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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

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