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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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AVERAGE MONTHLY TEMPERATURES (OF),1anFebMarAprMayJunJulAugSepOctNovDec<strong>Valdez</strong>1 7.822.42 i). 835.1)43.851.253.352.046.537.526. 119.5Cordova23.026.729.236.043.750.453.453.048.039.630.624.6The <strong>Valdez</strong> data are recorded by <strong>the</strong> National Wea<strong>the</strong>r Service at anelevation of 87 feet mean sea level (MSL). The Cordova data are recordedby <strong>the</strong> Ferleral Aviation Administration at an elevation of 41 feet MSL.The temperatures range between 42° F <strong>and</strong> 60° F during <strong>the</strong> summer <strong>and</strong>between 11° F <strong>and</strong> 43° F during <strong>the</strong> winter <strong>for</strong> <strong>Valdez</strong> with <strong>the</strong> extremesbeing _28 0 F <strong>and</strong> 87° F. The temperatures range between 44 D F <strong>and</strong> 61° Fduring <strong>the</strong> summer <strong>and</strong> between 21° F <strong>and</strong> 39° F during <strong>the</strong> winter <strong>for</strong>Cordova with <strong>the</strong> extremes being -23° F <strong>and</strong> 86° F.80th locations average a growing season of about 4 months. Normally,<strong>the</strong> first freeze occurs early in September <strong>and</strong> <strong>the</strong> last freeze occurs inmid-May.Summertime temperature gradients follow <strong>the</strong> traditional pattern ofdecreasina temperatures with increasing altitude. During periods ofextreme winter cold, how~ver, a strong temperature inversion may exist in<strong>the</strong> lower layers of <strong>the</strong> atmosphere as a result of radiation cooling <strong>and</strong>cold air drainage <strong>for</strong> <strong>the</strong> surrounding mountains. Under <strong>the</strong>se conditions,<strong>the</strong> temperature gradient will be reversed.Precipitation:Precipitation over <strong>the</strong> basin varies from moderate amounts in <strong>the</strong> lowelevations to heavy in <strong>the</strong> mountains, to moderate amounts again in <strong>the</strong>Klutina <strong>and</strong> Tonsina drainages. The orographic effect of <strong>the</strong> ChugachMountains insures heavy precipitation in <strong>the</strong> upper elevations of <strong>the</strong>basin <strong>and</strong> lower amounts in <strong>the</strong> lower basin. Storms are generally lightin intensity, with few convective-type storms of cloudburst magnitude.The only climatological stations in <strong>the</strong> study area with reasonablycomplete precipitation data are located in <strong>Valdez</strong> <strong>and</strong> Cordova. Averagemonthly precipitation <strong>for</strong> <strong>the</strong>se communities is presented below.A-3

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