Intensity-Duration-Frequency (IDF) rainfall curves, for data series and climate projection in African cities

被引:68
作者
De Paola, Francesco [1 ,2 ]
Giugni, Maurizio [1 ,2 ]
Topa, Maria Elena [2 ]
Bucchignani, Edoardo [3 ,4 ]
机构
[1] Univ Naples Federico II, DICEA, Naples, Italy
[2] AMRA Sca Rl, Naples, Italy
[3] Ctr Euromediterraneo Cambiamenti Climat CMCC, Capua, CE, Italy
[4] CIRA, Capua, CE, Italy
关键词
Intensity; Duration; Frequency curves; Disaggregation analysis; Climate change; Africa; DISAGGREGATION; PRECIPITATION; MODEL;
D O I
10.1186/2193-1801-3-133
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Changes in the hydrologic cycle due to increase in greenhouse gases cause variations in intensity, duration, and frequency of precipitation events. Quantifying the potential effects of climate change and adapting to them is one way to reduce urban vulnerability. Since rainfall characteristics are often used to design water structures, reviewing and updating rainfall characteristics (i.e., Intensity-Duration-Frequency (IDF) curves) for future climate scenarios is necessary (Reg Environ Change 13(1 Supplement): 25-33, 2013). The present study regards the evaluation of the IDF curves for three case studies: Addis Ababa (Ethiopia), Dar Es Salaam (Tanzania) and Douala (Cameroon). Starting from daily rainfall observed data, to define the IDF curves and the extreme values in a smaller time window (10', 30', 1 h, 3 h, 6 h, 12 h), disaggregation techniques of the collected data have been used, in order to generate a synthetic sequence of rainfall, with statistical properties similar to the recorded data. Then, the rainfall pattern of the three test cities was analyzed and IDF curves were evaluated. In order to estimate the contingent influence of climate change on the IDF curves, the described procedure was applied to the climate (rainfall) simulations over the time period 2010-2050, provided by CMCC (Centro Euro-Mediterraneo sui Cambiamenti Climatici). The evaluation of the IDF curves allowed to frame the rainfall evolution of the three case studies, considering initially only historical data, then taking into account the climate projections, in order to verify the changes in rainfall patterns. The same set of data and projections was also used for evaluating the Probable Maximum Precipitation (PMP).
引用
收藏
页码:1 / 18
页数:18
相关论文
共 29 条
[1]   Recent climate change in the Arabian Peninsula: annual rainfall and temperature analysis of Saudi Arabia for 1978-2009 [J].
Almazroui, Mansour ;
Islam, M. Nazrul ;
Athar, H. ;
Jones, D. ;
Rahman, M. Ashfaqur .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2012, 32 (06) :953-966
[2]   Effects of changing rainfall patterns on WSUD in Australia [J].
Beecham, Simon ;
Chowdhury, Rezaul .
PROCEEDINGS OF THE INSTITUTION OF CIVIL ENGINEERS-WATER MANAGEMENT, 2012, 165 (05) :285-298
[3]   Estimation of the probable maximum precipitation in Barcelona (Spain) [J].
Casas, M. Carmen ;
Rodriguez, Rauel ;
Prohom, Marc ;
Gazquez, Antonio ;
Redano, Angel .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2011, 31 (09) :1322-1327
[4]  
Chow V.T., 1951, EOS T AM GEOPHYS UN, V32, P231, DOI DOI 10.1029/TR032I002P00231
[5]   Australian rainfall trends and their relation to the southern oscillation index [J].
Chowdhury, R. K. ;
Beecham, S. .
HYDROLOGICAL PROCESSES, 2010, 24 (04) :504-514
[6]   A daily rainfall disaggregation model [J].
Connolly, RD ;
Schirmer, J ;
Dunn, PK .
AGRICULTURAL AND FOREST METEOROLOGY, 1998, 92 (02) :105-117
[7]   Unjust waters: climate change, flooding and the urban poor in Africa [J].
Douglas, Ian ;
Alam, Kurshid ;
Maghenda, MaryAnne ;
McDonnell, Yasmin ;
McLean, Louise ;
Campbell, Jack .
ENVIRONMENT AND URBANIZATION, 2008, 20 (01) :187-205
[8]  
El-Hadji IT, 2002, WATER SA, V28
[9]   A method for statistical downscaling of seasonal ensemble predictions [J].
Feddersen, H ;
Andersen, U .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2005, 57 (03) :398-408
[10]  
Giugni M, 2012, HAZARD SCENARIOS TES