Using expert elicitation to quantify catchment water balances and their uncertainties. Issue 7 (2nd July 2016)

• Record Type: Journal Article
• Authors: Sebok, E.; Refsgaard, J. C.; Warmink, J. J.; Stisen, S.; Jensen, K. H.
• Is Part Of: Water resources research. Volume 52:Issue 7(2016:Jul.)
• Page Start: 5111
• Page End: 5131
• Publication Date: 2016-07-02
• Subjects: expert elicitation -- catchment hydrology -- water balance -- uncertainty analysis -- multistep elicitation; Hydrology -- Periodicals; 333.91
• DOI: 10.1002/2015WR018461
• Languages: English
• ISSNs: 0043-1397

Abstract

Abstract: Expert elicitation with the participation of 35 experts was used to estimate a water balance for the nested Ahlergaarde and Holtum catchments in Western Denmark. Average annual values of precipitation, evapotranspiration, and surface runoff as well as subsurface outflow and recharge and their uncertainty were estimated in a multistep elicitation, where experts first gave their opinion on the probability distribution of their water balance component of interest, then the average annual values and uncertainty of water balance components and catchment‐scale water balances were obtained by reaching consensus during group discussions. The obtained water balance errors for the 1055 km 2 Ahlergaarde catchment and 120 km 2 Holtum catchment were −5 and −62 mm/yr, respectively, with an uncertainty of 66 and 86 mm/yr, respectively. As an advantage of the expert elicitation, drawing on the intuitive experience and capabilities of experts to assess complex, site‐specific problems, the contribution of independent sources of uncertainties to the total uncertainty was also evaluated similarly to the subsurface outflow component, which traditionally is estimated as the residual of the water balance. Key Points: Expert elicitation can be used to calculate catchment water balance and its uncertainty A multistep elicitation of a uniquely high number of experts gradually improved the water balance With the expert elicitation approach subsurface outflow and its uncertainty can be quantified