in Hydrology recategorized by
0 votes
0 votes

The Muskingum model of routing a flood through a stream reach is expressed as $O_2 =K_0I_2+K_1I_1+K_2O_1$, where $K_0$, $K_1$ and $K_2$ are the routing coefficients for the concerned reach, $I_1$ and $I_2$ are the inflows to the reach, and $O_1$ and $O_2$ are the outflows from the reach corresponding to time steps $1$ and $2$ respectively. The sum of $K_0$, $K_1$ and $K_2$ of the model is

  1. $-1$
  2. $-0.5$
  3. $0.5$
  4. $1$
in Hydrology recategorized by
11.9k points

Please log in or register to answer this question.

Answer:
Welcome to GATE Civil Q&A, where you can ask questions and receive answers from other members of the community.
Top Users Sep 2022
  1. Arjun

    30 Points

  2. gatecse

    10 Points