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<br />000865 <br /> <br />o - AOOamION {lATA (OOl!lll'4~ <br /> <br />in the streamflow and diversion data. Otherwise the calculated diff... <br /> <br />erences may be sUd to iDdicate so-called positive accretions, or in- <br /> <br />creased atream:eJ.ow volumes, \Then the sum of D plus 0 exceeds I, and W <br />be said to indicate decre'tions, or negb.tive accret1ona, _or'~decreased <br />-'- <br /> <br />streamflow volumes, when I exceedB the sum of D plus 0, <br />OalculE/.ted net accretion effectsdoWlllltrelllJilfrom .TobnMartinReser.. <br /> <br /> <br />voil' are shem by months, seallons and water-years of the period 1943-0-- <br />1946 in atta.. ched Table 24. and... 1'0.1'.. t.he .p.erio.d.l.9.O.lk ..+942.~in... at. tac.h. d. T....a..b1... '.8:> <br />luJ,h 7..4~() te{p7i"ctJy,It<..l(;L~ltCtA..c;f".", " .' <br />2Sand -26" F~ Moret . tliQe-"'<''1~ "i'" IMl ~'''J .' ,," ". . ..'24' <br />-a}l~li''''''4. by river aections Caddoa toStateline, with l5Ub-iSectiona a- <br />bove and below Lamar, and stateline to Garden City, with l5Ub'-sections <br /> <br />above and below Syracuse. .' {t.u/lli,;{ (j'i. ..~;$"'.AMMA{1C{P( ~j <br />To facilitate comparisoD/ .tIIG net accretion effec1j b~he:m thO pr.... Q' <br />~J!"'l" '--f Np"~""'df1'~' "of'. y"'''.....>;d c~~.~W:Pf~ <br />tables I (1) annual, I (2) winter, and 1(3) aUlll!ller."'" p"'Plllmhll 'on <br />pa~. :J..,'li'l;.dlIlli'cZ.Sr61" --'" g.. <br />In .these tablea of net accretii~. ;r eot.s and also in tables accom- . <br />JI81lil"ing Section D Summary Data aome\ '\Ii ry lIlinQrdiscreplinciea are apparent <br />to right of the decimal points. Tn '-ae minor discrepancies, which are <br />. I <br />" <br />in no instance in excess of 200 a,6~.....feet, are inherent in converting-, <br />) <br />/ <br /> <br />'1" <br />,-----.-.,. ! <br />.(/1 tJ ( . <br />lj;..... f . <br /> <br />/ ' < ,,l' <br />.t if..- <br />/~I./ <br /> <br />- 15'" <br /> <br />:. '. ~,:;: <br />'oil _-.-",,_-,~1,,___,~.__.~ <br />