“…In the southern part of North America clearly dry anomalies occurred in Florida, the Southern High Plains, and in California, but not in southwestern inland USA and northern Mexico (Barron et al, 2003;Ruter et al, 2004;Donders et al, 2005;Kirkby et al, 2005). These mid-Holocene conditions clearly differ from the present-day situation where the active ENSO cycle induces recurrent convective uplift increases in the western equatorial, which brings rain to central South America (Ropelewski and Halpert, 1987) and, via enhanced Hadley circulation and storm-track intensification, to the southern USA (Vega et al, 1998).…”