Stormwater quantity and quality response to climate change using artificial neural networks

被引:26
作者
He, Jianxun [1 ]
Valeo, Caterina [1 ]
Chu, Angus [1 ]
Neumann, Norman F. [2 ]
机构
[1] Univ Calgary, Schulich Sch Engn, Dept Civil Engn, Calgary, AB T2N 1N4, Canada
[2] Univ Alberta, Sch Publ Hlth, Edmonton, AB T6G 2R3, Canada
关键词
stormwater runoff; stormwater runoff quality; climate change; neural network; statistical downscaling; RIVER-BASIN; IMPACTS; RUNOFF; MODEL; SIMULATION; URBANIZATION; HELSINGBORG; DRAINAGE; SWEDEN; OUTPUT;
D O I
10.1002/hyp.7904
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
This research investigates the potential impacts of climate change on stormwater quantity and quality generated by urban residential areas on an event basis in the rainy season. An urban residential stormwater drainage area in southeast Calgary, Alberta, Canada is the focus of future climate projections from general circulation models (GCMs). A regression-based statistical downscaling tool was employed to conduct spatial downscaling of daily precipitation and daily mean temperature using projection outputs from the coupled GCM. Projected changes in precipitation and temperature were applied to current climate scenarios to generate future climate scenarios. Artificial neural networks (ANNs) developed for modelling stormwater runoff quantity and quality used projected climate scenarios as network inputs. The hydrological response to climate change was investigated through stormwater runoff volume and peak flow, while the water quality responses were investigated through the event mean value (EMV) of five parameters: turbidity, conductivity, water temperature, dissolved oxygen (DO) and pH. First flush (FF) effects were also noted. Under future climate scenarios, the EMVs of turbidity increased in all storms except for three events of short duration. The EMVs of conductivity were found to decline in small and frequent storms (return period < 5 years); but conductivity EMVs were observed to increase in intensive events (return period >= 5 years). In general, an increasing EMV was observed for water temperature, whereas a decreasing trend was found for DO EMV. No clear trend was found in the EMV of pH. In addition, projected future climate scenarios do not produce a stronger FF effect on dissolved solids and suspended solids compared to that produced by the current climate scenario. Copyright (C) 2010 John Wiley & Sons, Ltd.
引用
收藏
页码:1298 / 1312
页数:15
相关论文
共 51 条
[1]  
[Anonymous], 2001, Climate Change 2001: A Scientific Basis
[2]   Feasible adaptation strategies for increased risk of flooding in cities due to climate change [J].
Arnbjerg-Nielsen, K. ;
Fleischer, H. S. .
WATER SCIENCE AND TECHNOLOGY, 2009, 60 (02) :273-281
[3]   Distribution of pollutant mass vs volume in stormwater discharges and the first flush phenomenon [J].
Bertrand-Krajewski, JL ;
Chebbo, G ;
Saget, A .
WATER RESEARCH, 1998, 32 (08) :2341-2356
[4]   A transient climate change simulation with greenhouse gas and aerosol forcing: experimental design and comparison with the instrumental record for the twentieth century [J].
Boer, GJ ;
Flato, G ;
Reader, MC ;
Ramsden, D .
CLIMATE DYNAMICS, 2000, 16 (06) :405-425
[5]  
Booty W., 2005, Canadian Water Resources Journal, V30, P211
[6]   Comparison between kinematic wave and artificial neural network models in event-based runoff simulation for an overland plane [J].
Chua, Lloyd H. C. ;
Wong, Tommy S. W. ;
Sriramula, L. K. .
JOURNAL OF HYDROLOGY, 2008, 357 (3-4) :337-348
[7]   The first flush load of urban surface runoff [J].
Deletic, A .
WATER RESEARCH, 1998, 32 (08) :2462-2470
[8]   Assessment of possible impacts of climate change in an urban catchment [J].
Denault, Catherine ;
Millar, Robert G. ;
Lence, Barbara J. .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 2006, 42 (03) :685-697
[9]  
*DHI, 2004, MOUS TRAP TECHN REF
[10]   Hydrologic impact of climate change in the Saguenay watershed: comparison of downscaling methods and hydrologic models [J].
Dibike, YB ;
Coulibaly, P .
JOURNAL OF HYDROLOGY, 2005, 307 (1-4) :145-163