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Runoff sensitivity to snow depletion curve representation within a continental scale hydrologic model
Author(s) -
Sexstone Graham A.,
Driscoll Jessica M.,
Hay Lauren E.,
Hammond John C.,
Barnhart Theodore B.
Publication year - 2020
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.13735
Subject(s) - snowmelt , surface runoff , environmental science , snow , watershed , hydrology (agriculture) , precipitation , spatial variability , meltwater , geology , meteorology , geomorphology , statistics , geography , ecology , geotechnical engineering , biology , mathematics , machine learning , computer science
The spatial variability of snow water equivalent (SWE) can exert a strong influence on the timing and magnitude of snowmelt delivery to a watershed. Therefore, the representation of sub‐grid or sub‐watershed snow variability in hydrologic models is important for accurately simulating snowmelt dynamics and runoff response. The U.S. Geological Survey National Hydrologic Model infrastructure with the precipitation‐runoff modelling system (NHM‐PRMS) represents the sub‐grid variability of SWE with snow depletion curves (SDCs), which relate snow‐covered area to watershed‐mean SWE during the snowmelt period. The main objective of this research was to evaluate the sensitivity of simulated runoff to SDC representation within the NHM‐PRMS across the continental United States (CONUS). SDCs for the model experiment were derived assuming a range of SWE coefficient of variation values and a lognormal probability distribution function. The NHM‐PRMS was simulated at a daily time step for each SDC over a 14‐year period. Results highlight that increasing the sub‐grid snow variability (by changing the SDC) resulted in a consistently slower snowmelt rate and longer snowmelt duration when averaged across the hydrologic response unit scale. Simulated runoff was also found to be sensitive to SDC representation, as decreases in simulated snowmelt rate by 1 mm day −1 resulted in decreases in runoff ratio by 1.8% on average in snow‐dominated regions of the CONUS. Simulated decreases in runoff associated with slower snowmelt rates were approximately inversely proportional to increases in simulated evapotranspiration. High snow persistence and peak SWE:annual precipitation combined with a water‐limited dryness index was associated with the greatest runoff sensitivity to changing snowmelt. Results from this study highlight the importance of carefully parameterizing SDCs for hydrologic modelling. Furthermore, improving model representation of snowmelt input variability and its relation to runoff generation processes is shown to be an important consideration for future modelling applications.