Prognostic models of development of processes of catastrophic long-term annual river runoff formation
Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distri...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kovalenko, V. V. [verfasserIn] Gaidukova, E. V. [verfasserIn] Chistyakov, D. V. [verfasserIn] Hamlili, A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2010 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Russian meteorology and hydrology - New York, NY : Allerton Press, 2007, 35(2010), 10 vom: Okt., Seite 695-699 |
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| Übergeordnetes Werk: |
volume:35 ; year:2010 ; number:10 ; month:10 ; pages:695-699 |
| Links: |
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| DOI / URN: |
10.3103/S1068373910100079 |
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| Katalog-ID: |
SPR023455403 |
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| 100 | 1 | |a Kovalenko, V. V. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Prognostic models of development of processes of catastrophic long-term annual river runoff formation |
| 264 | 1 | |c 2010 | |
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| 520 | |a Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distribution of instability zones throughout the European territory of Russia. | ||
| 650 | 4 | |a RUSSIAN Meteorology |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Runoff Coefficient |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Autocorrelation Coefficient |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Runoff Formation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a HADCM3 Model |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Gaidukova, E. V. |e verfasserin |4 aut | |
| 700 | 1 | |a Chistyakov, D. V. |e verfasserin |4 aut | |
| 700 | 1 | |a Hamlili, A. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Russian meteorology and hydrology |d New York, NY : Allerton Press, 2007 |g 35(2010), 10 vom: Okt., Seite 695-699 |w (DE-627)531203581 |w (DE-600)2324879-8 |x 1934-8096 |7 nnns |
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| 912 | |a GBV_ILN_2034 | ||
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| 912 | |a GBV_ILN_2055 | ||
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| 912 | |a GBV_ILN_2061 | ||
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| 912 | |a GBV_ILN_2065 | ||
| 912 | |a GBV_ILN_2068 | ||
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| 912 | |a GBV_ILN_2106 | ||
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| 912 | |a GBV_ILN_2110 | ||
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| 912 | |a GBV_ILN_2113 | ||
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| 912 | |a GBV_ILN_2118 | ||
| 912 | |a GBV_ILN_2119 | ||
| 912 | |a GBV_ILN_2122 | ||
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| 912 | |a GBV_ILN_2143 | ||
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| 912 | |a GBV_ILN_2188 | ||
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| 912 | |a GBV_ILN_4306 | ||
| 912 | |a GBV_ILN_4307 | ||
| 912 | |a GBV_ILN_4313 | ||
| 912 | |a GBV_ILN_4322 | ||
| 912 | |a GBV_ILN_4323 | ||
| 912 | |a GBV_ILN_4324 | ||
| 912 | |a GBV_ILN_4325 | ||
| 912 | |a GBV_ILN_4326 | ||
| 912 | |a GBV_ILN_4333 | ||
| 912 | |a GBV_ILN_4334 | ||
| 912 | |a GBV_ILN_4335 | ||
| 912 | |a GBV_ILN_4336 | ||
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| 912 | |a GBV_ILN_4393 | ||
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10.3103/S1068373910100079 doi (DE-627)SPR023455403 (SPR)S1068373910100079-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Kovalenko, V. V. verfasserin aut Prognostic models of development of processes of catastrophic long-term annual river runoff formation 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distribution of instability zones throughout the European territory of Russia. RUSSIAN Meteorology (dpeaa)DE-He213 Runoff Coefficient (dpeaa)DE-He213 Autocorrelation Coefficient (dpeaa)DE-He213 Runoff Formation (dpeaa)DE-He213 HADCM3 Model (dpeaa)DE-He213 Gaidukova, E. V. verfasserin aut Chistyakov, D. V. verfasserin aut Hamlili, A. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 35(2010), 10 vom: Okt., Seite 695-699 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:35 year:2010 number:10 month:10 pages:695-699 https://dx.doi.org/10.3103/S1068373910100079 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 35 2010 10 10 695-699 |
| spelling |
10.3103/S1068373910100079 doi (DE-627)SPR023455403 (SPR)S1068373910100079-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Kovalenko, V. V. verfasserin aut Prognostic models of development of processes of catastrophic long-term annual river runoff formation 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distribution of instability zones throughout the European territory of Russia. RUSSIAN Meteorology (dpeaa)DE-He213 Runoff Coefficient (dpeaa)DE-He213 Autocorrelation Coefficient (dpeaa)DE-He213 Runoff Formation (dpeaa)DE-He213 HADCM3 Model (dpeaa)DE-He213 Gaidukova, E. V. verfasserin aut Chistyakov, D. V. verfasserin aut Hamlili, A. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 35(2010), 10 vom: Okt., Seite 695-699 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:35 year:2010 number:10 month:10 pages:695-699 https://dx.doi.org/10.3103/S1068373910100079 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 35 2010 10 10 695-699 |
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10.3103/S1068373910100079 doi (DE-627)SPR023455403 (SPR)S1068373910100079-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Kovalenko, V. V. verfasserin aut Prognostic models of development of processes of catastrophic long-term annual river runoff formation 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distribution of instability zones throughout the European territory of Russia. RUSSIAN Meteorology (dpeaa)DE-He213 Runoff Coefficient (dpeaa)DE-He213 Autocorrelation Coefficient (dpeaa)DE-He213 Runoff Formation (dpeaa)DE-He213 HADCM3 Model (dpeaa)DE-He213 Gaidukova, E. V. verfasserin aut Chistyakov, D. V. verfasserin aut Hamlili, A. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 35(2010), 10 vom: Okt., Seite 695-699 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:35 year:2010 number:10 month:10 pages:695-699 https://dx.doi.org/10.3103/S1068373910100079 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 35 2010 10 10 695-699 |
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Enthalten in Russian meteorology and hydrology 35(2010), 10 vom: Okt., Seite 695-699 volume:35 year:2010 number:10 month:10 pages:695-699 |
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RUSSIAN Meteorology Runoff Coefficient Autocorrelation Coefficient Runoff Formation HADCM3 Model |
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Russian meteorology and hydrology |
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Kovalenko, V. V. @@aut@@ Gaidukova, E. V. @@aut@@ Chistyakov, D. V. @@aut@@ Hamlili, A. @@aut@@ |
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Kovalenko, V. V. |
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Kovalenko, V. V. ddc 550 bkl 38.80 bkl 38.85 misc RUSSIAN Meteorology misc Runoff Coefficient misc Autocorrelation Coefficient misc Runoff Formation misc HADCM3 Model Prognostic models of development of processes of catastrophic long-term annual river runoff formation |
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550 ASE 38.80 bkl 38.85 bkl Prognostic models of development of processes of catastrophic long-term annual river runoff formation RUSSIAN Meteorology (dpeaa)DE-He213 Runoff Coefficient (dpeaa)DE-He213 Autocorrelation Coefficient (dpeaa)DE-He213 Runoff Formation (dpeaa)DE-He213 HADCM3 Model (dpeaa)DE-He213 |
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prognostic models of development of processes of catastrophic long-term annual river runoff formation |
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Prognostic models of development of processes of catastrophic long-term annual river runoff formation |
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Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distribution of instability zones throughout the European territory of Russia. |
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Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distribution of instability zones throughout the European territory of Russia. |
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Abstract A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. The maps are obtained from the actual and expected climate displaying the distribution of instability zones throughout the European territory of Russia. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR023455403</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220111102533.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201006s2010 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3103/S1068373910100079</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR023455403</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)S1068373910100079-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">Kovalenko, V. V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Prognostic models of development of processes of catastrophic long-term annual river runoff formation</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2010</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 A technique is proposed of the estimation of the stability level of the runoff formation process within the frameworks of Markovian paradigm resulting in the solution in the form of the set of Pearson’s curves. 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