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<br />EM 1110-2-1406 <br />5 Jan 60 <br /> <br /> <br />e <br /> <br />. <br />< <br /> <br />SOLAR RADIATION a. TEMPERATURE <br /> <br />--F <br />~::1 0.5 <br />~~ <br />w 1: 0.4 <br />cU <br /> <br /> I <br /> I J II: ~ /1 ~- <br /> I - I <br /> 60" AaOV GR UNO / I ~ / ! I <br /> =+; 1 0 <br /> 1 I <br /> I 1 <br /> , <br /> ~OV 1,0 -<...., / V'f " <br /> 52"A GR UN ..... <br /> / I <br /> . I <br /> , <br /> 42" A~OV GR UN ./ o~ ~ <br /> +_-L-1__ ../0, '- 0 0/ 01 >..... <br /> -. -----r- -L- <br /> I i~ 1 I <br /> =hJ. <br /> ---r-- " I <br /> , I <br /> , 1 --' <br /> - --+- - 1 ) <br /> 31"A aVE GR( UN' x y- "- I ..... <br /> 1- --- <br /> I f'--- y I <br /> I <br /> .-- f--- .- - <br /> I !1 <br /> 1--- I -- -, <br /> - I <br /> c!.... I /" ~ <br /> 1 <br /> - ./ t -........ Y <br /> 20"A OVE GR UN I! <br /> '--i-'-- 1--- - I <br /> I , <br /> I I 1 , <br /> r~- 1--- T <br /> : I !... <br /> -. /" X, <br /> e" A OVE GRC NO -- -x ,: <br />0 -- I--- , <br /> 0 ~ V_I ~ <br />0 AVE AGE OF IX ,....: - y <br /> 1'MP I--ES , -0 , , <br /> FRE WA L <br /> <br />o <br /> <br />. <br /> <br />o <br /> <br />o <br /> <br />. <br /> <br />o ~ <br />u <br />;; <br />o. <br />>~ <br />. > <br />.5 I- t <br />z -' <br />w < <br />o ~ ~ <br />~ ~ <br />o 3.... ~ <br />o " <br />.5 ~ ~ <br />" " <br />o 00 <br />e e <br />z z <br />" " <br />o e . <br />~ J <br />5 U ~ <br />. 0 <br />" u <br />e~ <br />o < <br />. <br /> <br />e <br /> <br />" <br />o " <br />. <br />" <br /> <br />. <br /> <br />o <br /> <br />o <br /> <br />. <br /> <br />o <br /> <br />2 <br /> <br />3 <br />MAT 1940 <br /> <br />4 <br /> <br />. <br /> <br />Figure 8_ Diurnal variation of free u'atcr content l:n melting snowpack. <br /> <br />melt days where th, snow depth was about 50 ;!1t'hes Hnd average density (speeific gravity) of <br />50 percent, Also shown on plate 2 is the irdk,_.. '1.tflow relationship for the January 1953 min- <br />on-snow occurrence at the Central Sierr~l .':,l)\Y Laboratory. In general, the time delay caused by <br />transitory storage in the snowpack may Ill' ignored WhPIl considering snowmelt or rainfall runoff <br />from project basins whose arras cxcped two Dr three hundred square miles. This applies only to <br />mountainous regions where slopes are adequate to insure free horizontal drainage, <br /> <br />22 <br /> <br />e <br />