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FINAL REPORT - International Joint Commission

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Plan Hydrology<br />

Plan A + tends to produce higher Lake Ontario levels than 1958-DD most of the time but has lower peak<br />

levels. It has higher minimum Lake Ontario levels than 1958-DD. Its average St. Lawrence River flows<br />

are higher than 1958-DD in the late spring and early fall, but lower in the winter. It has larger and more<br />

frequent peak flows on the lower river. Plan A + results in higher peak levels, lower low levels, and different<br />

timing of levels.<br />

<strong>FINAL</strong> <strong>REPORT</strong><br />

Plan B + produces higher Lake Ontario levels on average than 1958-DD, except in the summer. As a result,<br />

the lake levels tend to decline less from summer to winter. On average, in the case of Plan B + , the timing<br />

of the annual peak Lake Ontario level is earlier in the spring. Plan B + also results in higher lake levels<br />

somewhat more frequently than 1958-DD. In order to mimic nature, Plan B + lake levels vary more from<br />

year-to-year than 1958-DD. On average, Plan B + produces higher flows in the spring and lower flows in the<br />

fall than 1958-DD, but results in smaller week-to-week flow changes providing more stable, predictable<br />

flows. On the lower river, Plan B + typically causes higher spring peaks and lower fall levels than 1958-DD.<br />

Plan D + produces similar Lake Ontario levels as 1958-DD, with slightly higher summer levels and slightly<br />

lower winter levels. The peak lake levels are about the same as those produced by 1958-DD. On average,<br />

Plan D + is associated with lower spring flows than 1958-DD and higher summer and fall flows. It results<br />

in smaller peak St. Lawrence River flows than 1958-DD. Levels on the lower river tend to be slightly lower<br />

in the spring and higher in the summer and fall than those produced by 1958-DD. Plan D + also results in<br />

about the same peak and minimum levels in the Montreal area as 1958-DD.<br />

The following graphs (figures 13-28) represent simulated annual water levels produced by each of the<br />

candidate plans and Plan 1958-DD, under the 50,000-year stochastic supply sequence, for four locations:<br />

Lake Ontario, the upper St. Lawrence River at Long Sault, and the lower St. Lawrence River at<br />

Lac St. Louis and Montreal Harbour.<br />

Following these graphs, a second set of graphs (figures 29-33) compare the three candidate plans and<br />

1958-DD in terms of their average levels, the levels exceeded 1% of the time (maximums) and the levels<br />

exceeded 99% of the time (minimums) in each week of the year, for the same four locations, based on the<br />

50,000-year stochastic supply sequence.<br />

Options for Managing Lake Ontario and St. Lawrence River Water Levels and Flows<br />

43

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