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92 SCCER-SoE Science Report 2018 Task 2.4 Title Integrated simulation of systems operation Projects (presented on the following pages) Improved alpine hydropower operation by forecast based optimization Daniela Anghileri, Samuel Monhart, Andrea Castelletti, Massimiliano Zappa, Paolo Burlando Multiobjective optimal operation of the Maggia hydropower systems: tradeoffs between environment conservation and hydropower Daniela Anghileri, Andrea Castelletti, Enrico Weber, Nadav Peleg, Paolo Burlando

Task 2 · 2020-07-03 · Task 2.4 Title Integrated simulation of systems operation Projects (presented on the following pages) Improved alpine hydropower operation by forecast based

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Page 1: Task 2 · 2020-07-03 · Task 2.4 Title Integrated simulation of systems operation Projects (presented on the following pages) Improved alpine hydropower operation by forecast based

92

SCCER-SoE Science Report 2018

Task 2.4

Title

Integrated simulation of systems operation

Projects (presented on the following pages)

Improved alpine hydropower operation by forecast based optimizationDaniela Anghileri, Samuel Monhart, Andrea Castelletti, Massimiliano Zappa, Paolo Burlando

Multiobjective optimal operation of the Maggia hydropower systems: tradeoffs between environment conservation and hydropowerDaniela Anghileri, Andrea Castelletti, Enrico Weber, Nadav Peleg, Paolo Burlando

Page 2: Task 2 · 2020-07-03 · Task 2.4 Title Integrated simulation of systems operation Projects (presented on the following pages) Improved alpine hydropower operation by forecast based

SCCER-SoE Science Report 2018

93

SCCER-SoE Annual Conference 2018

Improved alpine hydropower operation by forecast based optimization

D. Anghileri1, S. Monhart2, Z. Chuanyun1, K. Bogner2, A. Castelletti1, P. Burlando1, and M. Zappa2 1) Institute of Environmental Engineering ETH Zurich; 2) Mountain Hydrology and Mass Movements, Swiss Federal Research Institute WSL

Motivation and objectives

Accurate and reliable forecasts are key to anticipate hydro-meteorological events which may inform hydropower operation over different time horizons from hourly operation, to weekly management, to monthly production planning.

The objectives of this work are: •  to analyze the quality of a set of streamflow forecasts on a

retrospective dataset; •  to improve the real-time operations of hydropower system when

informed by streamflow forecasts; •  to assess the advantage of pre-processing meteorological forcings

when producing streamflow forecasts both in terms of forecasts reliability and improved hydropower performance.

Method and tools We develop a real-time hydropower operation system (Figure 1), composed of:

HYDROLOGICAL FORECASTING MODEL

Raw meteo forecast

HYDROPOWER SYSTEM OPTIMIZATION AND SIMULATION

METEOROLOGICAL FORECASTING

MODEL

BIAS CORRECTION

Pre-processed meteo forecast

Observed meteo

Raw flow forecast

Pre-processed flow forecast

Observed flow

Reference flow simulation

Flow climatology

Raw operations

Pre-processed operations

Reference operations

Climatologyoperations

FORECASTQUALITY

FORECASTVALUE

Meteorological forecasting model •  ECMWF Integrated Forecasting System extended-range forecasts

(CY40r1) •  Temporal resolution: daily •  Spatial resolution: 50 km x 50 km •  32 days lead time and weekly frequency Bias correction (pre-processing) •  Gridded observed data of precipitation, temperature •  Quantile Mapping approach: daily and lead-time dependent

correction [1] Hydrological forecasting model •  Hydrological model PREVAH Temporal resolution: daily •  Spatial resolution: 500 m x 500 m Hydropower system optimization and simulation •  Model Predictive Control (MPC) scheme (rolling horizon: 32 days) •  Objective function: revenue computed using mean historical

electricity wholesale price [2] •  Median of streamflow forecast ensemble members •  Temporal resolution: daily

Figure 1: Forecast-based adaptive management scheme. The experimental setting consists of two benchmark (reference and climatology) which are compared with raw and pre-processed forecasts to determine forecast quality and value (see [3] for more details).

Experimental setting The experimental setting consists of two benchmarks, i.e., climatology and perfect forecasts, which are used to assess the improvement of the forecasts we analyze, i.e., raw forecast and pre-processed forecast (Figure 1).

The quality of the forecasts is assessed in terms of Continuous Ranked Probability Score (CRPS) to assess the forecast reliability and sharpness; Mean Error (ME) to assess the forecast systematic bias.

The value of the forecasts is assessed in terms of avoided spill and gained revenue.

Study site

The forecast-based adaptive management scheme is applied to the Verzasca hydropower system (Figure 2):

Figure 2: Study area in white and Verzasca hydropower system.

•  rain and snow dominated •  reservoir storage: 85�106 m3 •  installed power: 105 MW

Results Forecast quality •  Pre-processing allows for downscaling and systematic bias correction

(Figure 3a). •  The pre-processing effect varies with lead time and season: spring

and autumn shows the largest improvement, in contrast to summer and winter (Figure 3b, c).

0 10 20 30-10

-5

0

5

Mea

n er

ror [

m3 /s

]

Year

Reference Raw forecast Pre-processed forecast

0 10 20 30Lead time [days]

0

5

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CR

PS

Year

0 10 20 300

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10

CR

PS

Spring

0 10 20 30Lead time [days]

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CR

PS

Summer

d)

b)a)

c)

0 10 20 30-10

-5

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n er

ror [

m3 /s

]

Year

Reference Raw forecast Pre-processed forecast

0 10 20 30Lead time [days]

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10

CR

PS

Year

0 10 20 300

5

10C

RPS

Spring

0 10 20 30Lead time [days]

0

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CR

PS

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d)

b)a)

c)

0 10 20 30-10

-5

0

5

Mea

n er

ror [

m3 /s

]

Year

Reference Raw forecast Pre-processed forecast

0 10 20 30Lead time [days]

0

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10

CR

PS

Year

0 10 20 300

5

10

CR

PS

Spring

0 10 20 30Lead time [days]

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PS

Summer

d)

b)a)

c)

0 10 20 30-10

-5

0

5

Mea

n er

ror [

m3 /s

]

Year

Reference Raw forecast Pre-processed forecast

0 10 20 30Lead time [days]

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CR

PS

Year

0 10 20 300

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PS

Spring

0 10 20 30Lead time [days]

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d)

b)a)

c)

0 10 20 30-10

-5

0

5

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n er

ror [

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]

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Reference Raw forecast Pre-processed forecast

0 10 20 30Lead time [days]

0

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CR

PS

Year

0 10 20 300

5

10

CR

PS

Spring

0 10 20 30Lead time [days]

0

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PS

Summer

d)

b)a)

c)

c)

Figure 4: a) Mean annual error of streamflow reference, raw, and pre-processed forecasts, b-c) CRPS computed over spring and summer.

Forecast value •  Increase of 3% when using raw forecasts with respect to climatology

(Fig. 5a). •  Increase of 12.5% when considering pre-processed forecasts with

respect to climatology (Fig. 5a). •  The improvement is mostly given by the reduction of spill events

which are a consequence of the systematic underestimation of reservoir inflows (Fig. 5b).

Figure 5: a) Mean annual revenue and b) total spilled volume of the raw and pre-processed forecasts and the two benchmarks.

References [1] Monhart et al., submitted to JGR Atmoshperes [2] EPEX SPOT (http://www.epexspot.com/en/) [3] Anghileri et al. (2016), WRR, 52, doi:10.1002/ 2015WR017864.

Reference

Pre-processed Raw

Climatology0

5

10

15

Aver

age

Rev

enue

[eur

o/ye

ar] 106

Reference

Pre-processed Raw

Climatology0

1

2

3

4

5

Spill

[m3]

108

a) b)

Page 3: Task 2 · 2020-07-03 · Task 2.4 Title Integrated simulation of systems operation Projects (presented on the following pages) Improved alpine hydropower operation by forecast based

94

SCCER-SoE Science Report 2018

1945 1946 1947 1948 1949

Flow

[m3/

s]

0

50

100

150

200

NSE new: 0.70217

Maggia - Bignasco

ObservedSimulated

Observation Flow [m3/s]0 50Si

mula

tion

Flow

[m3/

s]

0

50

100

150Maggia - Bignasco

Duration (% of time)0 50 100

Flow

[m3 /s]

0

50

100

150Maggia - Bignasco

ObservationSimulation

Duration (% of time)J FMAMJ J ASOND

Flow

[m3 /s]

0

10

20

30Maggia - Bignasco

= a)

c) d) b)

Net production [MWh]

0

5

1500

10

Envi

ronm

enta

l dis

tanc

e to

targ

et [-

]

15

20

2000

Net revenue [CHF] 1054.543.52500 32.521.51

1950

2000

2050

2100

2150

2200

2250

2300

2350

2400

Net

pro

duct

ion

[MW

h]

SCCER-SoE Annual Conference 2018

Multiobjective optimal operation of the Maggia hydropower systems: tradeoffs between environment conservation and hydropower D. Anghileri1, E. Weber1, N. Peleg1, A. Castelletti1, and P. Burlando1. 1) Institute of Environmental Engineering ETH Zurich;

Motivation and objectives

Volatile electricity prices and hydrological conditions might call for more flexible hydropower operations, which may expose downstream riverine ecosystems to increased threats. The objectives of this work are: •  to analyze the well known conflict between hydropower generation

and environment conservation; •  to balance the profitability of hydropower companies and

environment conservation.

Method and tools To analyze the tradeoffs between hydropower interests and environment conservation, we use: i) an hydrological model (Topkapi-ETH) [1] •  to simulate water availability to hydropower facilities; •  to simulate the effects of different hydropower operations on the

downstream riverine ecosystem; ii) a multi-objective optimization technique (evolutionary multi-objective direct policy search) [2] •  to simulate the effects of different environmental conditions on

hydropower performance; •  to explore different trade-off operations that aim at balancing

hydropower performance and ecosystem conditions.

Preliminary results

Hydrological modeling We consider two different setups for simulating the pristine ecosystem during the pre-dam condition and the current situation during the post-dam condition.

Research questions

•  How much do environmental flows limit hydropower operating interests?

•  How much will more flexible operations of hydropower reservoirs harm the environment?

•  Do the trade-offs between hydropower interests and environment conservation change with increased energy price and water availability uncertainty?

Study site

!

!

!

!

!

!Bignasco, MaggiaBignasco, Bavona

Locarno, Solduno

Bignasco, Ponte nuovo

Cevio

Robiei

Airolo

Sonogno

Cimetta

Locarno Monti

Legend! Meteo station

Streamflow station

Lakes

Glacier [m]0 - 10

10 - 32

32 - 61

61 - 100

100 - 170

DEMHigh : 3350

Low : 191

±0 3 6 9 12 151.5

Km

!

!

!

!

!

!Bignasco, MaggiaBignasco, Bavona

Locarno, Solduno

Bignasco, Ponte nuovo

Cevio

Robiei

Airolo

Sonogno

Cimetta

Locarno Monti

Legend! Meteo station

Streamflow station

Lakes

Glacier [m]0 - 10

10 - 32

32 - 61

61 - 100

100 - 170

DEMHigh : 3350

Low : 191

±0 3 6 9 12 151.5

Km

Hydropower  system  features: •  Mul4-­‐reservoir  hydropower  system

•  Produc4on  and  pumping  plants •  Extensive  diversion  network

Figure 1: Left: Map of the Maggia river catchment and schematic of the hydropower system (reservoirs and plants are represented with triangles and circles respectively). The system is composed of 7 reservoirs with a total capacity of 600 MW, which produce annually 1265 GWh. Right: satellite image of the natural alluvial river which is regarded a floodplain of national interest.

Figure 2: Performances of the Topkapi-ETH hydrological model during the pre-dam condition measured in terms of: a) time series, b) scatter plot, c) duration curve, and d) annual daily mean comparison between observed and simulated flow at Maggia-Bignasco.

Hydropower optimization model We use multi-objective optimization to balance the following 3 interests: •  maximization of the net electricity production (production –

pumping); •  maximization of the net revenue (production income – pumping cost); •  maximization of the ecosystem quality (we consider the pre-dam

simulation as the reference target for the optimization).

Figure 3: Performances of alternative hydropower systems operations designed using evolutionary multi-objective direct policy search. The different points represent Pareto optimal trade-offs between the above mentioned 3 objective functions.

Outlook

•  Compare the optimized trade-offs with different strategies aiming at environment conservation, such as fixed and proportional environmental flows.

•  Analyze the evolution of the Pareto optimal trade-offs under climate change and electricity price projections.

•  Use a more sophisticated model of the alluvial floodplain to simulate the interaction between surface water and groundwater (in connection to the SNF NFP70 HydroEnv Project).

[1] Fatichi et al. (2015), JoH 525, 362–382. [2] Giuliani et al. (2016), ERL 11, 035009