The Impact of Meteorological Forcing Uncertainty on Hydrological Modeling: A Global Analysis of Cryosphere Basins

被引:22
作者
Tang, Guoqiang [1 ,2 ]
Clark, Martyn P. [1 ,3 ]
Knoben, Wouter J. M. [1 ]
Liu, Hongli [1 ]
Gharari, Shervan [4 ]
Arnal, Louise [1 ]
Beck, Hylke E. [5 ]
Wood, Andrew W. [2 ]
Newman, Andrew J. [6 ]
Papalexiou, Simon Michael [7 ]
机构
[1] Univ Saskatchewan, Ctr Hydrol, Canmore, AB, Canada
[2] Natl Ctr Atmospher Res, Climate & Global Dynam, Boulder, CO 80305 USA
[3] Univ Saskatchewan, Dept Geog & Planning, Saskatoon, SK, Canada
[4] Univ Saskatchewan, Ctr Hydrol, Saskatoon, SK, Canada
[5] King Abdullah Univ Sci & Technol, Thuwal, Saudi Arabia
[6] Natl Ctr Atmospher Res, Res Applicat Lab, Boulder, CO USA
[7] Univ Calgary, Dept Civil Engn, Calgary, AB, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
hydrological model; precipitation; air temperature; uncertainty; cryosphere; FRACTIONAL SNOW COVER; PRECIPITATION DATA; CLIMATE-CHANGE; ENSEMBLE PRECIPITATION; AIR-TEMPERATURE; RAINFALL; RUNOFF; CATCHMENT; DATASET; TRENDS;
D O I
10.1029/2022WR033767
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Meteorological forcing is a major source of uncertainty in hydrological modeling. The recent development of probabilistic large-domain meteorological data sets enables convenient uncertainty characterization, which however is rarely explored in large-domain research. This study analyzes how uncertainties in meteorological forcing data affect hydrological modeling in 289 representative cryosphere basins by forcing the Structure for Unifying Multiple Modeling Alternatives (SUMMA) and mizuRoute models with precipitation and air temperature ensembles from the Ensemble Meteorological Data set for Planet Earth (EM-Earth). EM-Earth probabilistic estimates are used in ensemble simulation for uncertainty analysis. The results reveal the magnitude, spatial distribution, and scale effect of uncertainties in meteorological, snow, runoff, soil water, and energy variables. There are three main findings. (a) The uncertainties in precipitation and temperature lead to substantial uncertainties in hydrological model outputs, some of which exceed 100% of the magnitude of the output variables themselves. (b) The uncertainties of different variables show distinct scale effects caused by spatial averaging or temporal averaging. (c) Precipitation uncertainties have the dominant impact for most basins and variables, while air temperature uncertainties are also nonnegligible, sometimes contributing more to modeling uncertainties than precipitation uncertainties. We find that three snow-related variables (snow water equivalent, snowfall amount, and snowfall fraction) can be used to estimate the impact of air temperature uncertainties for different model output variables. In summary, this study provides insight into the impact of probabilistic data sets on hydrological modeling and quantifies the uncertainties in cryosphere basin modeling that stem from the meteorological forcing data.
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页数:31
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