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Wind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_Revised.pptWind_Turbine_L11+L12_R
Fluid Dynamic Principles to Generate Axial Induction.ppt
Fluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to Generate Axial Induction.pptFluid Dynamic Principles to G
4.1 Siraj.ppt
Fluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Generate Axial InductionFluid Dynamic Principles to Genera
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- 1. Wind Science 101 Summer 2013 REU Eugene S. Takle, Coordinator gstakle@iastate.edu 30 May 2013
- 2. Outline Global scale 3-D global circulation patterns and wind energy Surface and upper-air tropical and mid-latitude weather systems, including prevailing westerlies Mesoscale Great Plains Low-Level Jet and nocturnal LLJs Sea-breeze Monsoon circulation Off-shore resources US wind resource maps Forecasting wind resources Atmospheric boundary layer Structure and diurnal/seasonal evolution Impact of static and dynamic stability on horizontal wind speeds and vertical profiles Turbulent flows and interactive wakes
- 5. http://eesc.columbia.edu/courses/ees/climate/lectures/gen_circ/index.html Differential Gain and Loss of Energy from the Earth System
- 6. Not to scale! Mean radius of the earth: 6371 km Height of the troposphere: 0-7 km at poles 20 km at Equator 90% of atmosphere is in the lowest 15 miles (24 km) 99% in lowest 30 miles (48 km) Non-Rotating Earth Heated at its Equator
- 7. Rotating Planet: Coriolis Force Fc = -2ΩxV Coriolis Force Ω
- 11. Global Circulation Revealed in Global Precipitation Patterns
- 13. Global Average Vertical Temperature Structure
- 14. To bring air from outside an airplane flying at 35,000 ft into the cabin, the compression to sea- level pressure would raise the air temperature to 430oC or 806oF Global Average Vertical Temperature Structure
- 16. Jet Stream Forms at the Boundary of Air Masses
- 18. Instabilities at Air Mass Boundaries
- 19. NOAA NCEP-NCAR CDAS-1 MONTHLY Diagnostic above_ground [ u , v ] climatology (m/s) January http://eesc.columbia.edu/courses/ees/climate/lectures/gen_circ/300mbWinds.html Wind speed near surface Upper-Level Winds
- 20. NOAA NCEP-NCAR CDAS-1 MONTHLY Diagnostic above_ground [ u , v ] climatology (m/s) July http://eesc.columbia.edu/courses/ees/climate/lectures/gen_circ/300mbWinds.html Wind speed near surface Upper-Level Winds
- 21. NOAA NCEP-NCAR CDAS-1 DAILY 300 mb height (m) and winds (m/s) 1 Apr 1997 http://eesc.columbia.edu/courses/ees/climate/lectures/gen_circ/300mbWinds.html Upper-Level Winds
- 22. NOAA NCEP-NCAR CDAS-1 MONTHLY 300 mb [ u , v ] climatology January Wind speed at 12 km Upper-Level Winds
- 23. NOAA NCEP-NCAR CDAS-1 MONTHLY 300 mb [ u , v ] climatology July http://eesc.columbia.edu/courses/ees/climate/lectures/gen_circ/300mbWinds.html Wind speed at 12 km Upper-Level Winds
- 24. Continental and Regional influences • Continental scale circulation, jet streams • Great Plains Low-Level Jet • Coastal Jets • Sea breezes • Mountain-valley flows • Mountain compression of stream lines • Monsoons • Off-shore wind
- 25. 500 mb 6 km Coupling Surface Flow to Upper-Level Flow
- 26. Mechanism of Regional Jets: Great Plains Low-Level Jet (GPLLJ) Nocturnal Low-Level Jet (LLJ) Coastal Jet (CJ)
- 27. Mechanism of Regional Jets: Great Plains Low-Level Jet (GPLLJ) Nocturnal Low-Level Jet (LLJ) Coastal Jet (CJ)
- 29. H L Pressure Gradient Fc Fp Fc = -2ΩxV Coriolis Force
- 32. H L Fp Fc V Ff Frictional Force Ff = -CdvV
- 33. H L Fp Fc V At night, friction is eliminated, flow is accelerated, V increases
- 34. H L Fp Fc V Coriolis force increase, wind vector rotates and speed continues to increase
- 35. H L Fp Fc V Vg Wind vector rotates and speed continues to increase and exceeds geostrophic wind
- 36. High Low Bermuda High Leads to Southerly Flow over the Great Plains
- 37. Rocky Mountains Missouri River High Temp Low Temp Low Press High Press X Great Plains Low-Level Jet
- 38. Simulation of the Great Plains Low-Level Jet. Adam Deppe thesis, Iowa State University, 2010 Measured wind speed Height (m) Wind Speed (m/s) GPLLJ Max
- 39. Mechanism of Regional Jets: Great Plains Low-Level Jet (GPLLJ) Nocturnal Low-Level Jet (LLJ) Coastal Jet (CJ)
- 40. High Temp Low Temp Low Press High Press Nebraska Illinois ~500 m X Nocturnal Low-Level Jet Nocturnal Low-Level Jet (LLJ)
- 41. Height above ground Horizontal wind speed Nocturnal Jet Maximum (~500 m above ground)
- 42. Mechanism of Regional Jets Great Plains Low-Level Jet (GPLLJ) Nocturnal Low-Level Jet (LLJ) Coastal Jet (CJ)
- 43. High Temp Low Temp Low Press High Press Coastal Jet (CJ)
- 44. Coastal Mountains High Temp Low Temp Low Press High Press Coastal Jet (CJ)
- 45. H L Fp Fc V Ff Frictional Force Ff = -CdvV Mountains produce an additional pressure force
- 46. Take Home Messages • Winds are created by horizontal temperature difference (which create density differences and hence pressure difference) • Rotation of the Earth creates bands of high winds (prevailing westerlies) at mid-latitudes • Interactions with the day-night heating and cooling of the earth’s surface create changes in the vertical structure of the horizontal wind • Orographic feature (coastal regions, mountains, etc) create local circulations that enhance or decrease wind speeds
- 47. 100 km
- 49. Musial, W., and B. Ram, 2010: Large-scale Offshore Wind Power in the United States. Assessment of Opportunities and Barriers. NREL/TP-500-40745. 240 pp. [Available online at http://www.osti.gov/bridge]
- 52. Musial, W., and B. Ram, 2010: Large-scale Offshore Wind Power in the United States. Assessment of Opportunities and Barriers. NREL/TP-500-40745. 240 pp. [Available online at http://www.osti.gov/bridge]
- 53. Musial, W., and B. Ram, 2010: Large-scale Offshore Wind Power in the United States. Assessment of Opportunities and Barriers. NREL/TP-500-40745. 240 pp. [Available online at http://www.osti.gov/bridge]
- 59. Takle, E. S., 1975: Wind and Wind Energy in Iowa. Report to the Iowa Energy Council. 99 pp.
- 61. Height (z) Windspeed u2 u1 = z2 z1 æ è ç ö ø ÷ 1 7 u = u* k ln z zo æ è ç ö ø ÷ Power Law Logarithmic Dependence U* = friction velocity k = von Karman’s constant (0.40) zo= roughness length
- 63. Number of Occurrences Winspeed (m/s) 2 10 8 6 4 12 14 16 18 20 22
- 64. Power law distribution Typically p is taken to be 1/7 = 0.143
- 65. Weibull Function
- 67. Number of Occurrences Winspeed (m/s) 2 10 8 6 4 12 14 16 18 20 22
- 70. 2 2.4 2.8 3.2 3.6 4 4.4 4.8 5.2 5.6 6 6.4 1940 1950 1960 1970 1980 1990 2000 2010 Wind Speed (m/s) Years Des Moines Annual Wind Speed
- 71. 2 2.4 2.8 3.2 3.6 4 4.4 4.8 5.2 5.6 6 6.4 6.8 7.2 1947 1957 1967 1977 1987 2000 2010 Wind Speed (m/s) Years Sioux City Annual Wind Speed
- 72. 2 2.4 2.8 3.2 3.6 4 4.4 4.8 5.2 5.6 6 6.4 1950 1960 1970 1980 1990 2000 2010 Wind Speed (m/s) Years Dubuque Annual Wind Speed
- 73. 0 2 4 6 8 10 12 14 N NNE ENE E ESE SSE S SSW WSW W WNW NNW Des Moines 1981-2010 Wind Roses 0 2 4 6 8 10 12 14 16 N NNE ENE E ESE SSE S SSW WSW W WNW NNW Des Moines 1951-1980 Wind Roses
- 74. 0 2 4 6 8 10 12 14 N NNE ENE E ESE SSE S SSW WSW W WNW NNW Mason City 1951-1980 Wind Roses 0 2 4 6 8 10 12 14 N NNE ENE E ESE SSE S SSW WSW W WNW NNW Mason City 1981-2010 Wind Roses