Sensitivity of Dynamical Downscaling Seasonal Precipitation Forecasts to Convection and Land Surface Parameterization in a High-Resolution Regional Climate Model

<div>Spatial patterns of vertically integrated (from 1,000 to 300 hPa) moisture fluxes (100 g/cm s<sup>−1</sup>) (arrows) and moisture flux convergence (multiplied by 10<sup>−5</sup> s<sup>−1</sup>) (shaded areas) of ERA-5 reanalysis, CFS reforecasts, and the WRF model in (a) spring, (b) summer, (c) autumn, and (d) winter.</div>

Advances in Meteorology

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Figure 6

Figure 6: Sensitivity of Dynamical Downscaling Seasonal Precipitation Forecasts to Convection and Land Surface Parameterization in a High-Resolution Regional Climate Model 

Figure 6 | Sensitivity of Dynamical Downscaling Seasonal Precipitation Forecasts to Convection and Land Surface Parameterization in a High-Resolution Regional Climate Model 