Temporal and Spatial Characteristics of Extreme Hourly Precipitation over Eastern China in the Warm Season
Based on hourly precipitation data in eastern China in the warm season during 1961-2000,spatial distributions of frequency for 20 mm h 1 and 50 mm h 1 precipitation were analyzed,and the criteria of short-duration rainfall events and severe rainfall events are discussed.Furthermore,the percentile me...
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          | Published in | Advances in atmospheric sciences Vol. 28; no. 5; pp. 1177 - 1183 | 
|---|---|
| Main Author | |
| Format | Journal Article | 
| Language | English | 
| Published | 
        Heidelberg
          SP Science Press
    
        01.09.2011
     Springer Nature B.V State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081  | 
| Subjects | |
| Online Access | Get full text | 
| ISSN | 0256-1530 1861-9533  | 
| DOI | 10.1007/s00376-011-0020-0 | 
Cover
| Abstract | Based on hourly precipitation data in eastern China in the warm season during 1961-2000,spatial distributions of frequency for 20 mm h 1 and 50 mm h 1 precipitation were analyzed,and the criteria of short-duration rainfall events and severe rainfall events are discussed.Furthermore,the percentile method was used to define local hourly extreme precipitation;based on this,diurnal variations and trends in extreme precipitation were further studied.The results of this study show that,over Yunnan,South China,North China,and Northeast China,the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening.In the Guizhou Plateau and the Sichuan Basin,the maximum frequency of extreme precipitation events occurs in the late night and/or early morning.And in the western Sichuan Plateau,the maximum frequency occurs in the middle of the night.The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in most parts of eastern China,especially in Northeast China and the middle and lower reaches of the Yangtze River,but precipitation has decreased significantly in North China in the past 50 years.In addition,stations in the Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime. | 
    
|---|---|
| AbstractList | Based on hourly precipitation data in eastern China in the warm season during 1961-2000, spatial distributions of frequency for 20 mm h super(-1) and 50 mm h super(-1) precipitation were analyzed, and the criteria of short-duration rainfall events and severe rainfall events are discussed. Furthermore, the percentile method was used to define local hourly extreme precipitation; based on this, diurnal variations and trends in extreme precipitation were further studied. The results of this study show that, over Yunnan, South China, North China, and Northeast China, the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening. In the Guizhou Plateau and the Sichuan Basin, the maximum frequency of extreme precipitation events occurs in the late night and/or early morning. And in the western Sichuan Plateau, the maximum frequency occurs in the middle of the night. The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in most parts of eastern China, especially in Northeast China and the middle and lower reaches of the Yangtze River, but precipitation has decreased significantly in North China in the past 50 years. In addition, stations in the Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime. P426.6; Based on hourly precipitation data in eastern China in the warm season during 1961 2000,spatial distributions of frequency for 20 mm h-1 and 50 mm h-1 precipitation were analyzed,and the criteria of short-duration rainfall events and severe rainfall events are discussed.Furthermore,the percentile method was used to define local hourly extreme precipitation; based on this,diurnal variations and trends in extreme precipitation were further studied.The results of this study show that,over Yunnan,South China,North China,and Northeast China,the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening.In the Guizhou Plateau and the Sichuan Basin,the maximum frequency of extreme precipitation events occursin the late night and/or early morning.And in the western Sichuan Plateau,the maximum frequency occursin the middle of the night.The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in mostparts of eastern China,especially in Northeast China and the middle and lower reaches of the Yangtze River,but precipitation has decreased significantly in North China in the past 50 years.In addition,stations inthe Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime. Based on hourly precipitation data in eastern China in the warm season during 1961–2000, spatial distributions of frequency for 20 mm h −1 and 50 mm h −1 precipitation were analyzed, and the criteria of short-duration rainfall events and severe rainfall events are discussed. Furthermore, the percentile method was used to define local hourly extreme precipitation; based on this, diurnal variations and trends in extreme precipitation were further studied. The results of this study show that, over Yunnan, South China, North China, and Northeast China, the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening. In the Guizhou Plateau and the Sichuan Basin, the maximum frequency of extreme precipitation events occurs in the late night and/or early morning. And in the western Sichuan Plateau, the maximum frequency occurs in the middle of the night. The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in most parts of eastern China, especially in Northeast China and the middle and lower reaches of the Yangtze River, but precipitation has decreased significantly in North China in the past 50 years. In addition, stations in the Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime. Based on hourly precipitation data in eastern China in the warm season during 1961-2000, spatial distributions of frequency for 20 mm h^sup -1^ and 50 mm h^sup -1^ precipitation were analyzed, and the criteria of short-duration rainfall events and severe rainfall events are discussed. Furthermore, the percentile method was used to define local hourly extreme precipitation; based on this, diurnal variations and trends in extreme precipitation were further studied. The results of this study show that, over Yunnan, South China, North China, and Northeast China, the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening. In the Guizhou Plateau and the Sichuan Basin, the maximum frequency of extreme precipitation events occurs in the late night and/or early morning. And in the western Sichuan Plateau, the maximum frequency occurs in the middle of the night. The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in most parts of eastern China, especially in Northeast China and the middle and lower reaches of the Yangtze River, but precipitation has decreased significantly in North China in the past 50 years. In addition, stations in the Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime.[PUBLICATION ABSTRACT] Based on hourly precipitation data in eastern China in the warm season during 1961-2000,spatial distributions of frequency for 20 mm h 1 and 50 mm h 1 precipitation were analyzed,and the criteria of short-duration rainfall events and severe rainfall events are discussed.Furthermore,the percentile method was used to define local hourly extreme precipitation;based on this,diurnal variations and trends in extreme precipitation were further studied.The results of this study show that,over Yunnan,South China,North China,and Northeast China,the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening.In the Guizhou Plateau and the Sichuan Basin,the maximum frequency of extreme precipitation events occurs in the late night and/or early morning.And in the western Sichuan Plateau,the maximum frequency occurs in the middle of the night.The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in most parts of eastern China,especially in Northeast China and the middle and lower reaches of the Yangtze River,but precipitation has decreased significantly in North China in the past 50 years.In addition,stations in the Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime.  | 
    
| Author | 张焕 翟盘茂 | 
    
| AuthorAffiliation | State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081 | 
    
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| Cites_doi | 10.1175/1520-0442(2001)014<2204:COEWHI>2.0.CO;2 10.1175/JCLI-3318.1 10.1175/JCLI3339.1 10.1175/1520-0477(2000)081<0417:OVATIE>2.3.CO;2 10.2151/jmsj.82.241 10.1175/1520-0493(2000)128<1194:COHREI>2.0.CO;2 10.1029/98JD02720 10.1029/2007GL030315 10.1080/07055900.2000.9649654 10.3354/cr019193 10.1002/joc.1763 10.2307/2285891 10.1175/1520-0477(1998)079<0231:STOPAF>2.0.CO;2 10.2151/jmsj.79.333 10.1023/A:1005428602279 10.2467/mripapers.39.79 10.1029/2005JD006290 10.1175/2008JCLI2188.1 10.1029/2003WR002073 10.1175/1520-0493(1975)103<0406:DVIPAT>2.0.CO;2 10.1007/s00703-004-0101-z 10.1175/1520-0450(1994)033<1445:SCOTDC>2.0.CO;2  | 
    
| ClassificationCodes | P426.6 | 
    
| ContentType | Journal Article | 
    
| Copyright | Chinese National Committee for International Association of Meteorology and Atmospheric Sciences, Institute of Atmospheric Physics, Science Press and Springer-Verlag Berlin Heidelberg 2011 Copyright © Wanfang Data Co. Ltd. All Rights Reserved.  | 
    
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| Notes | ZHANG Huan and ZHAI Panmao State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100081 hourly precipitation data; short-duration extreme precipitation; diurnal cycle; climatic distribution; trends Based on hourly precipitation data in eastern China in the warm season during 1961-2000,spatial distributions of frequency for 20 mm h 1 and 50 mm h 1 precipitation were analyzed,and the criteria of short-duration rainfall events and severe rainfall events are discussed.Furthermore,the percentile method was used to define local hourly extreme precipitation;based on this,diurnal variations and trends in extreme precipitation were further studied.The results of this study show that,over Yunnan,South China,North China,and Northeast China,the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening.In the Guizhou Plateau and the Sichuan Basin,the maximum frequency of extreme precipitation events occurs in the late night and/or early morning.And in the western Sichuan Plateau,the maximum frequency occurs in the middle of the night.The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in most parts of eastern China,especially in Northeast China and the middle and lower reaches of the Yangtze River,but precipitation has decreased significantly in North China in the past 50 years.In addition,stations in the Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime. 11-1925/O4 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 ObjectType-Article-1 ObjectType-Feature-2 content type line 23  | 
    
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| PublicationTitleAbbrev | Adv. Atmos. Sci | 
    
| PublicationTitleAlternate | Advances in Atmospheric Sciences | 
    
| PublicationTitle_FL | Advances in Atmospheric Sciences | 
    
| PublicationYear | 2011 | 
    
| Publisher | SP Science Press Springer Nature B.V State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081  | 
    
| Publisher_xml | – name: SP Science Press – name: Springer Nature B.V – name: State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081  | 
    
| References | Easterling, Evans, Groisman, Karl, Kunkel, Ambenje (CR5) 2000; 81 Frich, Alexander, Della-Marta, Gleason, Haylock, Tank, Peterson (CR6) 2002; 19 CR19 Yan, Yang (CR22) 2000; 5 Brooks, Stensrud (CR3) 2000; 128 CR12 Zhai, Sun, Ren, Liu, Gao, Zhang (CR24) 1999; 42 Kanae, Oki, Kashinda (CR9) 2004; 82 Bai, Liu, Liu (CR2) 2008; 51 Groisman, Knight, Easterling, Karl, Hegerl, Razuvaev (CR8) 2005; 18 Karl, Knight (CR10) 1998; 79 Zhang, Zwiers (CR27) 2004; 40 Sen (CR17) 1968; 63 Zhang, Vincent, Hogg, Niitsoo (CR28) 2000; 38 Zhai, Zhang, Pan, Wan (CR25) 2005; 18 Alexander (CR1) 2006; 111 Dai, Giorgi, Trenberth (CR4) 1999; 104 Qian, Lin (CR15) 2005; 90 Sen (CR18) 2008; 29 Wallace (CR20) 1975; 103 Ohsawa, Ueda, Hayashi, Watanabe, Matsumoto (CR13) 2001; 79 CR26 Yu, Xu, Zhou, Li (CR23) 1997; 34 Wang, Swail (CR21) 2001; 14 Fujibe (CR7) 1988; 39 Oki, Musiake (CR14) 1994; 33 Li, Yu, Zhou (CR11) 2008; 15 Qi, Huang (CR16) 2003; 14 P. M. Zhai (20_CR25) 2005; 18 X. Zhang (20_CR27) 2004; 40 20_CR19 P. Frich (20_CR6) 2002; 19 W. H. Qian (20_CR15) 2005; 90 G. Q. Qi (20_CR16) 2003; 14 J. Wallace (20_CR20) 1975; 103 20_CR12 A. J. Bai (20_CR2) 2008; 51 X. L. Wang (20_CR21) 2001; 14 P. K. Sen (20_CR17) 1968; 63 L. V. Alexander (20_CR1) 2006; 111 F. Fujibe (20_CR7) 1988; 39 X. Zhang (20_CR28) 2000; 38 R. S. Sen (20_CR18) 2008; 29 R. Yu (20_CR23) 1997; 34 Z. W. Yan (20_CR22) 2000; 5 20_CR26 H. E. Brooks (20_CR3) 2000; 128 T. R. Karl (20_CR10) 1998; 79 A. Dai (20_CR4) 1999; 104 T. Oki (20_CR14) 1994; 33 J. Li (20_CR11) 2008; 15 T. Ohsawa (20_CR13) 2001; 79 S. Kanae (20_CR9) 2004; 82 P. Y. Groisman (20_CR8) 2005; 18 D. R. Easterling (20_CR5) 2000; 81 P. M. Zhai (20_CR24) 1999; 42  | 
    
| References_xml | – volume: 14 start-page: 2204 year: 2001 end-page: 2220 ident: CR21 article-title: Changes of extreme wave heights in Northern Hemisphere oceans and related atmospheric circulation regimes publication-title: J. Climate doi: 10.1175/1520-0442(2001)014<2204:COEWHI>2.0.CO;2 – volume: 14 start-page: 12 issue: 3 year: 2003 end-page: 15 ident: CR16 article-title: Study on genetic and mechanical analysis of debris flow based on unsaturated soils mechanics publication-title: The Chinese Journal of Geological Hazard and Control – volume: 18 start-page: 1096 year: 2005 end-page: 1108 ident: CR25 article-title: Trends in Total Precipitation and Frequency of Daily Precipitation Extremes over China publication-title: J. Climate doi: 10.1175/JCLI-3318.1 – volume: 5 start-page: 267 issue: 3 year: 2000 end-page: 272 ident: CR22 article-title: Geographic patterns of extreme climate changes in China during 1951–1997 publication-title: Climatic and Environmental Research – volume: 18 start-page: 1326 year: 2005 end-page: 1350 ident: CR8 article-title: Trends in intense precipitation in the climate record publication-title: J. Climate doi: 10.1175/JCLI3339.1 – volume: 81 start-page: 417 year: 2000 end-page: 425 ident: CR5 article-title: Observed variability and trends in extreme climate events: A brief review publication-title: Bull. Amer. Meteor. Soc. doi: 10.1175/1520-0477(2000)081<0417:OVATIE>2.3.CO;2 – volume: 82 start-page: 241 year: 2004 end-page: 247 ident: CR9 article-title: Changes in hourly heavy precipitation at Tokyo from 1890 to 1999 publication-title: J. Meteor. Soc. Japan doi: 10.2151/jmsj.82.241 – ident: CR12 – volume: 128 start-page: 1194 year: 2000 end-page: 1201 ident: CR3 article-title: Climatology of heavy rain events in the United States from hourly precipitation observations publication-title: Mon. Wea. Rev. doi: 10.1175/1520-0493(2000)128<1194:COHREI>2.0.CO;2 – volume: 104 start-page: 6377 issue: D6 year: 1999 end-page: 6402 ident: CR4 article-title: Observed and model simulated diurnal cycles of precipitation over the contiguous United States publication-title: J. Geophys. Res. doi: 10.1029/98JD02720 – volume: 34 start-page: L13703 year: 1997 ident: CR23 article-title: Relation between rainfall duration and diurnal variation in the warm season precipitation over central eastern China publication-title: Geophys. Res. Lett. doi: 10.1029/2007GL030315 – volume: 38 start-page: 395 year: 2000 end-page: 429 ident: CR28 article-title: Temperature and precipitation trends in Canada during the 20th century publication-title: Atmos.-Ocean doi: 10.1080/07055900.2000.9649654 – volume: 19 start-page: 193 year: 2002 end-page: 212 ident: CR6 article-title: Observed coherent changes in climatic extremes during the second half of the twentieth century publication-title: Climate Research doi: 10.3354/cr019193 – volume: 29 start-page: 345 year: 2008 end-page: 355 ident: CR18 article-title: A spatial analysis of extreme hourly precipitation patterns in India publication-title: International Journal of Climatology doi: 10.1002/joc.1763 – volume: 63 start-page: 1379 year: 1968 end-page: 1389 ident: CR17 article-title: Estimates of the regression coefficient based on Kendall’s tau publication-title: Journal of the American Statistical Association doi: 10.2307/2285891 – ident: CR19 – volume: 51 start-page: 704 year: 2008 end-page: 714 ident: CR2 article-title: Diurnal variation of summer rainfall over the Tibetan Plateau and its neighboring regions revealed by TRMM Multisatellite Precipitation Analysis publication-title: Chinese Journal of Geophysics – volume: 79 start-page: 231 year: 1998 end-page: 241 ident: CR10 article-title: Secular trends of precipitation amount, frequency, and intensity in the United States publication-title: Bull. Amer. Meteor. Soc. doi: 10.1175/1520-0477(1998)079<0231:STOPAF>2.0.CO;2 – volume: 79 start-page: 333 year: 2001 end-page: 352 ident: CR13 article-title: Diurnal variations of convective activity and rainfall in tropical Asia publication-title: J. Meteor. Soc. Japan doi: 10.2151/jmsj.79.333 – volume: 42 start-page: 203 year: 1999 end-page: 218 ident: CR24 article-title: Changes of climate extremes in China publication-title: Climate Change doi: 10.1023/A:1005428602279 – volume: 39 start-page: 7994 year: 1988 ident: CR7 article-title: Diurnal variations of precipitation and thunderstorm frequency in Japan in the warm season publication-title: Papers in Meteorology and Geophysics doi: 10.2467/mripapers.39.79 – volume: 111 start-page: D05109 year: 2006 ident: CR1 article-title: Global observed changes in daily climate extremes of temperature publication-title: J. Geophys. Res. doi: 10.1029/2005JD006290 – volume: 15 start-page: 6036 year: 2008 end-page: 6043 ident: CR11 article-title: Seasonal variation of the diurnal of rainfall in southern contiguous China publication-title: J. Climate doi: 10.1175/2008JCLI2188.1 – volume: 40 start-page: W03805 year: 2004 ident: CR27 article-title: Comment on “Applicability of pre-whitening to eliminate the influence of serial correlation on the Mann-Kendall test” by Sheng Yue and Chun Yuan Wang publication-title: Water Resour. Res. doi: 10.1029/2003WR002073 – volume: 103 start-page: 406 year: 1975 end-page: 419 ident: CR20 article-title: Diurnal variations in precipitation and thunderstorm frequency over the conterminous United States publication-title: Mon. Wea. Rev. doi: 10.1175/1520-0493(1975)103<0406:DVIPAT>2.0.CO;2 – ident: CR26 – volume: 90 start-page: 193 issue: 3–4 year: 2005 end-page: 207 ident: CR15 article-title: Regional trends in recent precipitation indices in China publication-title: Meteor. Atmos. Phys. doi: 10.1007/s00703-004-0101-z – volume: 33 start-page: 1445 year: 1994 end-page: 1463 ident: CR14 article-title: Seasonal change of the diurnal cycle of precipitation over Japan and Malaysia publication-title: J. Appl. Meteor. doi: 10.1175/1520-0450(1994)033<1445:SCOTDC>2.0.CO;2 – volume: 81 start-page: 417 year: 2000 ident: 20_CR5 publication-title: Bull. Amer. Meteor. Soc. doi: 10.1175/1520-0477(2000)081<0417:OVATIE>2.3.CO;2 – volume: 40 start-page: W03805 year: 2004 ident: 20_CR27 publication-title: Water Resour. Res. doi: 10.1029/2003WR002073 – volume: 14 start-page: 2204 year: 2001 ident: 20_CR21 publication-title: J. Climate doi: 10.1175/1520-0442(2001)014<2204:COEWHI>2.0.CO;2 – volume: 5 start-page: 267 issue: 3 year: 2000 ident: 20_CR22 publication-title: Climatic and Environmental Research – volume: 104 start-page: 6377 issue: D6 year: 1999 ident: 20_CR4 publication-title: J. Geophys. Res. doi: 10.1029/98JD02720 – ident: 20_CR26 – volume: 38 start-page: 395 year: 2000 ident: 20_CR28 publication-title: Atmos.-Ocean doi: 10.1080/07055900.2000.9649654 – volume: 128 start-page: 1194 year: 2000 ident: 20_CR3 publication-title: Mon. Wea. Rev. doi: 10.1175/1520-0493(2000)128<1194:COHREI>2.0.CO;2 – volume: 33 start-page: 1445 year: 1994 ident: 20_CR14 publication-title: J. Appl. Meteor. doi: 10.1175/1520-0450(1994)033<1445:SCOTDC>2.0.CO;2 – volume: 34 start-page: L13703 year: 1997 ident: 20_CR23 publication-title: Geophys. Res. Lett. doi: 10.1029/2007GL030315 – volume: 51 start-page: 704 year: 2008 ident: 20_CR2 publication-title: Chinese Journal of Geophysics – volume: 103 start-page: 406 year: 1975 ident: 20_CR20 publication-title: Mon. Wea. Rev. doi: 10.1175/1520-0493(1975)103<0406:DVIPAT>2.0.CO;2 – ident: 20_CR19 – volume: 79 start-page: 333 year: 2001 ident: 20_CR13 publication-title: J. Meteor. Soc. Japan doi: 10.2151/jmsj.79.333 – volume: 111 start-page: D05109 year: 2006 ident: 20_CR1 publication-title: J. Geophys. Res. doi: 10.1029/2005JD006290 – volume: 18 start-page: 1326 year: 2005 ident: 20_CR8 publication-title: J. Climate doi: 10.1175/JCLI3339.1 – volume: 18 start-page: 1096 year: 2005 ident: 20_CR25 publication-title: J. Climate doi: 10.1175/JCLI-3318.1 – volume: 19 start-page: 193 year: 2002 ident: 20_CR6 publication-title: Climate Research doi: 10.3354/cr019193 – volume: 82 start-page: 241 year: 2004 ident: 20_CR9 publication-title: J. Meteor. Soc. Japan doi: 10.2151/jmsj.82.241 – volume: 15 start-page: 6036 year: 2008 ident: 20_CR11 publication-title: J. Climate doi: 10.1175/2008JCLI2188.1 – volume: 90 start-page: 193 issue: 3–4 year: 2005 ident: 20_CR15 publication-title: Meteor. Atmos. Phys. doi: 10.1007/s00703-004-0101-z – volume: 39 start-page: 7994 year: 1988 ident: 20_CR7 publication-title: Papers in Meteorology and Geophysics doi: 10.2467/mripapers.39.79 – volume: 79 start-page: 231 year: 1998 ident: 20_CR10 publication-title: Bull. Amer. Meteor. Soc. doi: 10.1175/1520-0477(1998)079<0231:STOPAF>2.0.CO;2 – volume: 63 start-page: 1379 year: 1968 ident: 20_CR17 publication-title: Journal of the American Statistical Association doi: 10.2307/2285891 – volume: 42 start-page: 203 year: 1999 ident: 20_CR24 publication-title: Climate Change doi: 10.1023/A:1005428602279 – volume: 14 start-page: 12 issue: 3 year: 2003 ident: 20_CR16 publication-title: The Chinese Journal of Geological Hazard and Control – volume: 29 start-page: 345 year: 2008 ident: 20_CR18 publication-title: International Journal of Climatology doi: 10.1002/joc.1763 – ident: 20_CR12  | 
    
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| Snippet | Based on hourly precipitation data in eastern China in the warm season during 1961-2000,spatial distributions of frequency for 20 mm h 1 and 50 mm h 1... Based on hourly precipitation data in eastern China in the warm season during 1961–2000, spatial distributions of frequency for 20 mm h −1 and 50 mm h −1... Based on hourly precipitation data in eastern China in the warm season during 1961-2000, spatial distributions of frequency for 20 mm h^sup -1^ and 50 mm h^sup... Based on hourly precipitation data in eastern China in the warm season during 1961-2000, spatial distributions of frequency for 20 mm h super(-1) and 50 mm h... P426.6; Based on hourly precipitation data in eastern China in the warm season during 1961 2000,spatial distributions of frequency for 20 mm h-1 and 50 mm h-1...  | 
    
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| SubjectTerms | Atmospheric Sciences Climate change Diurnal variations Earth and Environmental Science Earth Sciences Extreme weather Geophysics/Geodesy Hydrologic data Meteorology Precipitation Rainfall measurement Rivers Spatial distribution 中国东北地区 中国东部 小时 时空分布特征 暖季 极端降水 降水事件 降水量  | 
    
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| Title | Temporal and Spatial Characteristics of Extreme Hourly Precipitation over Eastern China in the Warm Season | 
    
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