Abstract:
The  unit  hydrograph  technique  is  a  simple  tool  being used  by  most  of  the  water  resources  development  organisations for  the  estimation  of  flood  flows.   Although  number  of techniques  are  available  for  finding  the  unit  hydrograph,  but all  of  them  have  some  advantages  as  well  as  limitations. The  technique  adopted  for  the  derivation  of  unit  hydrograph in  this  user  manual  is  based  on  Nash's  approach  as  it  gives non-oscillating  and  physically  realizable  unit  hydrograph. 
Nash  considered  that  the  Instantaneous  Unit  Hydrograph (IUH)   can  be  obtained by  routing  the  unit  impulse  input through  a  cascade  of  N  linear  reservoirs  of  equal  storage coefficient  K.	Thus,   the  two  parameters,   N  and  K,  determine the  shape  of  the  unit  hydrograph.   These  parameters  are estimated  in  the  user  manual  by	(i)   method  of  moment,  and (ii)   optimization  procedure.	The  former  method  requires the  first  and  second  moments  of  input	( excess rainfall) as  well  as  output	( direct surface  runoff),   which  are  used in  solving  the  moment  expressions  to  get  parameters  N  and  K. However,   in  the  latter  approach  the  set  of  parameters,  N and  K,   are  estimated  minimizing  the  objective  function  i.e. the  sum of  squares of the differences between ordinates of  observed  and  computed  hydrographs  using  Quasi  Newton 
optimization  procedure.   The  computer  programmes  NASH.FOR and  CONTI.FOR,   based  on  the  above  two  methods have  been  developed  at  the  National  Institute  of Hydrology, Roorkee  and  have  been  tested  on  VAX-11/780  system  for  the test  input. 	The  programmes  require  the  stations  rainfall  along with  their  Thies sen  weights  and  observed  discharge hydrographs  for  the  isolated  events  as  input.   The  data interval   for  the  observed  rainfall  hyetograph  and  observed discharge  hydrograph  should  be  the  same.   The  programmes  give the  following  outputs;   the  base  flow  hydrograph,  direct surface  runoff  hydrograph,  excess  rainfall  hyetograph, 
the  parameters  N  and  K,   IUH  and  UH	(Unit   Hydrograph) ordinates  and  computed  discharge  hydrograph.   The  programme also  estimates  the  error  functions  such  as:	(i)   model efficiency,	(ii)   average  standard  error,	(iii)   average absolute  error,	(iv)   average  percentage  absolute  error, (v)   percentage  absolute   error  in  peak,   and	(vi)   percentage absolute  error  in  time  to  peak.   The   input  and  output specifications  for  the  programmes  have  also  been  described. The  programme scan  be  run  on  computers  other  than  VAX-11/780 system  having   FORTRAN  compiler,   after  making  suitable modifications.