Table 2 Validation metric ratios are shown for RMSE, coverage, upper coverage, and width for the posterior with temperature dependence compared to without temperature dependence (denoted as p, ϕ and p, !ϕ, respectively, in the table header).
From: Physics-guided probabilistic modeling of extreme precipitation under climate change
Watershed | \(\frac{RMS{E}_{p,\varphi }}{RMS{E}_{p,!\varphi }}\) | \(\frac{co{v}_{p,\varphi }}{co{v}_{p,!\varphi }}\) | \(\frac{co{v}_{p,\varphi }^{u}}{co{v}_{p,!\varphi }^{u}}\) | \(\frac{{W}_{p,\varphi }}{{W}_{p,!\varphi }}\) |
|---|---|---|---|---|
Arkansas-White-Red | 1.06 | 0.99 | 0.99 | 1.00 |
California | 0.96 | 1.00 | 1.00 | 1.00 |
Great Basin | 1.04 | 1.00 | 1.02 | 1.04 |
Great Lakes | 0.93 | 1.04 | 1.01 | 1.02 |
Lower Colorado | 1.02 | 1.01 | 1.01 | 1.00 |
Lower Mississippi | 0.97 | 1.00 | 1.00 | 0.99 |
Mid Atlantic | 1.04 | 0.99 | 0.99 | 1.00 |
Missouri | 0.96 | 1.02 | 1.02 | 1.00 |
New England | 1.00 | 0.99 | 0.99 | 0.97 |
Ohio | 1.03 | 0.99 | 1.00 | 0.99 |
Pacific Northwest | 0.99 | 1.00 | 0.99 | 0.98 |
Rio Grande | 1.05 | 0.98 | 1.00 | 0.95 |
Souris-Red-Rainy | 1.02 | 0.99 | 1.00 | 1.00 |
South Atlantic-Gulf | 1.00 | 1.00 | 1.00 | 1.03 |
Tennessee | 1.02 | 1.00 | 1.00 | 1.00 |
Texas-Gulf | 1.05 | 1.00 | 1.00 | 1.00 |
Upper Colorado | 0.95 | 0.99 | 1.00 | 0.96 |
Upper Mississippi | 0.85 | 1.02 | 1.00 | 1.00 |
