Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow
Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainf...
Ausführliche Beschreibung
Autor*in: |
Chalov, S. R. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2023 |
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Schlagwörter: |
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Anmerkung: |
© Pleiades Publishing, Ltd. 2023 |
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Übergeordnetes Werk: |
Enthalten in: Russian meteorology and hydrology - New York, NY : Allerton Press, 2007, 48(2023), 2 vom: Feb., Seite 138-146 |
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Übergeordnetes Werk: |
volume:48 ; year:2023 ; number:2 ; month:02 ; pages:138-146 |
Links: |
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DOI / URN: |
10.3103/S1068373923020061 |
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Katalog-ID: |
SPR051586223 |
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100 | 1 | |a Chalov, S. R. |e verfasserin |4 aut | |
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520 | |a Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. | ||
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700 | 1 | |a Platonov, V. S. |4 aut | |
700 | 1 | |a Moreido, V. M. |4 aut | |
700 | 1 | |a Samokhin, M. A. |4 aut | |
700 | 1 | |a Yarynich, Yu. I. |4 aut | |
700 | 1 | |a Korshunova, N. N. |4 aut | |
700 | 1 | |a Bolgov, M. V. |4 aut | |
700 | 1 | |a Kasimov, N. S. |4 aut | |
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10.3103/S1068373923020061 doi (DE-627)SPR051586223 (SPR)S1068373923020061-e DE-627 ger DE-627 rakwb eng Chalov, S. R. verfasserin aut Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2023 Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. extreme rainfall (dpeaa)DE-He213 urban runoff (dpeaa)DE-He213 flood (dpeaa)DE-He213 COSMO-CLM (dpeaa)DE-He213 Platonov, V. S. aut Moreido, V. M. aut Samokhin, M. A. aut Yarynich, Yu. I. aut Korshunova, N. N. aut Bolgov, M. V. aut Kasimov, N. S. aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 48(2023), 2 vom: Feb., Seite 138-146 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:48 year:2023 number:2 month:02 pages:138-146 https://dx.doi.org/10.3103/S1068373923020061 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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 AR 48 2023 2 02 138-146 |
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10.3103/S1068373923020061 doi (DE-627)SPR051586223 (SPR)S1068373923020061-e DE-627 ger DE-627 rakwb eng Chalov, S. R. verfasserin aut Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2023 Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. extreme rainfall (dpeaa)DE-He213 urban runoff (dpeaa)DE-He213 flood (dpeaa)DE-He213 COSMO-CLM (dpeaa)DE-He213 Platonov, V. S. aut Moreido, V. M. aut Samokhin, M. A. aut Yarynich, Yu. I. aut Korshunova, N. N. aut Bolgov, M. V. aut Kasimov, N. S. aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 48(2023), 2 vom: Feb., Seite 138-146 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:48 year:2023 number:2 month:02 pages:138-146 https://dx.doi.org/10.3103/S1068373923020061 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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 AR 48 2023 2 02 138-146 |
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10.3103/S1068373923020061 doi (DE-627)SPR051586223 (SPR)S1068373923020061-e DE-627 ger DE-627 rakwb eng Chalov, S. R. verfasserin aut Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2023 Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. extreme rainfall (dpeaa)DE-He213 urban runoff (dpeaa)DE-He213 flood (dpeaa)DE-He213 COSMO-CLM (dpeaa)DE-He213 Platonov, V. S. aut Moreido, V. M. aut Samokhin, M. A. aut Yarynich, Yu. I. aut Korshunova, N. N. aut Bolgov, M. V. aut Kasimov, N. S. aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 48(2023), 2 vom: Feb., Seite 138-146 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:48 year:2023 number:2 month:02 pages:138-146 https://dx.doi.org/10.3103/S1068373923020061 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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 AR 48 2023 2 02 138-146 |
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10.3103/S1068373923020061 doi (DE-627)SPR051586223 (SPR)S1068373923020061-e DE-627 ger DE-627 rakwb eng Chalov, S. R. verfasserin aut Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2023 Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. extreme rainfall (dpeaa)DE-He213 urban runoff (dpeaa)DE-He213 flood (dpeaa)DE-He213 COSMO-CLM (dpeaa)DE-He213 Platonov, V. S. aut Moreido, V. M. aut Samokhin, M. A. aut Yarynich, Yu. I. aut Korshunova, N. N. aut Bolgov, M. V. aut Kasimov, N. S. aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 48(2023), 2 vom: Feb., Seite 138-146 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:48 year:2023 number:2 month:02 pages:138-146 https://dx.doi.org/10.3103/S1068373923020061 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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 AR 48 2023 2 02 138-146 |
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10.3103/S1068373923020061 doi (DE-627)SPR051586223 (SPR)S1068373923020061-e DE-627 ger DE-627 rakwb eng Chalov, S. R. verfasserin aut Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2023 Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. extreme rainfall (dpeaa)DE-He213 urban runoff (dpeaa)DE-He213 flood (dpeaa)DE-He213 COSMO-CLM (dpeaa)DE-He213 Platonov, V. S. aut Moreido, V. M. aut Samokhin, M. A. aut Yarynich, Yu. I. aut Korshunova, N. N. aut Bolgov, M. V. aut Kasimov, N. S. aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 48(2023), 2 vom: Feb., Seite 138-146 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:48 year:2023 number:2 month:02 pages:138-146 https://dx.doi.org/10.3103/S1068373923020061 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_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 AR 48 2023 2 02 138-146 |
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Chalov, S. R. @@aut@@ Platonov, V. S. @@aut@@ Moreido, V. M. @@aut@@ Samokhin, M. A. @@aut@@ Yarynich, Yu. I. @@aut@@ Korshunova, N. N. @@aut@@ Bolgov, M. V. @@aut@@ Kasimov, N. S. @@aut@@ |
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Chalov, S. R. |
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Chalov, S. R. misc extreme rainfall misc urban runoff misc flood misc COSMO-CLM Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow |
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Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow extreme rainfall (dpeaa)DE-He213 urban runoff (dpeaa)DE-He213 flood (dpeaa)DE-He213 COSMO-CLM (dpeaa)DE-He213 |
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Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow |
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Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow |
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Chalov, S. R. Platonov, V. S. Moreido, V. M. Samokhin, M. A. Yarynich, Yu. I. Korshunova, N. N. Bolgov, M. V. Kasimov, N. S. |
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small urban river runoff response to 2020 and 2021 extreme rainfalls on the territory of moscow |
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Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow |
abstract |
Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. © Pleiades Publishing, Ltd. 2023 |
abstractGer |
Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. © Pleiades Publishing, Ltd. 2023 |
abstract_unstemmed |
Abstract An important trend of modern development is the concentration of population in urban agglomerations, where a specific meso- and micro-climate is created under conditions of dramatically transformed natural landscapes. In the present paper, the long-term statistical analysis of intense rainfalls and annual daily precipitation maxima was carried out based on the Moscow region weather stations timeseries for the period of 1966–2021. An increase in the variability of intense precipitation over the Moscow region corresponding to the formation of significant floods was revealed in some years. The COSMO-CLM model simulated extreme precipitation for the basin of the Setun’ River (190 $ km^{2} $), the largest right-bank tributary of the Moskva River within the Moscow city, which was recorded over Moscow in May 2020 and June 2021. Maximum precipitation was registered over the Setun’ River basin during 45–90 minutes and induced rainfall floods that exceeded the spring flood by two times. The estimated basin travel time was 6–8 hours. Rainfalls form a multistep hydrograph inheriting the shower precipitation structure on small rivers. © Pleiades Publishing, Ltd. 2023 |
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title_short |
Small Urban River Runoff Response to 2020 and 2021 Extreme Rainfalls on the Territory of Moscow |
url |
https://dx.doi.org/10.3103/S1068373923020061 |
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author2 |
Platonov, V. S. Moreido, V. M. Samokhin, M. A. Yarynich, Yu. I. Korshunova, N. N. Bolgov, M. V. Kasimov, N. S. |
author2Str |
Platonov, V. S. Moreido, V. M. Samokhin, M. A. Yarynich, Yu. I. Korshunova, N. N. Bolgov, M. V. Kasimov, N. S. |
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up_date |
2024-07-03T22:40:48.596Z |
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score |
7.3995323 |