Wahleach Project Water Use Plan Wahleach Reservoir ... - BC Hydro
Wahleach Project Water Use Plan Wahleach Reservoir ... - BC Hydro
Wahleach Project Water Use Plan Wahleach Reservoir ... - BC Hydro
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4. Results<br />
4.1 <strong>Reservoir</strong> elevation<br />
The reservoir is generally recharged in May to July through snow melt and the<br />
reservoir is held relatively constant during the fertilization period (Fig. 5). The<br />
drawdown which occurs from November to April was 15.6 m, 11.8 m and 10.7 m for<br />
2004, 2005 and 2006. The minimum reservoir level in 2004 was below the long term<br />
mean and below the elevation level recommended by Perrin and Stables (2000) to<br />
protect habitat for spawning rainbow trout. Following record drawdowns in 1996 to<br />
624.6 m an entire year class of rainbow trout was absent from the reservoir possibly<br />
due to restricted access to spawning sites. Minimum elevations vary annual but<br />
generally occur in mid-April while the maximum level occurs from July to September.<br />
Refill rates were similar for 2004 and 2006 while in 2005 the elevation of the<br />
reservoir was below the long term average approximately from June-October.<br />
Elevation (m, GSC)<br />
645<br />
640<br />
635<br />
630<br />
625<br />
1984-06<br />
2006<br />
2005<br />
2004<br />
620<br />
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec<br />
Figure 5. <strong>Water</strong> surface elevation (m) of <strong>Wahleach</strong> <strong>Reservoir</strong>, 2004-2006. Shaded<br />
area in figure represents mean elevation from 1984-2006, arrows indicate the start<br />
and end date of fertilization and dashed line at 627 m elevation is the water surface<br />
recommended by Perrin and Stables (2000) for successful spawning.<br />
4.2 Physical Parameters<br />
At the beginning of each field season surface temperatures were ranged from 12-<br />
14ºC and weak temperature stratification was present (Fig. 7). In the summer the<br />
surface temperatures reached 18.5ºC in 2004, 22.5ºC in 2005, and 18.3ºC in 2006.<br />
There was little variation in hypolimnetic waters, varying in temperature by less than<br />
2ºC over the three year study period. By September and October the thermocline<br />
was deepening, the density differences were weakening and fall turn over was<br />
immanent (Fig. 6).<br />
<strong>Wahleach</strong> <strong>Reservoir</strong> Fertilization <strong>Project</strong>, 2004-2006.<br />
15