A novel subgrid model improves the representation of hydrologic processes.
Microtopography is known to be an important control on surface water retention, evaporation, infiltration, and runoff generation. Unfortunately, direct representation of microtopography effects in models of those processes is typically not feasible because of the high spatial and temporal resolution required. A subgrid model was developed to include microtopography effects in lower-resolution models, thus improving the representation of key hydrologic processes.
The newly developed subgrid model is broadly applicable to disparate landscapes and significantly improves the representation of runoff generation and inundation compared with neglecting small-scale topography. The subgrid model enables process-resolving models of permafrost thermal hydrology to expand to catchment scales and decadal timeframes.
Fine-scale simulations using high-resolution digital elevation models highlight the importance of microtopography and its effects on integrated hydrology in polygonal tundra, hummocky bogs, and hillslopes with incised rills. A subgrid model that modifies the flow and accumulation terms in lower-resolution models replicates the microtopography-resolving simulations at orders-of-magnitude smaller computation cost. The subgrid model makes it possible to incorporate thaw-induced dynamic topography in simulations addressing the evolution of carbon-rich Arctic tundra in a warming climate.
Contacts (BER PM)
David Lesmes and Daniel Stover
David.Lesmes@science.doe.gov and Daniel.Stover@science.doe.gov
Climate Change Science Institute, Oak Ridge National Laboratory
This work was supported by Interoperable Design of Extreme-scale Application Software (IDEAS) project and by the Next Generation Ecosystem Experiment (NGEE-Arctic) project.
Jan, A., E.T. Coon, J.D. Graham, and S.L. Painter, “A subgrid approach for modeling microtopography effects on overland flow.” Water Resources Research, 54(9), 6153-6167 (2018). [DOI:10.1029/2017WR021898]
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