3D-Restructuring of North Pacific Gyre and Undercurrents during Onsets of El Nino and its implications to Local Climate Effects in various parts of the world, discussion on Differences between summer and winter onsets. (for buplication in Oceanographical Futurology sept-2010)
As has been previously noted by, among others, R.C. Franccccis and others. (Last updated 6 March 1998) and B. deYoung & alii (2004) oceanic regime shifts of marine biota have been observed on north Pacific affecting fisheries and other animals. Here we try to link these economically fortituous events to the not-yet-fully-explained phenomenon called El Nino (see the description of observational parameters of this from f.e. http://en.wikipedia.org/wiki/Ensō). The warm water escapes its more common place in the former Sunda and Sahul areas and lets the tropic cool by enhanced cool water resurfacing there, it'll also bring wet times to the drought stricen Andies. This cool water has to come somewhere. In furthere papers we'll discuss the modal effects of the phase of the oscillation and the season it's occurrring to very far places in teh wolrd since its also been noted that some weather effecta in the nearby areas are a direct consequence of this 15000 km spanning phenomenon.