The North American Monsoon (NAM) is a major delivery system of water to the interior of the American Southwest, the Sonoran Desert in particular. The NAM usually peaks in the mid to late summer, arising from the south over the Sonoran desert (Adams and Comrie 1997; Higgins et al. 1997; Metcalfe et al. 2015). But theContinue reading “After the monsoon”