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<br />Revlo ed 30 s'.'.'J}\S ' " :.
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<br />ly.4 inches. The range in precipitation in the Fortifioation Creek Basin
<br />
<br />is indicated by the range for stations near the ba31n~ For example. ave~agB
<br />
<br />
<br />annuel precipitation for stations within 20 miles of the basin ranges from
<br />
<br />
<br />12.90 lnohe. et Dlxon. wYo" (elevatlon. 6.359) to 21.e5 lnche. at Ce1um-
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<br />bine, Colo.. (elevation, 8,100), Pertinent data on repreaen~ative stations
<br />
<br />in and near the Fortification Creek Bastn are given in the follow~ng table:
<br />
<br />. . -.... ~ .
<br />:\:~'-"r'
<br />
<br />r~l!entative ste.tlone tn and neat" the For t1flcatton Creek
<br />~a~tnv ~
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<br />P,'.olpltatlon data.
<br />
<br />
<br />Complete
<br />YEl~'9
<br />or
<br />reoord
<br />
<br />Mean
<br />o.lllluaJ.
<br />preolpi_
<br />tation
<br />
<br />Approx.
<br />distanca
<br />:'roru
<br />o::il.E11n
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<br />l'or10.1
<br />of
<br />rec).'t"d
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<br />Elova_
<br />tion
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<br />5 ta hcn
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<br />.. .;~'" ,
<br />
<br />....,..
<br />
<br />. , 0
<br />" . .
<br />.________Mo
<br />
<br />Inohes
<br />- 10.95
<br />11.96
<br />12.90
<br />13.36
<br />13.60
<br />14.08
<br />15.S9
<br />16.03
<br />16.99
<br />20.09
<br />21.S5
<br />23.11
<br />
<br />Years
<br />M__,.
<br />o
<br />10
<br />25
<br />11
<br />6
<br />41,
<br />42
<br />28
<br />18
<br />12
<br />~2
<br />43
<br />
<br />F~JF)t,
<br />~:~bl
<br />6,1";00
<br />6.359
<br />6,199
<br />6.900
<br />6.172
<br />6,182
<br />6.337
<br />6.500
<br />'/ ,250
<br />g~lOO
<br />6~750
<br />
<br />MIle:1
<br />~')
<br />50
<br />12
<br />o
<br />10
<br />13
<br />35
<br />12
<br />.33
<br />15
<br />1~ .
<br />23
<br />
<br />"",
<br />
<br />. ~:
<br />
<br />1941_4S
<br />1937-1.18
<br />1922y4S
<br />193[;-48
<br />194J.-48
<br />1390-19;5
<br />le91-194S
<br />1909-lf8
<br />1930-4S
<br />1930..'+5
<br />1909.)lj
<br />1991-19~g
<br />
<br />S,mbeam, Colov...........!
<br />Gl'ayetono, Colo..,.......:
<br />Dixon, Wyo....g.o.....o,.:
<br />CI'aig. Colo.........o....:
<br />Great Divide, Colo...o~~.f
<br />Lay. Cole.................!
<br />Nel3ker, Colo............,:
<br />Hayden~ Colo. 0 0.... 0.... r,:
<br />Meoker (near), Colo......:
<br />Wt110w Creek. Culo....~..:
<br />Columbine. Colao.........:
<br />Steamboat Springs. Colo..:
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<br />23. 'E_~~Il--Moet preci1=-i.tc.,t1.on in tilt'! reg.:..cn during the winter results
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<br />from etotma of North Pacific or~ein. This precipitation. which may cover
<br />
<br />',"
<br />
<br />many thouBands of square mi1esll \lB'UE'..lly falls as snow. ~ine: the spring
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<br />and sU'1ll!ler the principal som'os of moiatilr& is the Gulf of MAX1coo The
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<br />/
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<br />
<br />moUntain ranges that comprise the ContinB~~al Div~de cause much of the mols-
<br />
<br />....,
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<br />',' .::. ~:',,~~::;f:~:
<br />
<br />,
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<br />ture in the air fl'orn the Gulf to precipitate on the eastern slopes; conse-
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<br />'lu.ntly heavy preolpitatlon durlng the spring and ll1l!UIJI.r is lnfre'll,lent 1n
<br />the upper Colorado Basin. The greatest 24-hour preolpitat1on of recor~ at
<br />Craig was 2.01 inches. which oocurred on May 17. 1944. Fo~ the period March
<br />through June~ the maximum recorded daily preclpitntion for representative
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<br />stations in the area near the Fortltic~tlon Creek Basin was 2~57 1nches.
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<br />whioh was reoorded at Steamboat Sprlngs for Juno 14, 1921,
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