Articles | Volume 30, issue 20
https://doi.org/10.5194/hess-30-6359-2026
https://doi.org/10.5194/hess-30-6359-2026
Research article
 | 
19 Oct 2026
Research article |  | 19 Oct 2026

Basin-scale evaluation of the Noah-MP land surface model for runoff and snow generation in the Missouri River Basin: insights and recommendations for parameterization scheme selection

Eunsaem Cho, Eunsang Cho, Carrie Vuyovich, Bailing Li, and Jennifer M. Jacobs

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Cited articles

Abolafia-Rosenzweig, R., He, C., Lin, T. S., Barlage, M., and Rittger, K.: Improved cross-scale snow cover simulations by developing a scale-aware ground snow cover fraction parameterization in the Noah-MP land surface model, J. Adv. Model. Earth Sy., 17, e2024MS004704, https://doi.org/10.1029/2024MS004704, 2025. 
Abolafia-Rosenzweig, R., He, C., Ikeda, K., Liu, C., Lin, T.-S., Barlage, M., Xue, L., Rasouli, K., Zhang, Y., Newman, A., and Dudhia, J.: Revisiting snow water equivalent bias in the Noah-MP land surface model in the western US, Water Resour. Res., 62, e2025WR042586, https://doi.org/10.1029/2025WR042586, 2026. 
Abramowitz, G., Leuning, R., Clark, M., and Pitman, A.: Evaluating the performance of land surface models, J. Climate, 21, 5468–5481, https://doi.org/10.1175/2008JCLI2378.1, 2008. 
Agnihotri, J., Behrangi, A., Tavakoly, A., Geheran, M., Farmani, M. A., and Niu, G.-Y.: Higher frozen soil permeability represented in a hydrological model improves spring streamflow prediction from river basin to continental scales, Water Resour. Res., 59, e2022WR033075, https://doi.org/10.1029/2022WR033075, 2023. 
Ahiablame, L., Sheshukov, A. Y., Rahmani, V., and Moriasi, D.: Annual baseflow variations as influenced by climate variability and agricultural land use change in the Missouri River Basin, J. Hydrol., 551, 188–202, https://doi.org/10.1016/j.jhydrol.2017.05.055, 2017. 
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Short summary
This study evaluated how alternative parameterization schemes in the Noah-Multiparameterization model affect snow and runoff in the Missouri River Basin. Simulations were compared with U.S. Geological Survey streamflow, University of Arizona snow water equivalent, and Global Land Evaporation Amsterdam Model evapotranspiration across 50 Hydro-Climate Data Network subbasins. As a result, we confirmed alternative schemes could improve groundwater, evapotranspiration, and runoff representation.
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