the w ind

86
Óbuda University Power System Department The wind Dr. Péter Kádár Óbuda University, Power System Department, Hungary [email protected]

Upload: yelena

Post on 24-Feb-2016

36 views

Category:

Documents


2 download

DESCRIPTION

The w ind. Dr. Péter Kádár Óbuda University, Power System Department , Hungary kadar.peter@kvk . uni-obuda.hu. Draft. Wind basics Drivers of the wind energy application The energy of the wind Dynamic simulation Wind forecast. The wind… … forms the surface. The wind… … blows our hair. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: The w ind

Óbuda UniversityPower System Department

The wind

Dr. Péter KádárÓbuda University, Power System Department, Hungary

[email protected]

Page 2: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Draft

• Wind basics• Drivers of the wind energy application• The energy of the wind• Dynamic simulation• Wind forecast

2

Page 3: The w ind

Óbuda UniversityPower System Department

The wind… … forms the surface

Wind basics - Patra, 2012 3

Page 4: The w ind

Óbuda UniversityPower System Department

The wind… … blows our hair

Wind basics - Patra, 2012 4

Page 5: The w ind

Óbuda UniversityPower System Department

The wind… … brakes the signes

Wind basics - Patra, 2012 5

Page 6: The w ind

Óbuda UniversityPower System Department

The wind… … moves the sailboats

Wind basics - Patra, 2012 6

Page 7: The w ind

Óbuda UniversityPower System Department

The wind… … destroys the forests

Wind basics - Patra, 2012 7

Page 8: The w ind

Óbuda UniversityPower System Department

The wind… … forwards the snow

Wind basics - Patra, 2012 8

Page 9: The w ind

Óbuda UniversityPower System Department

The wind… … blows the flag

Wind basics - Patra, 2012 9

Page 10: The w ind

Óbuda UniversityPower System Department

The wind… … lifts our kite

Wind basics - Patra, 2012 10

Page 11: The w ind

Óbuda UniversityPower System Department

The wind… … dries our cloths

Wind basics - Patra, 2012 11

Page 12: The w ind

Óbuda UniversityPower System Department

And the wind… …bends the trees

Wind basics - Patra, 2012 12

Page 13: The w ind

Óbuda UniversityPower System Department

And the wind… …turns our propeller

Wind basics - Patra, 2012 13

Page 14: The w ind

Óbuda UniversityPower System Department

…but nobody can see it!

Wind basics - Patra, 2012 14

Page 15: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Windrose

15

Page 16: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Windrose

16

Page 17: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 17

Wind turbine and measurement system

anemometer

1 nap szélirány-időtartamai (perc)

0

100

200

300ÉSZAK

ÉÉKÉK

KÉK

KELET

KDK

DK

DDKDÉL

DDNYDNY

NYDNY

NYUGAT

NYÉNY

ÉNY

ÉÉNY

Eloszlás sűrűségfüggvény

02468

10121416

0 0,5 1 1,5 2 2,5 3 3,5 4 4,5 5 5,5 6

szélsebesség m/s

Mér

ések

dar

absz

áma

Page 18: The w ind

Óbuda UniversityPower System Department

Measurements

Wind basics - Patra, 2012 18

Page 19: The w ind

Óbuda UniversityPower System Department

Simple windrose

Wind basics - Patra, 2012 19

1 nap szélirány-időtartamai (perc)

0

100

200

300ÉSZAK

ÉÉKÉK

KÉK

KELET

KDK

DK

DDKDÉL

DDNYDNY

NYDNY

NYUGAT

NYÉNY

ÉNY

ÉÉNY

Page 20: The w ind

Óbuda UniversityPower System Department

Speed-Weighted windrose

• Direction?• Average speed?• Energy?

Wind basics - Patra, 2012 20

0

50

100

150

200ÉSZAK

ÉÉK

ÉK

KÉK

KELET

KDK

DK

DDKDÉL

DDNY

DNY

NYDNY

NYUGAT

NYÉNY

ÉNY

ÉÉNY

Átlagos szélsebesség súlyozva 2006.09.07.

Page 21: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Main winter directions

21

Page 22: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Main yearly directions

22

Page 23: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 23

Wind (speed) map for 10 m heights

Page 24: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Wind (speed) map for 75 m height

24

Page 25: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Daily wind course in diff. heights

A szélsebesség átlagos napi menete különböző magasságokbanSzeged, SODAR

0

1

2

3

4

5

6

7

8

9

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24

óra

m/s

30 m 45 m 60 m 75 m 90 m 105 m 120 m 135 m 150 m

25

Page 26: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Upscaling

• Measurements or calculations on different heights• Upscaling – continuous formula to define the windspeed in

other heights• e.g. Hellmann equation

26

Page 27: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 27

Local wind profile

20 0

17 5

22 5

25 0

27 5

30 0

32 5

35 0

37 5

5 10 15 20

T á vo lság [k m ]

Teng

ersz

int f

elet

ti m

agas

ság

[m]

N Y

H eg yh átsá l

20 0

22 5

25 0

27 5

30 0

35 0

37 5

32 5

Teng

ersz

int f

elet

ti m

agas

ság

[m]

3 m s-1

3 m s-1

4 m s-1

4 m s-1

5 m s-1

5 m s-1

6 m s-1

6 m s-1

É

H eg yh átsá l

Page 28: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 28

Global windforecast services

Page 29: The w ind

Óbuda UniversityPower System Department

www.met.hu

Wind basics - Patra, 2012 29

Page 30: The w ind

Óbuda UniversityPower System Department

On-line: http://www.idokep.hu

Wind basics - Patra, 2012 30

Page 31: The w ind

Óbuda UniversityPower System Department

Historical data(http://www.met.hu/megfigyelesek/index.php?v=Budapest)

Wind basics - Patra, 2012 31

Page 32: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 32

Global models

• Supercomputing• 27 km -> 2,5 km cubes• Differential equations

system

But• Different measurement points• Different application points

Forecast

Application

measurement

Terrestrial forms

Page 33: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 33

Professional services

• Numerical weather forecasts• Horizontal and vertical interpolation• Wind Atlas Analysis and Application Program + PARK

modell • Statistical elements• Meteorological models (e.g. ALADIN, MEANDER), other

sources (ECMWF, MM5, HIRLAM, stb.)• Result presentation by heights or by isobar?

Page 34: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Statistical approach

34

Page 35: The w ind

Óbuda UniversityPower System Department

Weibull distribution

Wind basics - Patra, 2012 35

Page 36: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 36

Local direction changes

Page 37: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 37

Local speed changes

Speed changes + direction changes = turbulence

Page 38: The w ind

Óbuda UniversityPower System Department

Turbulencies

Wind basics - Patra, 2012 38

A szélirány és -nagyság percenkénti változása (turbulencia)

-3,00

-2,00

-1,00

0,00

1,00

2,00

3,00

4,00

1 4 7 10 13 16 19 22 25 28 31 34 37 40 43 46 49 52 55 58

perc

m/s

és

rad

Szélsebesség változás (m/s)

Szélirány változás (rad)

Page 39: The w ind

Óbuda UniversityPower System Department

Local wind speed tower measurements in a wind park, during 4 min, in the range 6-10 m/s

(data from: Mov-R H1 Szélerőmű Kft., Hungary)

Wind basics - Patra, 2012 39

Page 40: The w ind

Óbuda UniversityPower System Department

Local wind speed tower measurements in a wind park, during 4 min, in the range 3-6 m/s

(data from: Mov-R H1 Szélerőmű Kft., Hungary)

Wind basics - Patra, 2012 40

Page 41: The w ind

Óbuda UniversityPower System Department

Local wind speed tower measurements in a wind park, during 4 min, over 10 m/s

(data from: Mov-R H1 Szélerőmű Kft., Hungary)

Wind basics - Patra, 2012 41

Page 42: The w ind

Óbuda UniversityPower System Department

Spread over of the wind energy application

Wind basics - Patra, 2012 42

Page 43: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Fig.Global cumulative installed wind capacity 1996-2010 Global Wind Energy Council 2010 (GWEC)

MW 43

Page 44: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Windpower capacity in Europe, 2006, MW

Forrás: www.ewea.org

0

10 000

20 000

30 000

40 000

50 000

60 000

70 000

80 000

1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009

MW

44

Page 45: The w ind

Óbuda UniversityPower System Department

Wind energy application in Europe

45

EWEA, 2010

Wind basics - Patra, 2012

Page 46: The w ind

Óbuda UniversityPower System Department

Yearly built in wind capacities in Europe

46

EWEA, 2010

20099581MW onshore582MW offshore

Wind basics - Patra, 2012

Page 47: The w ind

Óbuda UniversityPower System Department

Repowering

47Wind basics - Patra, 2012

Page 48: The w ind

Óbuda UniversityPower System Department

Some drivers of the windenergy business

• Growing demand for electricity• EU directives• Subventions• Sustainability• Reduction of CO2 emisson• Green investment boom (ROI 4-5 years)• Employment, etc.

Wind basics - Patra, 2012 48

Page 49: The w ind

Óbuda UniversityPower System Department

Catching the wind energy

Wind basics - Patra, 2012 49

Page 50: The w ind

Óbuda UniversityPower System Department

Simple energy modells

Wind basics - Patra, 2012

1. Tube modelv - speed, V - volume do not changesP – pressure, T – temperature decreeases

Reality: v, V, P, T - changes

50

2. Deccelerating massv - speed, V - volume decreasesP – pressure, T – temperature do not changes

Page 51: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 51

Power of the wind (moving mass model)

P = 0,5 ρ A v3 ηwhere • P = mechanical (~electrical) power of the wind turbine, • ρ = 1,29 kg/Nm3 – density of the air, • A = r2 π = d2 π / 4 area swept by the rotor blades (r is the

length of the blade, d = 2 r diameter of the rotor), • v = wind speed, •  η = efficiency of the rotor (theoretical max. is 60 %,

practically 10-30 % ).

Page 52: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Obstacle and the flowing air

• a - turbulent• b - laminal• c – turbulent (stall)

52

Page 53: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 53

The possible energy conversion

• Fix bladed rotor• TipSpeedRatio: v blade edge / v air

• 100 %? no

Page 54: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Different rotors and blades

• P vs wind speed• Different rpm

54

Page 55: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 55

Practical characteristics of wind turbine with control

Electronic control of• Rotor speed• Pitch

Page 56: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 56

Factory characteristics

Page 57: The w ind

Óbuda UniversityPower System Department

Typical characteristics

Wind basics - Patra, 2012 57

Szélturbina karakterisztikák

-500

0

500

1 000

1 500

2 000

2 500

0 5 10 15 20 25 30

Szélsebesség (m/s)

Kim

enő

telje

sítm

ény

(kW

)

V-90-2MWMM82G90V-90-1.8MWE-48MD77E-70

Page 58: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 58

Performance measurements

Page 59: The w ind

Óbuda UniversityPower System Department

Dynamic simulation

Wind basics - Patra, 2012 59

Page 60: The w ind

Óbuda UniversityPower System Department

Simulation logic

• Basic questions: „What happened if…”• No yearly averages but• Real wind measurements + • Defined wind park locations + • Wind turbine characteristics• Result: MW curve during a long period (a year)

Wind basics - Patra, 2012 60

Page 61: The w ind

Óbuda UniversityPower System Department

Investigated places, parks

Wind basics - Patra, 2012 61

Page 62: The w ind

Óbuda UniversityPower System Department

Frequency of the output changes

Wind basics - Patra, 2012 62

Szélfarmok összesített kimenő teljesítmény-változásának gyakorisága (10 perces)

0,00%

5,00%

10,00%

15,00%

20,00%

25,00%

30,00%

170 0

00

150 0

00

130 0

00

110 0

00

90 00

0

70 00

0

50 00

0

30 00

0

10 00

0 0

-20 00

0

-40 00

0

-60 00

0

-80 00

0

-100 0

00

-120 0

00

-140 0

00

-160 0

00

Teljesítmény változás 10 percenként

Gya

koris

ág

Page 63: The w ind

Óbuda UniversityPower System Department

Average wind speed vs monthly production

Wind basics - Patra, 2012 63

Havi szélsebesség átlag, és havi megtermelt energia kapcsolata

0,00

5000,00

10000,00

15000,00

20000,00

25000,00

30000,00

1,50 2,50 3,50 4,50 5,50 6,50 7,50

m/s

MW

h

AgárdFolyásGyőrMosonTúrkeve

Page 64: The w ind

Óbuda UniversityPower System Department

Daily energy production vs built in capacity

Wind basics - Patra, 2012 64

A napi átlagteljesítmény gyakorisága a beépített teljesítményre vonatkoztatva

0,00%

5,00%

10,00%

15,00%

20,00%

25,00%84

%

80%

76%

72%

68%

64%

60%

56%

52%

48%

44%

40%

36%

32%

28%

24%

20%

16%

12% 8% 4% 0%

Beépített teljesítmény %-a

Gya

koris

ág

Page 65: The w ind

Óbuda UniversityPower System Department

Monthly energy production

Wind basics - Patra, 2012 65

Havonta megtermelt energia

0

20 000

40 000

60 000

80 000

100 000

120 000

Janu

ár

Febru

ár

Március

Április

Május

Júniu

sJú

lius

Augus

ztus

Szeptember

Októbe

r

Novembe

r

Decembe

r

Hónap

MW

h

Page 66: The w ind

Óbuda UniversityPower System Department

Small wind

Wind basics - Patra, 2012 66

Kimenő teljesítmény a minimális energiatermelésű napon - 2005.11.02 (és előtte/utána 1 nappal)

0

20000

40000

60000

80000

100000

120000

140000

160000

180000

0:00

:00

1:40

:00

3:20

:00

5:00

:00

6:40

:00

8:20

:00

10:0

0:00

11:4

0:00

13:2

0:00

15:0

0:00

16:4

0:00

18:2

0:00

20:0

0:00

21:4

0:00

23:2

0:00

1:00

:00

2:40

:00

4:20

:00

6:00

:00

7:40

:00

9:20

:00

11:0

0:00

12:4

0:00

14:2

0:00

16:0

0:00

17:4

0:00

19:2

0:00

21:0

0:00

22:4

0:00

0:20

:00

2:00

:00

3:40

:00

5:20

:00

7:00

:00

8:40

:00

10:2

0:00

12:0

0:00

13:4

0:00

15:2

0:00

17:0

0:00

18:4

0:00

20:2

0:00

22:0

0:00

23:4

0:00

Idő

kW

Túrkeve

Moson

Győr

Folyás

Agárd

Page 67: The w ind

Óbuda UniversityPower System Department

Large wind

Wind basics - Patra, 2012 67

Kimenő teljesítmény a maximális energiatermelésű (és átlagteljesítményű) napon - 2005.12.30(és előtte/utána 1 nappal)

0

100000

200000

300000

400000

500000

600000

0:00

:00

1:40

:00

3:20

:00

5:00

:00

6:40

:00

8:20

:00

10:0

0:00

11:4

0:00

13:2

0:00

15:0

0:00

16:4

0:00

18:2

0:00

20:0

0:00

21:4

0:00

23:2

0:00

1:00

:00

2:40

:00

4:20

:00

6:00

:00

7:40

:00

9:20

:00

11:0

0:00

12:4

0:00

14:2

0:00

16:0

0:00

17:4

0:00

19:2

0:00

21:0

0:00

22:4

0:00

0:20

:00

2:00

:00

3:40

:00

5:20

:00

7:00

:00

8:40

:00

10:2

0:00

12:0

0:00

13:4

0:00

15:2

0:00

17:0

0:00

18:4

0:00

20:2

0:00

22:0

0:00

23:4

0:00

Idő

kW

Túrkeve

Moson

Győr

Folyás

Agárd

Page 68: The w ind

Óbuda UniversityPower System Department

Meteorological front in and out

Wind basics - Patra, 2012 68

Kimenő teljesítmény a front megérkezésekor

0

50000

100000

150000

200000

250000

300000

350000

400000

450000

Idő

kW

Túrkeve

Moson

GyőrFolyás

Agárd

Kimenő teljesítmény a front elvonulásakor

0

50000

100000

150000

200000

250000

300000

350000

400000

450000

Idő

kW

TúrkeveMoson

Győr

FolyásAgárd

Page 69: The w ind

Óbuda UniversityPower System Department

The „problematic” days

Wind basics - Patra, 2012 69

Kimenő teljesítmény egy átlagos energiatermelésű napon - 2005.05.17 (és előtte/utána 1 nappal)

0

50000

100000

150000

200000

250000

300000

350000

400000

450000

0:00

:00

1:40

:00

3:20

:00

5:00

:00

6:40

:00

8:20

:00

10:0

0:00

11:4

0:00

13:2

0:00

15:0

0:00

16:4

0:00

18:2

0:00

20:0

0:00

21:4

0:00

23:2

0:00

1:00

:00

2:40

:00

4:20

:00

6:00

:00

7:40

:00

9:20

:00

11:0

0:00

12:4

0:00

14:2

0:00

16:0

0:00

17:4

0:00

19:2

0:00

21:0

0:00

22:4

0:00

0:20

:00

2:00

:00

3:40

:00

5:20

:00

7:00

:00

8:40

:00

10:2

0:00

12:0

0:00

13:4

0:00

15:2

0:00

17:0

0:00

18:4

0:00

20:2

0:00

22:0

0:00

23:4

0:00

Idő

kW

Túrkeve

Moson

Győr

Folyás

Agárd

Page 70: The w ind

Óbuda UniversityPower System Department

Correlation analysis of wind measurements

Wind basics - Patra, 2012 70

Page 71: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

The problem

• Wind production forecast = wind forecast + turbine caharactereistics

• There is no exact wind forecast for the wind turbine sites• The forecast is crucial for the integration large wind parks

into the network• The question: Can we forecast the generated energy based

on remote wind forecast?

71

Page 72: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012 72

The real task

• Not in that place• Not in that time• Not correct wind forecast

Forecast

Application

measurement

Terrestrial forms

Page 73: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

The factory characteristics

• In the project we investigate a V-27 turbine at “Bükkaranyos” and wind measurement ant “Folyás” meteorological station.

• The figure shows a typical characteristics of wind turbines (V27). This curve is measured in stationary mode, it does not contain the effect of local turbulences, direction changes and wind speed differences between the upper and lower part of the (spinning) rotor measurements.

73

Page 74: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Characteristics based on pure measurements

?

74

Page 75: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Correlation?

The causes of the lack of correlation are• The distance between the wind turbine and wind

measurement• The local wind turbulences that create difference

in the wind blow at the two measurement points.

75

Page 76: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Other causes: turbulence

• The local wind turbulences that create difference in the wind blow at the two measurement points.

• fast (1-6 sec), the medium (1-6 min) and the slow (1-6 hour) changes.

• The fast and medium wind speed and direction changes are not handled (followed) by the turbine, it causes deviances.

• Turbine dynamics and measurement errors, etc.– Wind speed changes– Wind direction changes– Wind speed changes measurement on minute scale

76

Page 77: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Distributional reorganization: a functional transformation

An ideal wind speed and power output measurement at the same tower should give the factory characteristics of the wind turbine, the two measurements correlate on the factory curve. If we prepare the cumulative distribution function of both measurements, the previous correlation is still valid and we get the same curve.

77

Page 78: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Back to the measurements (Bükkaranyos – Folyás: 33km)

78

Page 79: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Characteristics matching

Based on the above mentioned, the locally differently running curve is substituted by a globally similarly cumulated distribution function. We investigate not the specific synchronized moments but the same period, so we integrate the power into generated energy. This is an energy based characteristics retrieval. Figure shows characteristics similar to the factory characteristics (marked by dots).

79

Page 80: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Meaurement distances

Name of wind measurement place

Distance of the wind turbine “Bükkaranyos”

Folyás 33 km

Agárd 187 km

Túrkeve 98 km

Mosonmagyaróvár 263 km

Győr 238 km

80

Page 81: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Wind power generation forecast

See WinDemo!

81

Page 82: The w ind

Óbuda UniversityPower System Department

Wind power generation forecast

Rough:• Windspeed• CharactereisticFine• + temperature• + pressure• + humidity• + direction

CORRELATION FACTOR!

Wind basics - Patra, 2012 82

Page 83: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Upscaling

• The previously shown remote upscaling factor is defined by the energy production of a time period. Applying the Hellmann equation (1) for the same tower (height 33 m, measurements height 10 m), the exponent is 0,445, that is a good experimental result.

83

Page 84: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Remote scaling

84

Page 85: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Conclusion

• It is not possible to retrieve the vendor given stationary winds speed–generation characteristics of the wind turbine based on the real-time measurements.

• The calculations above show that for real-time generation forecast purposes only close measurement/estimation points could be used.

• The wind forecasts work on worldwide global models, these are theoretically not capable of forecasting local turbulences – which cause the 0,5 - 5 min deviations in the power output.

• In spite of this fact, based on further measurements quite good energy production estimations can be done. We used the cumulative distribution function to define the ratio between remote wind speed measurement and the possible local wind speed at the turbine.

85

Page 86: The w ind

Óbuda UniversityPower System Department

Wind basics - Patra, 2012

Thanks for the attention!

86