the w ind
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 PresentationTRANSCRIPT
Óbuda UniversityPower System Department
The wind
Dr. Péter KádárÓbuda University, Power System Department, Hungary
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
Óbuda UniversityPower System Department
The wind… … forms the surface
Wind basics - Patra, 2012 3
Óbuda UniversityPower System Department
The wind… … blows our hair
Wind basics - Patra, 2012 4
Óbuda UniversityPower System Department
The wind… … brakes the signes
Wind basics - Patra, 2012 5
Óbuda UniversityPower System Department
The wind… … moves the sailboats
Wind basics - Patra, 2012 6
Óbuda UniversityPower System Department
The wind… … destroys the forests
Wind basics - Patra, 2012 7
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The wind… … forwards the snow
Wind basics - Patra, 2012 8
Óbuda UniversityPower System Department
The wind… … blows the flag
Wind basics - Patra, 2012 9
Óbuda UniversityPower System Department
The wind… … lifts our kite
Wind basics - Patra, 2012 10
Óbuda UniversityPower System Department
The wind… … dries our cloths
Wind basics - Patra, 2012 11
Óbuda UniversityPower System Department
And the wind… …bends the trees
Wind basics - Patra, 2012 12
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And the wind… …turns our propeller
Wind basics - Patra, 2012 13
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…but nobody can see it!
Wind basics - Patra, 2012 14
Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Windrose
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Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Windrose
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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
Óbuda UniversityPower System Department
Measurements
Wind basics - Patra, 2012 18
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
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.
Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Main winter directions
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Wind basics - Patra, 2012
Main yearly directions
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Wind basics - Patra, 2012 23
Wind (speed) map for 10 m heights
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Wind basics - Patra, 2012
Wind (speed) map for 75 m height
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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
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6
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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
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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
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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
Óbuda UniversityPower System Department
Wind basics - Patra, 2012 28
Global windforecast services
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www.met.hu
Wind basics - Patra, 2012 29
Óbuda UniversityPower System Department
On-line: http://www.idokep.hu
Wind basics - Patra, 2012 30
Óbuda UniversityPower System Department
Historical data(http://www.met.hu/megfigyelesek/index.php?v=Budapest)
Wind basics - Patra, 2012 31
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
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?
Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Statistical approach
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Weibull distribution
Wind basics - Patra, 2012 35
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Wind basics - Patra, 2012 36
Local direction changes
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Wind basics - Patra, 2012 37
Local speed changes
Speed changes + direction changes = turbulence
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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)
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
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
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
Óbuda UniversityPower System Department
Spread over of the wind energy application
Wind basics - Patra, 2012 42
Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Fig.Global cumulative installed wind capacity 1996-2010 Global Wind Energy Council 2010 (GWEC)
MW 43
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
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80 000
1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009
MW
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Óbuda UniversityPower System Department
Wind energy application in Europe
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EWEA, 2010
Wind basics - Patra, 2012
Óbuda UniversityPower System Department
Yearly built in wind capacities in Europe
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EWEA, 2010
20099581MW onshore582MW offshore
Wind basics - Patra, 2012
Óbuda UniversityPower System Department
Repowering
47Wind basics - Patra, 2012
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
Óbuda UniversityPower System Department
Catching the wind energy
Wind basics - Patra, 2012 49
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
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2. Deccelerating massv - speed, V - volume decreasesP – pressure, T – temperature do not changes
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 % ).
Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Obstacle and the flowing air
• a - turbulent• b - laminal• c – turbulent (stall)
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Wind basics - Patra, 2012 53
The possible energy conversion
• Fix bladed rotor• TipSpeedRatio: v blade edge / v air
• 100 %? no
Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Different rotors and blades
• P vs wind speed• Different rpm
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Wind basics - Patra, 2012 55
Practical characteristics of wind turbine with control
Electronic control of• Rotor speed• Pitch
Óbuda UniversityPower System Department
Wind basics - Patra, 2012 56
Factory characteristics
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
Óbuda UniversityPower System Department
Wind basics - Patra, 2012 58
Performance measurements
Óbuda UniversityPower System Department
Dynamic simulation
Wind basics - Patra, 2012 59
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
Óbuda UniversityPower System Department
Investigated places, parks
Wind basics - Patra, 2012 61
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
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-160 0
00
Teljesítmény változás 10 percenként
Gya
koris
ág
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
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25000,00
30000,00
1,50 2,50 3,50 4,50 5,50 6,50 7,50
m/s
MW
h
AgárdFolyásGyőrMosonTúrkeve
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
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
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
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0:00
:00
1:40
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3:20
:00
5:00
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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
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)
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5:00
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8:20
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10:0
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11:4
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13:2
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15:0
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0:00
18:2
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0:00
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0:00
23:2
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1:00
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2:40
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4:20
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6:00
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7:40
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12:4
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14:2
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0:00
23:4
0:00
Idő
kW
Túrkeve
Moson
Győr
Folyás
Agárd
Óbuda UniversityPower System Department
Meteorological front in and out
Wind basics - Patra, 2012 68
Kimenő teljesítmény a front megérkezésekor
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Idő
kW
Túrkeve
Moson
GyőrFolyás
Agárd
Kimenő teljesítmény a front elvonulásakor
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Idő
kW
TúrkeveMoson
Győr
FolyásAgárd
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)
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:00
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:00
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:00
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:00
8:20
:00
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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
Óbuda UniversityPower System Department
Correlation analysis of wind measurements
Wind basics - Patra, 2012 70
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?
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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
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.
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Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Characteristics based on pure measurements
?
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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.
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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
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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
Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Back to the measurements (Bükkaranyos – Folyás: 33km)
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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
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
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Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Wind power generation forecast
See WinDemo!
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Óbuda UniversityPower System Department
Wind power generation forecast
Rough:• Windspeed• CharactereisticFine• + temperature• + pressure• + humidity• + direction
CORRELATION FACTOR!
Wind basics - Patra, 2012 82
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.
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Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Remote scaling
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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.
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Óbuda UniversityPower System Department
Wind basics - Patra, 2012
Thanks for the attention!
86