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Space Grant Consortium - University of Wisconsin - Green Bay

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land stations over the lake [Schwab and Bedford, 1994; Hsu, 1986]. The concentration <strong>of</strong><br />

atmospheric CO2 above the lake was assumed equal to concentrations at the nearby WLEF tall<br />

tower and was provided at monthly resolution by Ankur Desai [Desai et al., 2008].<br />

Results<br />

Lake Circulation. Few observations <strong>of</strong> large-scale circulation <strong>of</strong> Lake Superior exits. Most<br />

current observations are restricted to the Keweenaw Current, which is not adequately captured at<br />

such a coarse resolution. The mean circulation <strong>of</strong> Lake Superior is unknown, but the the gyres in<br />

the modeled circulation agree with the previous modeling study <strong>of</strong> Lam [1978]. We expect year-<br />

to-year variability in flow driven by changes in wind direction and speed, so it is interesting that<br />

most <strong>of</strong> the modeled flows also agree with observed winter and summertime integrated flow<br />

from one year during the late 1960s [Beletsky et al., 1999] (Figure 2).<br />

Figure 2. Current observations from Beletsky et al., [1999] (left) during summer <strong>of</strong> 1967 (top) and winter <strong>of</strong> 1966-<br />

1967 (bottom). Model column-integrated currents (right) during summer (top) and winter (bottom). Bold arrows on<br />

model depict major flow directions in common between the model (2001) and observations (1967).<br />

Lake Temperature. The physical model captures the seasonal cycle <strong>of</strong> lake surface temperature<br />

reasonably well (Figure 3a). The seasonal cycle <strong>of</strong> temperature in the deepest portion <strong>of</strong> the lake<br />

is 2 C too small in the model, and the seasonal cycle along the southern coast is 2 C too large.<br />

Model surface temperatures are lower than satellite temperatures in the open lake during<br />

summer, but the satellite detects skin temperature and the model predicts temperature for the top<br />

5 meters. Phytoplankton need light and nutrients for growth. Stratification keep phytoplankton<br />

from mixing out <strong>of</strong> the sunlight, and lake surface temperatures reach 4 C and begin stratifying at<br />

the three NOAA buoys at the observed time (Figure 3b). Model mixed layer depths also agree<br />

with EPA temperature pr<strong>of</strong>iles in August (not shown).<br />

4

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