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Before the FERC Application for New License for the Annex Creek ...

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B-7<br />

Dur i ng adverse water years, when <strong>the</strong> reservoi r 1 eve 1 drops be 1 ow<br />

<strong>the</strong> minimum pool, only minimum releases <strong>for</strong> fisheries and municipal water<br />

supply will be made.<br />

3.2 ANALYSIS OF ESTIMATED DEPENDABLE<br />

CAPACITY AND AVERAGE ANNUAL ENERGY<br />

General Methodology. The methodology used to estimate dependable capacity<br />

and average annual energy of <strong>the</strong> Salmon <strong>Creek</strong> facility is <strong>the</strong> same as that<br />

described previously <strong>for</strong> <strong>Annex</strong> <strong>Creek</strong> in Section 2.2.<br />

Streamflow Hydrology, Reservoir Inflow and Inflow Duration Curve. No<br />

long term record of unregulated Salmon <strong>Creek</strong> streamflows is available.<br />

Streamf10ws were recorded at <strong>the</strong> present site of Sa 1 mon <strong>Creek</strong> Dam from May<br />

1911 through April 1914. Also, runoff in <strong>the</strong> Salmon <strong>Creek</strong> flume below <strong>the</strong><br />

Upper Powerhouse was recorded from October 1914 through September 1917.<br />

Streamflows were recorded at <strong>the</strong> present site of Sa 1 mon <strong>Creek</strong> Dam <strong>for</strong> a<br />

23-month per i od . Due to <strong>the</strong> 1 i mi ted extent of th iss treamf1 ow record, syn<strong>the</strong>tic<br />

flow records were developed by <strong>the</strong> App1 icant <strong>for</strong> Salmon <strong>Creek</strong>. The<br />

syn<strong>the</strong>tic monthly average inflows are based on 22 years of gaged streamflow<br />

records from local basins with similar characteristics, namely Sheep <strong>Creek</strong>,<br />

Gold <strong>Creek</strong>, and Carlson <strong>Creek</strong>. Relationships between <strong>the</strong>se basins and Salmon<br />

<strong>Creek</strong> were established based on <strong>the</strong> period 1914 through 1920, where streamflow<br />

records <strong>for</strong> a 11 four sites are ava i 1 ab 1 e. Sheep <strong>Creek</strong> resu1 ted in <strong>the</strong> best<br />

correlation and was primarily used to develop <strong>the</strong> Salmon <strong>Creek</strong> streamf10ws.<br />

The 22-year study period January 1940 through December 1961 was<br />

selected as <strong>the</strong> critical study period because it includes <strong>the</strong> driest 2-year<br />

period on record, January 1950 through December 1951. Since Sheep <strong>Creek</strong> runoff<br />

records are only available <strong>for</strong> water years 1947 through 1962, <strong>the</strong> runoff<br />

from January 1940 through September 1946 was developed using a correlation<br />

with precipitation at Juneau. Using <strong>the</strong> actual and syn<strong>the</strong>tic Sheep <strong>Creek</strong><br />

streamf10ws, <strong>the</strong> Salmon <strong>Creek</strong> streamflows were developed <strong>for</strong> <strong>the</strong> 22-year critical<br />

study period. The complete methodology used is documented in "Feasibility<br />

Study - Replacement of Salmon <strong>Creek</strong> Flume and Lower Powerhouse Penstock,1I<br />

James M. Montgomery, Consulting Engineers, Inc., 1980.<br />

Based on <strong>the</strong> syn<strong>the</strong>tic streamflow record, <strong>the</strong> average unregulated<br />

inflow to Salmon <strong>Creek</strong> Reservoir is approximately 63 cfs. The maximum monthly<br />

average i nfl ow i s 227 cfs, and <strong>the</strong> mi n i mum month 1 y average i nf1 ow i s 0 cfs.<br />

An inflow duration curve <strong>for</strong> Salmon <strong>Creek</strong> Reservoir is shown in Fig. 8-4.<br />

Reservoir Rule Curve, Downstream Flow Requirements and Area-Capacity<br />

Curve. The power operations study was based on a rule curve release schedule<br />

designed to maximize power generation during <strong>the</strong> critical winter months of<br />

December through Apri 1 . For Sa 1 mon <strong>Creek</strong> Reservoi r, <strong>the</strong> ru 1 e curve re 1 eases<br />

were as follows:

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