Uncertainty in water resources management is in part about variability and in part about ambiguity. Both are associated with lack of clarity because of the behavior of all system components, lack of data, lack of detail, lack of structure to consider the water resources management problems, working and framing assumptions being used to consider the problems, known and unknown sources of bias, and ignorance about how much effort it is worth expending to clarify the management situation. The two major sources of variability are temporal and spatial heterogeneity. Temporal variability occurs when values fluctuate with time. Other values which are affected by spatial variability are dependent upon location of an area. A major part of the water resources management risk confusion relates to an inadequate distinction between the objective risk (real, physical) and subjective (perceived) risk. Because of the confusion between the two concepts, many characteristics of subjective risk are believed to be valid also for objective risk. The main objective of this paper is to initiate a discussion of the possible methodology for the reliability analysis of water resources systems that will be capable of: (a) addressing water resources uncertainty caused by variability and ambiguity, (b) integrating objective and subjective risk and (c) assisting the water resources management based on better understanding of temporal and spatial variability of risk.
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Research Article|
July 01 2009
A new method for spatial and temporal analysis of risk in water resources management
Slobodan P. Simonovic
1Department of Civil and Environmental Engineering, University of Western Ontario, London Ontario, Canada N6A 5B9
E-mail: [email protected]
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Journal of Hydroinformatics (2009) 11 (3-4): 320–329.
Article history
Received:
March 13 2008
Accepted:
May 29 2008
Citation
Slobodan P. Simonovic; A new method for spatial and temporal analysis of risk in water resources management. Journal of Hydroinformatics 1 July 2009; 11 (3-4): 320–329. doi: https://doi.org/10.2166/hydro.2009.018
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