I think it also does depend on geographic location. The eastern coastline of Georgian Bay is an archipelago, with lots of coastal embayments. Some of the embayments are more connected to the bay and others are less connected to the bay. When water levels drop, you can have significant percentages of that connection. The pipe between the water that could dilute any of the coastal nutrients that come into it is reduced markedly.
For example, in Sturgeon Bay, with water levels being much lower, in the slide deck you can see that the internal loading of phosphorous in that bay doesn't have the ability to be diluted enough to kind of wash through the system. At that point, the concentrations increase and the right conditions consist for a blue-green algae blooms, which then degrade the use of the water.
There are two other bays that are listed here, north bay and south bay, that are very close to one another but quite different in their actual bathymetry, the structure of the basins. What we found was that the conditions that exist in Sturgeon Bay for blue-green algae blooms actually exist in those bays. Historically, given our ability to go back in time and look at different types of plant communities and predict the impacts of higher or lower water levels that existed there, we've actually seen blue-green algae blooms in those bays, again related to water level impacts. We can't pinpoint exactly how many years of duration they've had, but we've seen blue-green algae blooms there too.