Large Ensemble Diagnostic Evaluation of Hydrologic Parameter Uncertainty in the Community Land Model Version 5 (CLM5)

Author:

Yan Hongxiang1ORCID,Sun Ning1ORCID,Eldardiry Hisham1ORCID,Thurber Travis B.1ORCID,Reed Patrick M.2ORCID,Malek Keyvan2ORCID,Gupta Rohini2ORCID,Kennedy Daniel3ORCID,Swenson Sean C.3ORCID,Hou Zhangshuan1ORCID,Cheng Yanyan4ORCID,Rice Jennie S.1ORCID

Affiliation:

1. Pacific Northwest National Laboratory Richland WA USA

2. Department of Civil and Environmental Engineering Cornell University Ithaca NY USA

3. National Center for Atmospheric Research Boulder CO USA

4. Department of Industrial Systems Engineering and Management National University of Singapore Singapore Singapore

Abstract

AbstractLand surface models such as the Community Land Model version 5 (CLM5) seek to enhance understanding of terrestrial hydrology and aid in the evaluation of anthropogenic and climate change impacts. However, the effects of parametric uncertainty on CLM5 hydrologic predictions across regions, timescales, and flow regimes have yet to be explored in detail. The common use of the default hydrologic model parameters in CLM5 risks generating streamflow predictions that may lead to incorrect inferences for important dynamics and/or extremes. In this study, we benchmark CLM5 streamflow predictions relative to the commonly employed default hydrologic parameters for 464 headwater basins over the conterminous United States (CONUS). We evaluate baseline CLM5 default parameter performance relative to a large (1,307) Latin Hypercube Sampling‐based diagnostic comparison of streamflow prediction skill using over 20 error measures. We provide a global sensitivity analysis that clarifies the significant spatial variations in parametric controls for CLM5 streamflow predictions across regions, temporal scales, and error metrics of interest. The baseline CLM5 shows relatively moderate to poor streamflow prediction skill in several CONUS regions, especially the arid Southwest and Central U.S. Hydrologic parameter uncertainty strongly affects CLM5 streamflow predictions, but its impacts vary in complex ways across U.S. regions, timescales, and flow regimes. Overall, CLM5's surface runoff and soil water parameters have the largest effects on simulated high flows, while canopy water and evaporation parameters have the most significant effects on the water balance.

Funder

U.S. Department of Energy

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Chemistry,Global and Planetary Change

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