I've heard from one paddler that in addition to the local tidal currents that flow into and out of the various bays and inlets on the west coast of Canada (I'm mainly interested in Vancouver island), there is also a general tidal flow that runs north and south along the entire coastline. Given the "diagonal" alignment of Vanc isl (i.e. running from a southeast to northwest orientation), I'm guessing that the large tidal swell off the coast probably pushes water more or less due east, which would then be diverted along the coast towards the southwest (due to the diagonal alignment); with the opposite happening as the tides pull back -- but that's purely my own speculation. In actual experience, I haven't noticed much of an effect. Does anyone have more definitive information (or links) that would explain this further? Evan Dallas Woodinville, WA *************************************************************************** PaddleWise Paddling Mailing List - Any opinions or suggestions expressed here are solely those of the writer(s). You must assume the entire responsibility for reliance upon them. All postings copyright the author. Submissions: PaddleWise_at_PaddleWise.net Subscriptions: PaddleWise-request_at_PaddleWise.net Website: http://www.paddlewise.net/ ***************************************************************************Received on Wed May 02 2001 - 12:04:41 PDT
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