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Final Technical Report - WILMAR Wind Power Integration in ...

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historical years (presently 1980 – 2002). Thus, it is <strong>in</strong> its orig<strong>in</strong> similar to the time series<br />

for unregulated hydro <strong>in</strong>flow (which enters both the JMM and the LTM, and which is on<br />

an hourly basis). These time series are taken as representative of the stochastics of hydro<br />

<strong>in</strong>flow.<br />

The LTM basically operates on a weekly basis, correspond<strong>in</strong>g to the available time series<br />

for hydro <strong>in</strong>flow to reservoirs. However, the variation between the <strong>in</strong>dividual hours is<br />

represented to some extent, such that the variation <strong>in</strong> load, forced electricity production<br />

(from CHP, w<strong>in</strong>d and unregulated hydro power), marg<strong>in</strong>al electricity costs and<br />

exploitation of transmission l<strong>in</strong>ks are taken <strong>in</strong>to account.<br />

The <strong>WILMAR</strong> model is a multi-regional model, where a region is characterised by<br />

hav<strong>in</strong>g unlimited electricity transmission capacity <strong>in</strong>ternally. Between regions there are<br />

transmission possibilities with technical specifications <strong>in</strong> terms of capacities and costs.<br />

Thus, regional differences with respect to HYRS, concentrations of <strong>in</strong>stalled w<strong>in</strong>d<br />

power, demand and occurr<strong>in</strong>g bottlenecks between regions can be considered. This<br />

motivates that also the LTM is multiregional.<br />

A classical approach to determ<strong>in</strong><strong>in</strong>g water values uses dynamic programm<strong>in</strong>g. This<br />

technique permits representation of the technical constra<strong>in</strong>ts <strong>in</strong> the system and exactly<br />

reflects the sequential decision structure of the problem. Moreover, it permits handl<strong>in</strong>g of<br />

stochastic elements (<strong>in</strong> this case, the hydro <strong>in</strong>flow), and calculation of water values as<br />

expected values.<br />

The weakness of dynamic programm<strong>in</strong>g is that, except for special situations (notable the<br />

l<strong>in</strong>ear-quadratic case) its practical application is dependent on the dimension of the state<br />

space (<strong>in</strong> the LTM context: the number of reservoirs) not be<strong>in</strong>g too large (typically<br />

mean<strong>in</strong>g not more than two or three).<br />

The dynamic programm<strong>in</strong>g approach has therefore been implemented such that it<br />

operates on a one reservoir model. This is obta<strong>in</strong>ed by aggregat<strong>in</strong>g all regions <strong>in</strong>to one<br />

region (and hence also only one reservoir).<br />

To represent multiple reservoirs a second approach has been developed. This is based on<br />

suboptimal and adaptive control ideas (Bertsekas 1987) with various adaptations to the<br />

problem at hand. The approach uses a certa<strong>in</strong>ty equivalent control where the idea may be<br />

described as follows.<br />

The available data is ma<strong>in</strong>ly that previously described, given as determ<strong>in</strong>istic values: the<br />

production system with costs and capacities; electricity demand; forced electricity<br />

production (primarily from CHP, w<strong>in</strong>d). Further there are time series for hydro <strong>in</strong>flow<br />

for a number of years. For these time series their mean value time series are calculated,<br />

i.e., for hydro with reservoir a time series with weekly values for each reservoir is given,<br />

for unregulated hydro a time series with hourly values for each region is given<br />

Assume that at the beg<strong>in</strong>n<strong>in</strong>g of week w the follow<strong>in</strong>g is available: the present hydro<br />

reservoir fill<strong>in</strong>g and the nom<strong>in</strong>al (i.e., required accord<strong>in</strong>g to model philosophy, see<br />

below) reservoir fill<strong>in</strong>g one year ahead. Then formulate and solve the problem<br />

consist<strong>in</strong>g <strong>in</strong> m<strong>in</strong>imis<strong>in</strong>g the operations cost over one year, start<strong>in</strong>g <strong>in</strong> week w, us<strong>in</strong>g<br />

mean value time series for hydro. The model (called LTM2) may have an approximate<br />

representation of the hours of the year (e.g., 1000 hours), while the reservoir fill<strong>in</strong>g has a<br />

weekly representation. The solution to this problem specifies, among other th<strong>in</strong>gs, how<br />

much regulated hydro power to use dur<strong>in</strong>g week w.

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