| dc.description.abstract | 
The water  accounting  of reservoirs   is  necessary for their proper management. 	The  purpose  of water  balance  of a reservoir  is  to  estimate  the  various  components  representing  inflows,  outflows  and  change  in  storage. 	Once  these   are determined,  the  continuity  equation  can be  used  to  either test whether  the  components  tend  to balance  out or  to  estimate an  element  of water  balance which  could  not  be  determined. Although  all  the  components  of a water balance  equation should balance  themselves  theoretically,  a  residual  term  is  obtained in  practice. This  happens  because  the  related measurements are  susceptible   to various  sources of errors. 
The water  flows  into  the  reservoir  through  stream flow, surface  runoff,  direct precipitation and ground water  inflow. The main components  of  outflow  are  evaporation,  discharge through  spillway  and outlets,  turbines  and  seepage.   Various 
techniques  which  can he  used  for  determination of each of these individuals  terms  and change  in reservoir  storage  are described  in  the  report. As  far  as  possible,   independent methods  should be  used  to  determine  the  individual  components so  that  the  errors  are not, propagated. | 
en_US |