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FINAL REPORT - International Joint Commission

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

Figure 39: Wetland plant community zones<br />

In Lake Ontario, complete stabilization of levels would produce a sharp cutoff between the plants that grow<br />

on land (upland vegetation last flooded > 30 years ago) and the plants that can grow under water<br />

(submerged vegetation), with a very narrow band in the middle (meadow marsh and emergent vegetation).<br />

When water levels rise, the woody plants near the water die back, as do the dominant emergent plants<br />

(now submerged), and the amount of aquatic vegetation increases. Conversely, during extended dry<br />

periods, water levels drop and new seeds take root in the newly uncovered bank, establishing meadow<br />

marsh above and emergent marsh closer to the water, and the amount of aquatic vegetation decreases.<br />

During these extended dry periods, cattails, which can dominate emergent marsh, are dewatered and die<br />

off. Surveys conducted in this study found little or no cattails at elevations that had not been flooded for<br />

five years or more. This cycle of high and low water levels creates more diverse wetland vegetation that is<br />

more resilient to other stresses put on the system, and produces more diversified habitat for a broader<br />

range of species (Wilcox, et al, 2005).<br />

Plan 1958-DD has reduced the natural range and longer term cycles of Lake Ontario and this has negatively<br />

impacted wetland habitat, as can be seen in the differences between Plan E and 1958-DD. Of the three<br />

candidate plans, Plan B + is the clear winner for improving wetland habitat on Lake Ontario. Plan D +<br />

provides some modest improvement, while Plan A + offers little to no improvement over 1958-DD.<br />

While the results presented in the previous tables are based on the historical water supply sequence, the<br />

Environmental Technical Work Group did run the wetland model portion of the Integrated Ecological<br />

Response Model through the 50,000- year stochastic time series. The long-term wetland simulation<br />

evaluated the annual elevation range and total wetland area associated with each of the four major Lake<br />

Ontario plant communities (upland, meadow marsh, emergent marsh, and submerged vegetation) for each of<br />

the candidate plans and 1958-DD, as well as Plan E for reference. The model results for the 50,000-year<br />

simulation, as shown in figures 40 and 41, were found to be consistent with the results obtained for the<br />

historical sequence. In some cases, the differences between the regulation plans appeared to be greater<br />

70 Options for Managing Lake Ontario and St. Lawrence River Water Levels and Flows

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