2012), 1-2 vom: 15. März, Seite 155-176 |
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| Übergeordnetes Werk: |
volume:110 ; year:2012 ; number:1-2 ; day:15 ; month:03 ; pages:155-176 |
| Links: |
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| DOI / URN: |
10.1007/s00704-012-0620-3 |
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| Katalog-ID: |
SPR007328842 |
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| 100 | 1 | |a Kouroutzoglou, John |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a On the vertical structure of Mediterranean explosive cyclones |
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| 520 | |a Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. | ||
| 650 | 4 | |a Cyclone |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Mediterranean Cyclone |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Explosive Cyclone |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Surface Cyclone |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Isobaric Level |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Flocas, Helena A. |e verfasserin |4 aut | |
| 700 | 1 | |a Keay, Kevin |e verfasserin |4 aut | |
| 700 | 1 | |a Simmonds, Ian |e verfasserin |4 aut | |
| 700 | 1 | |a Hatzaki, Maria |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Theoretical and applied climatology |d Wien [u.a.] : Springer, 1948 |g 110(2012), 1-2 vom: 15. März, Seite 155-176 |w (DE-627)25490968X |w (DE-600)1463177-5 |x 1434-4483 |7 nnns |
| 773 | 1 | 8 | |g volume:110 |g year:2012 |g number:1-2 |g day:15 |g month:03 |g pages:155-176 |
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10.1007/s00704-012-0620-3 doi (DE-627)SPR007328842 (SPR)s00704-012-0620-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl Kouroutzoglou, John verfasserin aut On the vertical structure of Mediterranean explosive cyclones 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. Cyclone (dpeaa)DE-He213 Mediterranean Cyclone (dpeaa)DE-He213 Explosive Cyclone (dpeaa)DE-He213 Surface Cyclone (dpeaa)DE-He213 Isobaric Level (dpeaa)DE-He213 Flocas, Helena A. verfasserin aut Keay, Kevin verfasserin aut Simmonds, Ian verfasserin aut Hatzaki, Maria verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 110(2012), 1-2 vom: 15. März, Seite 155-176 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:110 year:2012 number:1-2 day:15 month:03 pages:155-176 https://dx.doi.org/10.1007/s00704-012-0620-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 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_2056 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 110 2012 1-2 15 03 155-176 |
| spelling |
10.1007/s00704-012-0620-3 doi (DE-627)SPR007328842 (SPR)s00704-012-0620-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl Kouroutzoglou, John verfasserin aut On the vertical structure of Mediterranean explosive cyclones 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. Cyclone (dpeaa)DE-He213 Mediterranean Cyclone (dpeaa)DE-He213 Explosive Cyclone (dpeaa)DE-He213 Surface Cyclone (dpeaa)DE-He213 Isobaric Level (dpeaa)DE-He213 Flocas, Helena A. verfasserin aut Keay, Kevin verfasserin aut Simmonds, Ian verfasserin aut Hatzaki, Maria verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 110(2012), 1-2 vom: 15. März, Seite 155-176 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:110 year:2012 number:1-2 day:15 month:03 pages:155-176 https://dx.doi.org/10.1007/s00704-012-0620-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 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_2056 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 110 2012 1-2 15 03 155-176 |
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10.1007/s00704-012-0620-3 doi (DE-627)SPR007328842 (SPR)s00704-012-0620-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl Kouroutzoglou, John verfasserin aut On the vertical structure of Mediterranean explosive cyclones 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. Cyclone (dpeaa)DE-He213 Mediterranean Cyclone (dpeaa)DE-He213 Explosive Cyclone (dpeaa)DE-He213 Surface Cyclone (dpeaa)DE-He213 Isobaric Level (dpeaa)DE-He213 Flocas, Helena A. verfasserin aut Keay, Kevin verfasserin aut Simmonds, Ian verfasserin aut Hatzaki, Maria verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 110(2012), 1-2 vom: 15. März, Seite 155-176 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:110 year:2012 number:1-2 day:15 month:03 pages:155-176 https://dx.doi.org/10.1007/s00704-012-0620-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 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_2056 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 110 2012 1-2 15 03 155-176 |
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10.1007/s00704-012-0620-3 doi (DE-627)SPR007328842 (SPR)s00704-012-0620-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl Kouroutzoglou, John verfasserin aut On the vertical structure of Mediterranean explosive cyclones 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. Cyclone (dpeaa)DE-He213 Mediterranean Cyclone (dpeaa)DE-He213 Explosive Cyclone (dpeaa)DE-He213 Surface Cyclone (dpeaa)DE-He213 Isobaric Level (dpeaa)DE-He213 Flocas, Helena A. verfasserin aut Keay, Kevin verfasserin aut Simmonds, Ian verfasserin aut Hatzaki, Maria verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 110(2012), 1-2 vom: 15. März, Seite 155-176 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:110 year:2012 number:1-2 day:15 month:03 pages:155-176 https://dx.doi.org/10.1007/s00704-012-0620-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 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_2056 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 110 2012 1-2 15 03 155-176 |
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10.1007/s00704-012-0620-3 doi (DE-627)SPR007328842 (SPR)s00704-012-0620-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.82 bkl Kouroutzoglou, John verfasserin aut On the vertical structure of Mediterranean explosive cyclones 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. Cyclone (dpeaa)DE-He213 Mediterranean Cyclone (dpeaa)DE-He213 Explosive Cyclone (dpeaa)DE-He213 Surface Cyclone (dpeaa)DE-He213 Isobaric Level (dpeaa)DE-He213 Flocas, Helena A. verfasserin aut Keay, Kevin verfasserin aut Simmonds, Ian verfasserin aut Hatzaki, Maria verfasserin aut Enthalten in Theoretical and applied climatology Wien [u.a.] : Springer, 1948 110(2012), 1-2 vom: 15. März, Seite 155-176 (DE-627)25490968X (DE-600)1463177-5 1434-4483 nnns volume:110 year:2012 number:1-2 day:15 month:03 pages:155-176 https://dx.doi.org/10.1007/s00704-012-0620-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GEO 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_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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 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_2056 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.82 ASE AR 110 2012 1-2 15 03 155-176 |
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Enthalten in Theoretical and applied climatology 110(2012), 1-2 vom: 15. März, Seite 155-176 volume:110 year:2012 number:1-2 day:15 month:03 pages:155-176 |
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Enthalten in Theoretical and applied climatology 110(2012), 1-2 vom: 15. März, Seite 155-176 volume:110 year:2012 number:1-2 day:15 month:03 pages:155-176 |
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Cyclone Mediterranean Cyclone Explosive Cyclone Surface Cyclone Isobaric Level |
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Kouroutzoglou, John @@aut@@ Flocas, Helena A. @@aut@@ Keay, Kevin @@aut@@ Simmonds, Ian @@aut@@ Hatzaki, Maria @@aut@@ |
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The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. 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Kouroutzoglou, John |
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Kouroutzoglou, John ddc 550 bkl 38.82 misc Cyclone misc Mediterranean Cyclone misc Explosive Cyclone misc Surface Cyclone misc Isobaric Level On the vertical structure of Mediterranean explosive cyclones |
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550 ASE 38.82 bkl On the vertical structure of Mediterranean explosive cyclones Cyclone (dpeaa)DE-He213 Mediterranean Cyclone (dpeaa)DE-He213 Explosive Cyclone (dpeaa)DE-He213 Surface Cyclone (dpeaa)DE-He213 Isobaric Level (dpeaa)DE-He213 |
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on the vertical structure of mediterranean explosive cyclones |
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On the vertical structure of Mediterranean explosive cyclones |
| abstract |
Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. |
| abstractGer |
Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. |
| abstract_unstemmed |
Abstract An attempt is made to explore the vertical structure of the surface explosive cyclones in the Mediterranean on a climatological basis during the cold period of the year in order to get a better insight in the interaction between the upper and lower levels responsible for the genesis and evolvement of the phenomenon. The vertical profile of the explosive cyclones was examined with the aid of the vertical tracing software of the University of Melbourne Cyclone Tracking Algorithm, using the 1 × 1° spatial resolution of ERA-40 reanalysis data. It was found that about 57 % of the track steps of surface explosive cyclones extend up to 500 hPa. The north-westward tilting of the surface cyclones with height during the stage of explosive cyclogenesis, with a mean distance of 350 km between mean sea and 500 hPa levels, confirms the importance of baroclinicity. About 45 % of the surface explosive cyclones reached their maximum depth before their 500 hPa counterparts, implying the role of surface processes. |
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| container_issue |
1-2 |
| title_short |
On the vertical structure of Mediterranean explosive cyclones |
| url |
https://dx.doi.org/10.1007/s00704-012-0620-3 |
| remote_bool |
true |
| author2 |
Flocas, Helena A. Keay, Kevin Simmonds, Ian Hatzaki, Maria |
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Flocas, Helena A. Keay, Kevin Simmonds, Ian Hatzaki, Maria |
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| doi_str |
10.1007/s00704-012-0620-3 |
| up_date |
2024-07-04T02:50:58.170Z |
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| score |
7.3974867 |