over the high Sierra Madre Occidental, the western and eastern slopes, the Gulf of California
coastal plain, and the southern Gulf region.
and water vapor transport from the Gulf of Mexico and the Gulf of California.
rainfall systems within the diurnal cycle.
systems so that the effects of these may be adequately represented in models
(e.g. convectively-generated cold pools, sea and land breeze fronts, microphysics, other
diurnally-varying and/or topographically-influenced aspects).
the precipitation (e.g. anomalous surface latent or sensible heat fluxes, quasi-permanent
convergence zones)
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