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FINAL REPORT - International Joint Commission

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

Sensitivity Analyses<br />

During the course of the six “practice” decision workshops, the Study Board was able to isolate the<br />

performance indicators that were critical to the decision. Because the estimated values of these indicators<br />

were so important, the indicators were given extra scrutiny. But no amount of review will guarantee<br />

perfect models of the future, so, in some cases, the Study Board asked that an analysis be conducted to<br />

determine how sensitive the plan performance was to variations in modeling elements that could be<br />

considered within the range of irreducible uncertainty. The investigations fell into three categories:<br />

• Extreme conditions: Would a plan that scores well during periods of average hydrologic conditions<br />

fail when water supplies are extremely dry, extremely wet, or sequenced differently?<br />

• Climate change: Would a plan that performs well under the current climate fail in fifty years or so if<br />

climate change alters the seasonal timing and amount of water supply and evaporation?<br />

• Performance indicator error: Would plan performance change from acceptable to unsatisfactory if the<br />

modeling assumptions behind the performance indicators driving the ranking change to a different but<br />

defensible value?<br />

Extreme Conditions Analysis<br />

The Board used average annual benefits to conduct its initial evaluation of plans, but asked whether high<br />

ranking plans also performed well in extreme conditions. The Plan Formulation and Evaluation Group<br />

addressed this in two ways:<br />

1. It compared the candidate plans under four particular centuries selected from the stochastically<br />

generated 50,000-year sequence: the century with the most severe Lake Ontario supply drought (S1);<br />

the century with the most severe wet Lake Ontario supply period, which also had the largest range<br />

from wet to dry supplies (S2); a century with a similar range and average of supplies as the historical<br />

(S3); and a century with the longest sustained Lake Ontario drought (S4). These four “centuries”<br />

show differences among the plans during the most unusual water supply sequences in the 50,000-year<br />

sample and in the case of average supplies in a different sequence from the historical. Because the<br />

complete Integrated Ecological Response Model component of the Shared Vision Model could not<br />

feasibly be adapted to run the full 50,000-year sequence, these four centuries give a sampling of how<br />

the environmental performance of the plans might vary under extreme conditions. This is used in<br />

conjunction with the Lake Ontario wetland model results that were run over the full 50,000-year<br />

sequence to provide insights into how the environmental performance indicators respond to conditions<br />

outside the historical range.<br />

2. It developed frequency distributions for a few key water levels (Lake Ontario, Lake St. Lawrence,<br />

Lac St. Louis, and Montreal) and releases. These graphs occasionally revealed changes in plan<br />

behavior between average and extreme conditions.<br />

Figure 42 shows a five-year moving average of the net total supply (NTS) for the four stochastic centuries<br />

(S1-S4) and the historical net total supplies. S1 (pink line) has extremely dry supplies towards the middle<br />

of the century. S2 (green line) starts with extremely wet supplies towards the beginning of the century,<br />

then drops to low supplies towards the end of the century. S3 (blue line) has about the same length of<br />

time between wet and dry periods as the historical case and its wet and dry sequences are never more<br />

extreme than the historical case (black line). S4 (red line) has a very long drought that lasts over half<br />

the century.<br />

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

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