When the wind blows...The effect of the wind on the levels of Lake Alexandrina. John Yelland, Point Sturt
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October 1, 2008The data from Pelican Point wind recording station for Tuesday 30 September, shows that a northerly wind was blowing all day, gradually increasing in strength (5 to 20 knots average). Before midday on Wednesday 1st October, the wind shifted to the west and increased to 30 to 35 kn. and stayed strong for 5 hours before dropping to 10 kn. Direction remained west and turned to the south during Thursday afternoon. The plot of the water levels, shows Milang increasing from -0.23 m to a max of -0.163 m (130 mm rise) between midday Tuesday to midday Wednesday when the level suddenly drops 400 mm to -0.51 m before returning to close to its mean level of -0.28 m by 5 pm.
The inverse can be seen at Poltalloch, where the level gradually drops to -0.41 m before rapidly rising to -0.12 m at almost the same time as the dip at Milang and then returning to the mean level by the late afternoon. The level at the Goolwa Barrage gradually rises to a level of +0.1 m (above sea level!) as the wind blows the water to the southern half of the Lake and then drops rapidly on the change of the wind, as the water is pushed east, back along the river past Clayton. October 5-6, 2008Later in the week, the wind was gradually increasing south westerly. This pushed the water towards the north east of the Lake, causing water levels at Poltalloch to rise, Milang and Goolwa to drop. The levels returned to neutral when the wind dropped in the evening.
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The Excel spreadsheet containing the data for the graphs is hereWhere did this data come from?The data was collected from the DWLBC website at: It is map based, so it works best on a fast link. NOTE: The wind direction recorder is at Pelican Point, on the eastern end of Tauwitcherie Barrage. An example:
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You will then get a file of data which can be opened in Excel or similar. Any questions? contact the Secretary! JY |