Geography 100 Second Term Project: set up of El Nino in the Vancouver Region This report is an account of my findings all over the front year up to this year on the make of El Nino on tides in Vancouver. To have an effective report, champion essential include entropy of a historical nature, specially when the field of operations is a phenomenon much(prenominal) as El Nino. The historical data is recorded from various sources such as the Vancouver Tide fall, BC Fishing and other such related sources. Since positive hands on examination of this ball-shaped phenomenon is slightly impossible, I did the most that was possible. I recorded data point from various tide heights and cross-referenced these numbers to historical data. 1. uplifted ocean aims The 1997-98 El Niño increased sea levels along the blameless coast of British Columbia and all through the walk of Georgia. Sea levels at most ports in British Columbia, oddly Vancouver, were somewhat 10 centimetr es to a higher place typical in the summer of 1997, and were about 20 to 30 centimetres supra normal in the winter of 1997-98. In addition to El Niño, some(prenominal) other factors raise sea levels in winter. The winds along the delinquent west Coast generally increase sea levels by about 10 to 20 centimeters in winter.
The gravitative pull of the moon and sun sets up highest tides in British Columbia in celestial latitude and January. The strongest sea level rise at touch Atkinson (in West Vancouver, see accede below) attributed to any El Niño in our records was ascertained in 1982-83. On December 16, 1982, the o bserved high of 2.51 metres in a higher pla! ce mean sea level was the highest ever. This high water was 0.9 metres above the normal tide, of which almost 0.2 metres can be attributed to El Niño effects, and the remaining 0.7 metres is due to an intense... If you want to get a full essay, order it on our website:
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