energy system modelling summer semester 2018, lecture 1...dec 01 dec 03 dec 05 dec 07 dec 09 dec 11...

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Energy System Modelling Summer Semester 2018, Lecture 1 Dr. Tom Brown, [email protected], https://nworbmot.org/ Karlsruhe Institute of Technology (KIT), Institute for Automation and Applied Informatics (IAI) 11th July 2018

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Page 1: Energy System Modelling Summer Semester 2018, Lecture 1...Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 13 0.0 0.2 0.4 0.6 0.8 1.0 Profile normalised by max (per unit) Wind Hydro Storing/Curtailment

Energy System Modelling

Summer Semester 2018, Lecture 1

Dr. Tom Brown, [email protected], https://nworbmot.org/

Karlsruhe Institute of Technology (KIT), Institute for Automation and Applied Informatics (IAI)

11th July 2018

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Table of Contents

1. Administration

2. Course outline

3. Introduction: Balancing Variable Renewable Energy

4. Electricity Consumption

5. Electricity Generation

6. Variable Renewable Energy (VRE)

7. Balancing a single country

2

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Administration

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Contact Details

Dr. Tom Brown

Young Investigator Group Leader

Energy System Modelling Research Group

Institute for Automation and Applied Informatics (IAI)

KIT, North Campus

[email protected]

https://nworbmot.org/

I am a physicist who has specialised in the optimisation of energy systems and the interactions

of complex networks. I now work at the intersection of informatics, economics, engineering,

mathematics, meteorology and physics.

4

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Lectures and Exercise Classes

The course will take place over five days: 11.7, 13.7, 16.7, 17.7 and 18.7.

Each day will consist of 3 lectures and one exercise class:

09:45-11:15 Lecture 1

11:30-13:00 Lecture 2

14:00-15:30 Exercise Class

15:45-17:15 Lecture 3

Some of the exercises will require you to program in Python, so please bring a laptop. We will

help you to install Python and the requisite libraries.

The course has 4 ECTS points.

Location: 50.41 Raum 145/146

5

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Course Website

You can find the course website here:

https://nworbmot.org/courses/esm-2018/

by following the links from:

https://nworbmot.org/

Course notes, exercise sheets and other links can be found there.

6

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Registration for Oral Exam

To get an evaluation at the end of the course, you need to register online for the oral

examination.

The oral examinations will take place some time in August on a single date. The date will be

decided during the final lecture, based on when we are all available.

7

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MA Thesis: Industrial Demand in a Fossil-Free European Energy System

We have some exciting opportunities in the Energy System Modelling group at IAI to look at

the integration of industrial demand and emissions in our European energy system model.

See the advert:

https://nworbmot.org/courses/esm-2018/esm-ma-bio-industry.pdf

Objectives:

• Collect sustainable biomass potentials for each European country by fuel type (forest

residues, agricultural residues, municipal waste, etc.) based on existing sources.

• Collect energy use and emissions per country per industry from standard statistical sources.

• Build the different energy pathways into an existing model of the European energy system.

• Simulate the optimal mix of energy sources and technologies to eliminate CO2 emissions

from the industrial sector.

8

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Literature

There is no book which covers all aspects of this course. In particular there is no good source

for the combination of data analysis, complex network theory, optimisation and energy systems.

But there are lots of online lecture notes. The world of renewables also changes fast...

The following are concise:

• Volker Quashning, “Regenerative Energiesysteme”, Carl Hanser Verlag Munchen, 2015

• Leon Freris, David Infield, “Renewable Energy in Power Systems”, Wiley, 2006

• Goran Andersson Skript, “Elektrische Energiesysteme: Vorlesungsteil

Energieubertragung,” online

• D.R. Biggar, M.R. Hesamzadeh, “The Economics of Electricity Markets,” Wiley, 2014

9

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Course outline

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Course outline

This course will cover the following topics:

• General properties of renewable power, time series analysis

• Backup generation, curtailment

• Network modelling in power systems

• Storage modelling

• Optimization theory

• Energy system economics

• Dynamics of renewable energy networks (synchronization, etc.)

• Complex network techniques for renewable energy networks (flow tracing, etc.)

11

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Introduction: Balancing Variable Re-

newable Energy

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The Global Carbon Dioxide Challenge: Budgets from 2016

600 Gt budget gives 33% chance of 1.5◦C (Paris: ‘pursue efforts to limit [warming] to 1.5◦C’)

800 Gt budget gives 66% chance of 2◦C (Paris: hold ‘the increase...to well below 2◦C’)

13Source: ‘Three years to safeguard our climate,’ Nature, 2017

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Research questions

1. What infrastructure (wind, solar, hydro generators, heating/cooling units, storage and

networks) does a highly renewable energy system require and where should it go?

2. Given a desired CO2 emissions reduction (e.g. 95% compared to 1990), what is the

cost-optimal combination of infrastructure?

3. How do we deal with the variablility of wind and solar: balancing in space with networks

or in time with storage?

14

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Daily variations: challenges and solutions

00:0030-Apr

03:0006:0009:0012:0015:0018:0021:000.0

0.2

0.4

0.6

Germ

an so

lar g

ener

atio

n [p

er u

nit]

Germany solar

00:0025-Apr

03:0006:0009:0012:0015:0018:0021:00

0.2

0.4

0.6

0.8

1.0

Germ

an ro

ad tr

ansp

ort [

per u

nit]

Germany road transport

Daily variations in supply

and demand can be

balanced by

• short-term storage

(e.g. batteries,

pumped-hydro, small

thermal storage)

• demand-side

management (e.g.

battery electric

vehicles, industry)

• east-west grids over

multiple time zones

15

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Synoptic variations: challenges and solutions

Jan2011

3103 10 17 240.0

0.2

0.4

0.6

0.8

Germ

an w

ind

gene

ratio

n [p

er u

nit]

Germany onshore windSynoptic variations in

supply and demand can be

balanced by

• medium-term

storage (e.g.

chemically with

hydrogen or methane

storage, thermal

energy storage, hydro

reservoirs)

• continent-wide grids

Transmission lines

Country nodes

16

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Seasonal variations: challenges and solutions

Jan2011

FebMar AprMay Jun Jul AugSep OctNovDec0.0

0.1

0.2

0.3

0.4

0.5

0.6

Mon

thly

yie

ld [p

er u

nit c

apac

ity]

Germany onshore windGermany solar

Jan2011

FebMar AprMay Jun Jul AugSepOct NovDec0

50

100

150

200

250

Germ

an h

eat d

eman

d [G

W] Germany heat demand

Seasonal variations in

supply and demand can be

balanced by

• long-term storage

(e.g. chemically with

hydrogen or methane

storage, long-term

thermal energy

storage, hydro

reservoirs)

• north-south grids

over multiple

latitudes

17

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Variability: Single wind site in Berlin

Looking at the wind output of a single wind plant over two weeks, it is highly variable,

frequently dropping close to zero and fluctuating strongly.

Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0

0.2

0.4

0.6

0.8

1.0

Pro

file

norm

alis

ed b

y m

ax (

per

unit

)

Berlin wind

18

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Electricity consumption is much more regular

Electrical demand is much more regular over time - dealing with the mismatch between

locally-produced wind and the demand would require a lot of storage...

Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0

0.2

0.4

0.6

0.8

1.0

Pro

file

norm

alis

ed b

y m

ax (

per

unit

)

Germany load

19

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Variability: Different wind conditions over Germany

But the wind does not blow the same at every site at every time: at a given time there are a

variety of wind conditions across Germany. These differences balance out over time and

space.

20Source: https://earth.nullschool.net/

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Variability: Single country: Germany

For a whole country like Germany this results in valleys and peaks that are somewhat

smoother, but the profile still frequently drops close to zero.

Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0

0.2

0.4

0.6

0.8

1.0

Pro

file

norm

alis

ed b

y m

ax (

per

unit

)

Berlin wind

Germany onshore wind

21

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Variability: Different wind conditions over Europe

The scale of the weather systems are bigger than countries, so to leverage the full smoothing

effects, you need to integrate wind at the continental scale.

22Source: https://earth.nullschool.net/

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Variability: A continent: Europe

If we can integrate the feed-in of wind turbines across the European continent, the feed-in is

considerably smoother: we’ve eliminated most valleys and peaks.

Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0

0.2

0.4

0.6

0.8

1.0

Pro

file

norm

alis

ed b

y m

ax (

per

unit

)

Berlin wind

Germany onshore wind

Europe all wind

23

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Variability: A continent: Wind plus Hydro

Flexible, renewable hydroelectricity from storage dams in Scandinavia and the Alps can fill

many of the valleys; excess energy can either be curtailed (spilled) or stored.

Dec 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec 130.0

0.2

0.4

0.6

0.8

1.0

Pro

file

norm

alis

ed b

y m

ax (

per

unit

)

Wind

Hydro

Storing/Curtailment

Electrical Demand

24

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Costs: No interconnecting transmission allowed

Technology by energy:offshore

wind

10%

onshorewind

35%

solar

37%

run of river

4%

gas

5%

hydro

9%

Average cost e86/MWh:

0

20

40

60

80

100

Avera

ge s

yst

em

cost

[EU

R/M

Wh]

offshore wind

onshore wind

solar

gashydrogen storage

battery storage

Transmission lines (= 10 GW)

Yearly energy (= 50 TWh/a)

Countries must be self-sufficient at all times; lots of storage

and some gas to deal with fluctuations of wind and solar. 25

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Dispatch with no interconnecting transmission

For Great Britain with no interconnecting transmission, excess wind is either stored as

hydrogen or curtailed:

Jul 01 Jul 03 Jul 05 Jul 07 Jul 09 Jul 11 Jul 13

20

0

20

40

60

Pow

er

[GW

]

Demand

GB onshore wind

GB offshore wind

GB gas

GB hydrogen storage

GB onwind available

GB offwind available

26

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Costs: Cost-optimal expansion of interconnecting transmission

Technology by energy:offshore

wind

8%

onshorewind

56%solar17%

run of river5%

gas

5%

hydro

10%

Average cost e64/MWh:

no lines optimal0

20

40

60

80

100

Avera

ge s

yst

em

cost

[EU

R/M

Wh]

transmission linesoffshore wind

onshore wind

solargashydrogen storagebattery storage

Transmission lines (= 10 GW)

Yearly energy (= 50 TWh/a)

Large transmission expansion; onshore wind dominates. This

optimal solution may run into public acceptance problems. 27

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Dispatch with cost-optimal interconnecting transmission

Almost all excess wind can be now be exported:

Jul 01 Jul 03 Jul 05 Jul 07 Jul 09 Jul 11 Jul 1340

20

0

20

40

60

80

100

120

140

Pow

er

[GW

]

Demand

GB onshore wind

GB offshore wind

GB gas

GB hydrogen storage

GB onwind available

GB offwind available

Exports

28

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Electricity Only Costs Comparison

0 50 100 150 200 250

Allowed interconnecting transmission lines [TWkm]

0

50

100

150

200

250

300

Syst

em

cost

[EU

R b

illio

n p

er

year]

today'sgrid

battery storage

hydrogen storage

gas

solar

onshore wind

offshore wind

transmission lines

• Average total system costs

can be as low as e 64/MWh

• Energy is dominated by wind

(64% for the cost-optimal

system), followed by hydro

(15%) and solar (17%)

• Restricting transmission

results in more storage to

deal with variability, driving

up the costs by up to 34%

• Many benefits already locked

in at a few multiples of

today’s grid29

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Different flexibility options have difference temporal scales

Jan2011

Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0.0

0.2

0.4

0.6

0.8

1.0

1.2

Energy level of storage (norm

ed)

hydrogen storagereservoir hydro

• Hydro

reservoirs are

seasonal

• Hydrogen

storage is

synoptic

30

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Different flexibility options have difference temporal scales

Aug2011

08 15 22 290.0

0.2

0.4

0.6

0.8

1.0

1.2

Energy level of storage (norm

ed)

battery storagePHS

hydrogen storagereservoir hydro

• Pumped hydro

and battery

storage are

daily

31

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Features of this example

This example has several features which will accompany us through this lecture:

1. We have to account for the variations of wind and solar in time and space.

2. These variations take place at different scales (daily, synoptic, seasonal).

3. We often have a choice between balancing in time (with storage) or in space (with

networks).

4. Optimisation is important to increase cost-effectiveness, but we should also look at

near-optimal solutions.

32

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It’s not just about electricity demand...

EU28 CO2 emissions in 2015 (total 3.2 Gt CO2, 8% of global):

public electricity and heat

33.3%residential heating

11.8%services heating 4.9%rail transport 0.2%

road transport

26.8%

navigation

4.7%

aviation

4.9% industry (non-electric)13.0%

other0.4%

33Source: Brown, data from EEA

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...but electification of other sectors is critical for decarbonisation

Wind and solar dominate the expandable potentials for low-carbon energy provision, so

electrification is essential to decarbonise sectors such as transport and heating.

Fortunately, these sectors can also offer crucial flexibility back to the electricity system.

34Source: Tesla; heat pump: Kristoferb at English Wikipedia

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Efficiency of renewables and sector coupling

exceed 50 %.

Fuel

Fossil-fuel condensing power station

Losses

Electricity

Renewableelectricity

Tom

orro

wTo

day

Electricity Heat Transport

Wind/solar energy

Electricity Renewableelectricity

Electric mobility

Renewableelectricity

Ambient heat

Heat pumps

Losses

Heat

Fuel

Gas heating

Losses

Heat Fuel

Internal-combustion engine

Losses

Propulsion

Propulsion

Losses

35Source: BMWi White Paper 2015

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Low cost of renewable energy 2017 (NB: ignores variability)

36Source: Lazard’s LCOE Analysis V11

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Energy Transition: Several changes happening simultaneously

Energiewende: The Energy Transition, consists of several parts:

• Transition to an energy system with low greenhouse gas emissions

• Renewables replace fossil-fuelled generation (and nuclear in some countries)

• Increasing integration of international electricity markets

• Better integration of transmission constraints in electricity markets

• Sector coupling: heating, transport and industry electrify

• More decentralised location and ownership in the power sector

37

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What can informatics contribute?

In all these questions we are limited by computational complexity.

Informatics can contribute on the data side:

• Processing and analysing enormous weather datasets

• Geographical potential analysis with GIS tools

• Visualisation of results

and on the algorithmic side:

• Data reduction: clustering and PCA examples to follow later

• New optimisation routines for speed and accuracy

• Information theory to trace interdependencies

Build on informatics’ interdisciplinary links to engineering, economics, meteorology,

mathematics and physics.38

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Electricity Consumption

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Why is electricity useful?

Electricity is a versatile form of energy carried by electrical charge which can be consumed in a

wide variety of ways (with selected examples):

• Lighting (lightbulbs, halogen lamps, televisions)

• Mechanical work (hoovers, washing machines, electric vehicles)

• Heating (cooking, resistive room heating, heat pumps)

• Cooling (refrigerators, air conditioning)

• Electronics (computation, data storage, control systems)

• Industry (electrochemical processes)

Compare the convenience and versatility of electricity with another energy carrier: the chemical

energy stored in natural gas (methane), which can only be accessed by burning it.

40

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Power: Flow of energy

Power is the rate of consumption of energy.

It is measured in Watts:

1 Watt = 1 Joule per second

The symbol for Watt is W, 1 W = 1 J/s.

1 kilo-Watt = 1 kW = 1,000 W

1 mega-Watt = 1 MW = 1,000,000 W

1 giga-Watt = 1 GW = 1,000,000,000 W

1 tera-Watt = 1 TW = 1,000,000,000,000 W

41

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Power: Examples of consumption

At full power, the following items consume:

Item Power

New efficient lightbulb 10 W

Old-fashioned lightbulb 70 W

Single room air-conditioning 1.5 kW

Kettle 2 kW

Factory ∼1-500 MW

CERN 200 MW

Germany total demand 35-80 GW

42

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Energy

In the electricity sector, energy is usually measured in ‘Watt-hours’, Wh.

1 kWh = power consumption of 1 kW for one hour

E.g. a 10 W lightbulb left on for two hours will consume

10 W * 2 h = 20 Wh

It is easy to convert this back to the SI unit for energy, Joules:

1 kWh = (1000 W) * (1 h) = (1000 J/s)*(3600 s) = 3.6 MJ

43

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Electricity spot market: trading of energy

Energy is traded in MWh; current price around 30-40 e/MWh, but sinking thanks to

renewables and the merit order effect:

44Source: Agora Energiewende

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Consumption metering

• Look for your

electricity meter at

home

• Mine here shows

42470.3 kWh

• Check what the value

is a week later

45

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Electricity bill

My bill for 2014-5: 1900 kWh for a year, at a cost of e570, which corresponds to 0.3 e/kWh

or 300 e/MWh. But the spot market price is 30 e/MWh, so what’s going on??

46

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Household price breakdown

Although the wholesale price is going down, other taxes, grid charges and renewables subsidy

(EEG surcharge) have kept the price high.

HOWEVER the EEG is only high because it is paying for solar panels bought at a time when

they were still comparatively expensive; but through the German subsidy, production volumes

were high and the learning curve has brought the costs down exponentially.47Source: Agora Energiewende

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Yearly energy to power

Germany consumes around 600 TWh per year, written 600 TWh/a.

What is the average power consumption?

600 TWh/a =(600 TW) ∗ (1 h)

(365 ∗ 24 h)

=600

8760TW

= 68.5 GW

48

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Discrete Consumers Aggregation

The discrete actions of individual consumers smooth out statistically if we aggregate over many

consumers.

49

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Load curve properties

The Germany load curve (around 500 TWh/a) shows daily, weekly and seasonal patterns;

religious festivals are also visible.

Jan2011

Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0

10

20

30

40

50

60

70

80

DE load [

GW

]

DE load

50

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Load duration curve

For some analysis it is useful to construct a duration curve by stacking the hourly values from

highest to lowest.

0 20 40 60 80

Percentage of time during year

0

10

20

30

40

50

60

70

80

DE load [

GW

]

DE load

51

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Load density function

Similarly we can also build the probability density function:

0 20 40 60 80 100

DE load [GW]

0.000

0.005

0.010

0.015

0.020

0.025

0.030

0.035

0.040

Pro

babili

ty d

ensi

ty

DE load

52

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Load spectrum

If we Fourier transform, the seasonal, weekly and daily frequencies are clearly visible.

0 50 100 150 200 250 300 350 400

frequency [a−1]

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

1.8

Spect

ral densi

ty

1e9

DE load

53

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Electricity Generation

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How is electricity generated?

Conservation of Energy: Energy cannot be created or destroyed: it can only be converted

from one form to another.

There are several ‘primary’ sources of energy which are converted into electrical energy in

modern power systems:

• Chemical energy, accessed by combustion (coal, gas, oil, biomass)

• Nuclear energy, accessed by fission reactions, perhaps one day by fusion too

• Hydroelectric energy, allowing water to flow downhill (gravitational potential energy)

• Wind energy (kinetic energy of air)

• Solar energy (accessed with photovoltaic (PV) panels or concentrating solar thermal power

(CSP))

• Geothermal energy

NB: The definition of ‘primary’ is somewhat arbitrary.55

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Power: Examples of generation

At full power, the following items generate:

Item Power

Solar panel on house roof 15 kW

Wind turbine 3 MW

Coal power station 1 GW

56

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Generators

With the exception of solar photovoltaic panels (and electrochemical energy and a few other

minor exceptions), all generators convert to electrical energy via rotational kinetic energy and

electromagnetic induction in an alternating current generator.

57Source: Wikipedia

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Example of electricity generation across major EU countries in 2013

NO ES GB DE FR0

100

200

300

400

500

600

700

800

900

Ele

ctri

city

Genera

tion in 2

013 [

TW

h/a

]

Solar

Wind

Biomass

Hydro

Oil

Gas

Hard Coal

Lignite

Nuclear

58

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Electricity generation in Germany per year

In 15 years Germany has gone from a system dominated by nuclear and fossil fuels, to one with

33% renewables in electricity consumption.

2002 2004 2006 2008 2010 2012 2014

year

0

100

200

300

400

500

600

Yearl

y e

lect

rici

ty g

enera

tion in G

erm

any [

TW

h/a

]

Nuclear

Brown Coal

Hard Coal

Gas

Hydro

Biomass

Wind

Solar

Exports

59Source: Author’s own representation based on

https://www.energy-charts.de/energy_en.htm

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Efficiency

When fuel is consumed, much/most of the energy of the fuel is lost as waste heat rather than

being converted to electricity.

The thermal energy, or calorific value, of the fuel is given in terms of MWhth, to distinguish it

from the electrical energy MWhel.

The ratio of input thermal energy to output electrical energy is the efficiency.

Fuel Calorific energy Per unit efficiency Electrical energy

MWhth/tonne MWhel/MWhth MWhel/tonne

Lignite 2.5 0.4 1.0

Hard Coal 6.7 0.45 2.7

Gas 15.4 0.4 6.16

Uranium 150000 0.33 50000

60

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Fuel costs to marginal costs

The cost of a fuel is often given in e/kg or e/MWhth.

Using the efficiency, we can convert this to e/MWhel.

Fuel Per unit efficiency Cost per thermal Cost per elec.

MWhel/MWhth e/MWhth e/MWhel

Lignite 0.4 4.5 11

Hard Coal 0.45 10 22

Gas 0.4 23 58

Uranium 0.33 3.3 10

61

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CO2 emissions per MWh

The CO2 emissions of the fuel.

Fuel tCO2/t tC02/MWhth tCO2/MWhel

Lignite 0.9 0.36 0.9

Hard Coal 2.4 0.36 0.8

Gas 3.1 0.2 0.5

Uranium 0 0 0

Current CO2 price in EU Emissions Trading Scheme (ETS) is around e16/tCO2

62

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CO2 emissions from electricity sector

Despite the increase in renewables in the electricity sector, CO2 emission have not been

reduced substantially in Germany. This is partly because German exports have also increased.

63Source: Agora Energiewende

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Variable Renewable Energy (VRE)

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Wind time series

Unlike the load, the wind is much more variable, regularly dropping close to zero and rarely

reaching full output (when aggregated over all of Germany).

Jan2011

Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0.0

0.2

0.4

0.6

0.8

1.0

DE o

nw

ind [

per

unit

]

DE onwind

65

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Wind time series: weekly

If we take a weekly average we see higher wind in the winter and some periodic patterns over

2-3 weeks (synoptic scale).

Jan2011

Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan2012

0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

DE o

nwin

d [p

er u

nit]

DE onwind

66

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Wind duration curve

0 20 40 60 80

Percentage of time during year

0.0

0.2

0.4

0.6

0.8

1.0D

E o

nw

ind [

per

unit

]

DE onwind

67

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Wind density function

0.0 0.2 0.4 0.6 0.8 1.0

DE onwind [per unit]

0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.5Pro

babili

ty d

ensi

ty

DE onwind

68

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Wind spectrum

If we Fourier transform, the seasonal, synoptic and daily patterns become visible.

0 50 100 150 200 250 300 350 400

frequency [a−1]

0

20000

40000

60000

80000

100000

120000

Spect

ral densi

ty

DE onwind

69

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Solar time series

Solar is variable, but more predictable than wind.

Jan2011

Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

DE s

ola

r [p

er

unit

]

DE solar

70

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Solar time series: weekly

If we take a weekly average we see higher solar in the summer.

Jan2011

Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan2012

0.00

0.05

0.10

0.15

0.20

0.25

DE s

ola

r [p

er

unit

]

DE solar

71

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Solar duration curve

0 20 40 60 80

Percentage of time during year

0.0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8D

E s

ola

r [p

er

unit

]

DE solar

72

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Solar density function

0.0 0.2 0.4 0.6 0.8 1.0

DE solar [per unit]

0

1

2

3

4

5

6

7

8

9Pro

babili

ty d

ensi

ty

DE solar

73

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Solar spectrum

If we Fourier transform, the seasonal and daily patterns become visible.

0 50 100 150 200 250 300 350 400

frequency [a−1]

0

100000

200000

300000

400000

500000

600000

700000

800000

Spect

ral densi

ty

DE solar

74

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Balancing a single country

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Power mismatch

Suppose we now try and cover the electrical demand with the generation from wind and solar.

How much wind do we need? We have three time series:

• {dt}, dt ∈ R the load (varying between 35 GW and 80 GW)

• {wt},wt ∈ [0, 1] the wind availability (how much a 1 MW wind turbine produces)

• {st}, st ∈ [0, 1] the solar availability (how much a 1 MW solar turbine produces)

We try W MW of wind and S MW of solar. Now the effective residual load or mismatch is

mt = dt −Wwt − Sst

We choose W and S such that on average we cover all the load

〈mt〉 = 0

and so that the 70% of the energy comes from wind and 30% from solar (W = 147 GW and

S = 135 GW).76

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Mismatch time series

Jan2011

Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec200

150

100

50

0

50

100D

E m

ism

atc

h [

GW

]

DE mismatch

77

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Mismatch duration curve

0 20 40 60 80

Percentage of time during year

200

150

100

50

0

50

100D

E m

ism

atc

h [

GW

]

DE mismatch

78

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Mismatch density function

150 100 50 0 50

DE mismatch [GW]

0.000

0.002

0.004

0.006

0.008

0.010

0.012

0.014Pro

babili

ty d

ensi

ty

DE mismatch

79

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Mismatch spectrum

If we Fourier transform, the synoptic (from wind) and daily patterns (from demand and solar)

become visible. Seasonal variations appear to cancel out.

0 50 100 150 200 250 300 350 400

frequency [a−1]

0.0

0.2

0.4

0.6

0.8

1.0

1.2

1.4

1.6

Spect

ral densi

ty

1e10

DE mismatch

80

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How to deal with the mismatch?

The problem is that

〈mt〉 = 0

is not good enough! We need to meet the demand in every single hour.

This means:

• If mt > 0, i.e. we have unmet demand, then we need backup generation from

dispatchable sources e.g. hydroelectricity reservoirs, fossil/biomass fuels.

• If mt < 0, i.e. we have over-supply, then we have to shed / spill / curtail the renewable

energy.

81

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Mismatch

Mar2011

07 14 21 280

50

100

150

200Pow

er

[GW

]

consumed

backup

curtailment

82

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Mismatch

Jul2011

04 11 18 250

20

40

60

80

100

120

140

160

180Pow

er

[GW

]

consumed

backup

curtailment

83

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Mismatch

Dec2011

05 12 19 260

50

100

150

200Pow

er

[GW

]

consumed

backup

curtailment

84

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Mismatch duration curve

0 20 40 60 80

Percentage of time during year

100

50

0

50

Mis

matc

h [

GW

]backup

curtailment

85

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What to do?

Backup energy costs money and may also cause CO2 emissions.

Curtailing renewable energy is also a waste.

We’ll look in the next lectures at 4 solutions:

1. Smoothing stochastic variations of renewable feed-in over larger areas, e.g. the whole of

Europe.

2. Using storage to shift energy from times of surplus to deficit.

3. Shifting demand to different times, when renewables are abundant.

4. Consuming the electricity in other sectors, e.g. transport or heating.

86