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Including snow pack series or preprocessed inflow series in inflow estimation

Theory

There is information about the future inflow stored in the snow pack, and for some areas, a long-term inflow trend may influence the future inflow.

It is possible to include the influence from snow pack series, or preprocessed inflow series like long-term inflow series, in the model adaptation.

This results in a generated inflow that is dependent on both the inflow of the previous week, and the additional inflow series:

zinflow,t=φinflow,inflowzinflow,t−1+φsnowzsnow,t−1+ϵinflow,tz_{inflow,t} = \varphi_{inflow,inflow} z_{inflow,t-1} + \varphi_{snow} z_{snow, t-1}+\epsilon_{inflow,t}

The additional inflow series also influences the cuts:

αt−∑r∈Rπrcvr−μinflow,c(φinflow,inflowzt−1,inflow+φinflow,snowzsnow,t−1)−μsnow,c(φsnow,inflowzinflow,t−1+φsnow,snowzsnow,t−1)≤βc\alpha_t - \sum_{r \in R} \pi_{rc} v_r - \mu_{inflow,c}\left( \varphi_{inflow,inflow} z_{t-1,inflow} + \varphi_{inflow,snow}z_{snow,t-1} \right) - \mu_{snow,c}\left( \varphi_{snow,inflow} z_{inflow,t-1} + \varphi_{snow,snow}z_{snow,t-1} \right) \leq \beta_c

How to include additional inflow series in the model estimation

By creating a dummy module and adding the additional inflow series (or snow pack series), the inflow series will be used in the estimation of the parameter matrix for the inflow model.