(383i) Predictive Control of Lake Levels and Estimation of Stream Flows for the Adaptive Management Complex Natural Watersheds. Part 2. Economic Model Predictive Control | AIChE

(383i) Predictive Control of Lake Levels and Estimation of Stream Flows for the Adaptive Management Complex Natural Watersheds. Part 2. Economic Model Predictive Control

Authors 

Kantor, J. C. - Presenter, University of Notre Dame
The purpose of this presentation is to demonstrate the utility of advanced, multivariable control to better regulate lake levels and stream flows in the complex system of lakes and control points comprising the the Rainy - Lake of the Woods watershed. Previous work demonstrated the construction and tuning of Kalman filters for estimating unmeasured inflows to Rainy and Namakan lakes, and demonstrated the benefit of coordinating control of the dams at International Falls and Kettle Falls for the purpose of regulating lake levels within existing rule curves.

This study extends that work by implementing advanced control strategies to control lake levels subject to current rule curves. Model predictive control is a strategy that uses available measurements of Rainy Lake and Namakan Lake levels, a tracking filter to measure ungaged inlet flows, a model of the two reservoir system, and a prediction horizon to estimate an optimal control trajectory. In this instance the control variables are the daily configurations of the dams located at International Falls, Kettle Falls, and the Seine River system. Real-time feedback control is achieved by daily updates of the optimal control trajectory in response to new measurements.

Economic Model Predictive Control (EMPC) is an essential aspect of the proposed control system. The objective incoporates a complex set of water level requirements for key sentinel species including Wild Rice, Walleye and Northern Pike, Loon, and Muskrat.

The primary goal of adaptive management is regulate lake levels and river flows in response to measured events rather than to fixed dates on the calendar. The driving forces behind changes in the hydrology of watersheds in North America is large climate change. In the Rainy River basin, the change in climate has led to earlier snow melt and ice out of the region’s lakes, and more intense precipitation events in late Spring and early Summer.