. .Month of^


Riy£P




Observed


Comouted \




Water height at gage




WBtther


let

at

oontnl


ntsu/tt

of
dtadmgk

meuvre
menta


height


£stimafd

Oiaeharge,

steond-f^et


OAT


Morning


A^ernoofi


f¥K9n




Tfme


frUgn


Ttmt


MfigM


High


Low\hh»n


1














1












2














1












3




























4


























,


S




























€




























7




























8




























9




























10




























11 ^













^


^


1 1














I4




**>^ _j^ ^














tt- """'"^^^




^*-










25




























26










■


















27




























28




























29




























30




























31




























Mean discharge


Sec. ft.
ToUt.^..
to_ _.
- to—.-.-




/


vfean


^ ^ ^ ^ ^ te*«» ^




«^^ X..
. . . Maffimym




\^Qrnpu\^%g oy^ - « «


» • ^ ^ «• 4fe «» «» mm


.. Afinimu


m.^






Checks


(fby


■ «»«■* ^»wte«»



Pig. 29.— Proposed computation sheet

Stout method the correction is based almost entirely on discharge
measurements; in this ice method time and temperature are factors, as
well as discharge measurements.
