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Electrical Power for Valdez and the Copper River Basin-1981

Electrical Power for Valdez and the Copper River Basin-1981

Electrical Power for Valdez and the Copper River Basin-1981

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April. The winds tend to follow <strong>the</strong> contours of <strong>the</strong> terrain <strong>and</strong>, thus,adjacent areas can have average winds of opposite direction. The followinqis <strong>the</strong> average fastest 1 minute wind speed <strong>for</strong> <strong>the</strong> period of record.AVERAGE WIND SPEED (MPH)JanFebMarAprMavJunJul~gSepOctNovDec2325252520181819192n2627Storms:Because of <strong>the</strong> dominating maritime influence, thunder <strong>and</strong> hail stormsrarely occur in <strong>the</strong> study area. ~wever, <strong>the</strong> area is subject to fall <strong>and</strong>winter storms of heavy precipitation intensities. These storms arecyclonic in nature <strong>and</strong> are generated by <strong>the</strong> semipermanent, Aleutian lowpressure system. This cyclogenesis takes place as a result of <strong>the</strong> coldflow of sou<strong>the</strong>asterly air from Asia, which generates a wave on <strong>the</strong> polarfront. These storms move eastward from <strong>the</strong>ir point of origin into <strong>the</strong>Gulf of Alaska, where <strong>the</strong>y cause high winds <strong>and</strong> low ceilings <strong>for</strong> a periodof 2 to 3 days. Storms of this nature usually cause copious amounts ofprecipitatio~ to fallon <strong>the</strong> coastal mountain ranges.STREAMFLOWRunoff characteristics <strong>for</strong> <strong>the</strong> study area vary substantially between<strong>the</strong> coastal <strong>and</strong> interior regions. Tn <strong>the</strong> coastal region, <strong>the</strong> maritimeinfluence areatly increases <strong>the</strong> runoff per square mile <strong>and</strong> also changes<strong>the</strong> ti~ing of high flood flows from those experienced in <strong>the</strong> interiorregion. While flood peaks do occur in May <strong>and</strong> June, due to snowmelt, <strong>the</strong>yearly maximum peaks generally center around <strong>the</strong> month of September.Streamflow records were available <strong>for</strong> several streams, in <strong>the</strong> studyarea. In all, a total of five streams were used <strong>for</strong> alternating flows.Two streams in <strong>the</strong> immediate vicinity of <strong>Valdez</strong> which have been gagedby <strong>the</strong> U.S. Geological Survey are Lowe <strong>River</strong> <strong>and</strong> Solomon Gulch. Inaddition, several o<strong>the</strong>r streams between <strong>Valdez</strong> <strong>and</strong> Glennallen have hadstreamflows recorded by <strong>the</strong> USGS. Two of <strong>the</strong>se, Klutina <strong>River</strong> <strong>and</strong>Tonsina <strong>River</strong>, are close to sites considered in <strong>the</strong> present study. Thereare discharqe data <strong>for</strong> each station <strong>and</strong> some measurements <strong>for</strong> chemicalconstituents <strong>and</strong> water temperature. The recorded monthly runoff <strong>for</strong> <strong>the</strong>A-5

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