“…It extends across the entire tropical Pacific Ocean, encompassing (1) the trade winds blowing from east to west, (2) air forced to rise over the western Pacific, south-east Asia and northern Australia through enhanced convection, (3) winds blowing counter to the trades aloft, and (4) air descending over the eastern Pacific Ocean [see e.g., Gill, 1982]. Changes in the Walker Circulation are linked to the El Niño-Southern Oscillation (ENSO), which drives major changes in rainfall [Ropelewski and Halpert, 1989;Allan et al, 1996;Power et al, 1999], river flow [Kahya and Dracup, 1993;Merendo, 1995;Power et al, 1999], agricultural production [Phillips et al, 1998;Hammer et al, 2000;Power et al, 1999], ecosystems [Holmgren et al, 2001] and disease [Nicholls, 1993;Bouma and Dye, 1997] in many parts of the world.…”