Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time
Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Aliev, A. S. [verfasserIn] Veliev, S. S. [verfasserIn] Tagieva, E. N. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2011 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Russian meteorology and hydrology - New York, NY : Allerton Press, 2007, 36(2011), 12 vom: Dez., Seite 806-810 |
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| Übergeordnetes Werk: |
volume:36 ; year:2011 ; number:12 ; month:12 ; pages:806-810 |
| Links: |
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| DOI / URN: |
10.3103/S1068373911120053 |
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| Katalog-ID: |
SPR023456825 |
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| 100 | 1 | |a Aliev, A. S. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time |
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| 520 | |a Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. | ||
| 650 | 4 | |a Holocene |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Late Pleistocene |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Azerbaijan |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a RUSSIAN Meteorology |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Quaternary Period |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Veliev, S. S. |e verfasserin |4 aut | |
| 700 | 1 | |a Tagieva, E. N. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Russian meteorology and hydrology |d New York, NY : Allerton Press, 2007 |g 36(2011), 12 vom: Dez., Seite 806-810 |w (DE-627)531203581 |w (DE-600)2324879-8 |x 1934-8096 |7 nnns |
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10.3103/S1068373911120053 doi (DE-627)SPR023456825 (SPR)S1068373911120053-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Aliev, A. S. verfasserin aut Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. Holocene (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Azerbaijan (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Quaternary Period (dpeaa)DE-He213 Veliev, S. S. verfasserin aut Tagieva, E. N. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 36(2011), 12 vom: Dez., Seite 806-810 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:36 year:2011 number:12 month:12 pages:806-810 https://dx.doi.org/10.3103/S1068373911120053 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 36 2011 12 12 806-810 |
| spelling |
10.3103/S1068373911120053 doi (DE-627)SPR023456825 (SPR)S1068373911120053-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Aliev, A. S. verfasserin aut Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. Holocene (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Azerbaijan (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Quaternary Period (dpeaa)DE-He213 Veliev, S. S. verfasserin aut Tagieva, E. N. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 36(2011), 12 vom: Dez., Seite 806-810 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:36 year:2011 number:12 month:12 pages:806-810 https://dx.doi.org/10.3103/S1068373911120053 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 36 2011 12 12 806-810 |
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10.3103/S1068373911120053 doi (DE-627)SPR023456825 (SPR)S1068373911120053-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Aliev, A. S. verfasserin aut Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. Holocene (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Azerbaijan (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Quaternary Period (dpeaa)DE-He213 Veliev, S. S. verfasserin aut Tagieva, E. N. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 36(2011), 12 vom: Dez., Seite 806-810 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:36 year:2011 number:12 month:12 pages:806-810 https://dx.doi.org/10.3103/S1068373911120053 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 36 2011 12 12 806-810 |
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10.3103/S1068373911120053 doi (DE-627)SPR023456825 (SPR)S1068373911120053-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Aliev, A. S. verfasserin aut Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. Holocene (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Azerbaijan (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Quaternary Period (dpeaa)DE-He213 Veliev, S. S. verfasserin aut Tagieva, E. N. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 36(2011), 12 vom: Dez., Seite 806-810 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:36 year:2011 number:12 month:12 pages:806-810 https://dx.doi.org/10.3103/S1068373911120053 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 36 2011 12 12 806-810 |
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10.3103/S1068373911120053 doi (DE-627)SPR023456825 (SPR)S1068373911120053-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Aliev, A. S. verfasserin aut Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. Holocene (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Azerbaijan (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Quaternary Period (dpeaa)DE-He213 Veliev, S. S. verfasserin aut Tagieva, E. N. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 36(2011), 12 vom: Dez., Seite 806-810 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:36 year:2011 number:12 month:12 pages:806-810 https://dx.doi.org/10.3103/S1068373911120053 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 36 2011 12 12 806-810 |
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Enthalten in Russian meteorology and hydrology 36(2011), 12 vom: Dez., Seite 806-810 volume:36 year:2011 number:12 month:12 pages:806-810 |
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Aliev, A. S. @@aut@@ Veliev, S. S. @@aut@@ Tagieva, E. N. @@aut@@ |
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Aliev, A. S. |
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Aliev, A. S. ddc 550 bkl 38.80 bkl 38.85 misc Holocene misc Late Pleistocene misc Azerbaijan misc RUSSIAN Meteorology misc Quaternary Period Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time |
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550 ASE 38.80 bkl 38.85 bkl Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time Holocene (dpeaa)DE-He213 Late Pleistocene (dpeaa)DE-He213 Azerbaijan (dpeaa)DE-He213 RUSSIAN Meteorology (dpeaa)DE-He213 Quaternary Period (dpeaa)DE-He213 |
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Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time |
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climate changes and the caspian sea level fluctuations in the holocene and historical time |
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Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time |
| abstract |
Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. |
| abstractGer |
Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. |
| abstract_unstemmed |
Abstract The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. The correspondence of the Late Khvalyn transgression to the time of the thawing of the European (Scandinavian) ice cap is revealed as well as that of the climatic optimum of the Holocene to the Boreal period (10-8 thousand years ago). In the next New-Caspian epoch, the Caspian Sea regression occurred. In the historical time, the maxima of cold snaps and Caspian Sea level are registered every five centuries. |
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Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time |
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| doi_str |
10.3103/S1068373911120053 |
| up_date |
2024-07-03T19:03:00.988Z |
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1803585722504970240 |
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S.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Climate changes and the Caspian Sea Level fluctuations in the Holocene and historical time</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2011</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 The influence of climate changes in Eurasia on the Caspian Sea level fluctuations in the Holocene is studied on the basis of historical data. 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