Joint treatment of point measurement, sampling and neighborhood uncertainty in space-time rainfall mapping

被引:2
作者
Ehlers, L. B. [1 ,2 ]
Sonnenborg, T. O. [1 ]
Heuvelink, G. B. M. [3 ]
He, X. [1 ,4 ]
Refsgaard, J. C. [1 ]
机构
[1] Geol Survey Denmark & Greenland, Dept Hydrol, Oster Voldgade 10, DK-1350 Copenhagen, Denmark
[2] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen, Denmark
[3] Wageningen Univ, Soil Geog & Landscape Grp, NL-6708 PB Wageningen, Netherlands
[4] China Inst Water Resources & Hydropower Res IWHR, Dept Water Resources, Beijing 100038, Peoples R China
关键词
Rain gauge; Rainfall uncertainty; Sequential Gaussian simulation; Neighborhood uncertainty; Spatial and temporal support effects; SPATIOTEMPORAL INTERPOLATION; PRECIPITATION; VARIABILITY; CATCHMENT; FRAMEWORK; IMPACT; ERRORS;
D O I
10.1016/j.jhydrol.2019.03.100
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The importance of representing the spatial structure of rainfall accurately has been emphasized in various hydrological studies. It has also been widely acknowledged that there is a need to account for uncertainty in rainfall input. Common approaches focus on accounting for either point measurement or sampling uncertainty in rainfall estimation. We present a method that jointly considers three sources of uncertainty affecting the space-time mapping of rainfall: point measurement, sampling and neighborhood uncertainty. To our knowledge, neighborhood uncertainty has not been included in any prior rainfall uncertainty analysis. We generated an ensemble of 400 realizations of daily rainfall fields at a 2 km x 2 km spatial resolution for a catchment in Western Denmark (1055 km(2)). At the core of our method is the sequential Gaussian simulation (SGS) technique. Results indicate that our approach is able to reproduce key statistical features of the rainfall distribution. We examined the impact of different spatial (grid and catchment) and temporal supports (one day, one month, 5-year period) on the overall uncertainty. We also quantified the effect of each uncertainty source on rainfall field uncertainty. Finally, we compared our simulation results with those of a parallel expert elicitation study. We found that the expert elicitation uncertainty for average catchment rainfall in a 5-year period was considerably larger than quantified in our study (CV of 1.1% vs. 5%). An even larger discrepancy was found for the 5-year average of gauge rainfall, where expert elicitation resulted in a value that was an order of magnitude higher (CV of 0.2% vs. 2%). Possible reasons for this gap are discussed.
引用
收藏
页码:148 / 159
页数:12
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