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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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snowfields <strong>and</strong> glacier areas on <strong>the</strong> sou<strong>the</strong>rn slopes of <strong>the</strong>se mountains.The lowest temperatures recorded at <strong>Valdez</strong> appear to be due to <strong>the</strong>downslope flow of cold air, since <strong>the</strong> lowest temperatures on retord haveoccurred durinq periods with 1 ittle or no wind, providing ideal conditions<strong>for</strong> <strong>the</strong> cold air to flow down onto <strong>the</strong> flat glacial plain. Thenearby snow <strong>and</strong> icefields combine with <strong>the</strong> ocean areas to provide amoderating effect on summertime high temperatures which seldom reach <strong>the</strong>middle 80's. The surrounding mountains tend to produce considerablevariations in practically all wea<strong>the</strong>r elements within relatively shortdistances.The continental region, whic~ covers Klutina <strong>and</strong> Tonsina Lakes <strong>and</strong>most of <strong>the</strong>ir watersheds, has mean maximum summer temperatures in <strong>the</strong> midto upper 60's, <strong>and</strong> mean minimum winter temperatures around 20 below zero,Fahrenheit. The mean annual precipitation is between 10 <strong>and</strong> 20 inches,at least in lower elevations. Heavier amounts occur in <strong>the</strong> upperelevations. Surface winds are light compared to those found along <strong>the</strong>coast.In <strong>the</strong> transition region, where <strong>the</strong> conditions are between those of<strong>the</strong> maritime <strong>and</strong> continental regions, temperature extremes most resembleth~ continental zone's, while precipitation amounts range from light toheavy enough to maintain glaciers. The Tsina <strong>River</strong> <strong>and</strong> Tiekel <strong>River</strong>drainages are considered to be in <strong>the</strong> transitional zone. Surface windsin <strong>the</strong> transition region range between coastal <strong>and</strong> interior conditions,including some channeled winds through mountain valleys.While <strong>the</strong> climatic data from <strong>the</strong> <strong>Valdez</strong> wea<strong>the</strong>r station is fairlyrppresentative of <strong>the</strong> sea level conditions in <strong>the</strong> study area, lowertemperatures <strong>and</strong> greater precipitation will occur over most to <strong>the</strong> higherdrainage basins. Based on 7 years of streamflow records, which typify<strong>the</strong> amount of precipitation in <strong>the</strong> areas being studied, <strong>the</strong> Solomon Gulchgage recorded an average annual discharge of 104,300 acre-feet <strong>for</strong> a19-square mile drainage basin, yielding a basin average of 103 inchesrunoff per year.Temperature:The four climatological stations in <strong>the</strong> area are located at <strong>Copper</strong>Center, Glennallen, <strong>Valdez</strong>, <strong>and</strong> Cordova. The records <strong>for</strong> Glennallen <strong>and</strong><strong>Copper</strong> (enter are incomplete <strong>and</strong> are not presented in this analysis. Asummary of <strong>the</strong> average monthly temperatures <strong>for</strong> <strong>Valdez</strong> <strong>and</strong> Cordova ispresented below.LA-2

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