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A high-resolution simulation of groundwater and surface water over most of the continental US with the integrated hydrologic model ParFlow v3

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Academic year: 2020

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Figure

Figure 1. Maps of top soil type (applied over the top 2 m of the model) (a), elevation (m a.s.l.) (b), bottom soil type (c), potential recharge,P –E, (m yr−1) (d), saturated hydraulic conductivity (m h−1; applied over the bottom 100 m of the model) (e) over the model domain (f).
Figure 2. Plot of observed streamflow (a) and observed water tabledepth (b).
Figure 3. Map of simulated surface flow (m3 s−1) over the CONUS domain with two insets zooming into the Ohio River basin
Figure 5. Scatterplots of simulated vs. observed hydraulic headand surface flow (a) (b).
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