# Shared Flashcard Set

## Details

Wind Science Final
Wind Science Final
88
Geography
03/24/2010

Term
 Fractional Speed-up Ratio
Definition
 Ss = [uz - Uz]/Uz -Where uz is the wnd speed at heigh z, and Uz i the wind speed at height z on the reference anemometer.   zo (aerodynamic roughess length) decreases as surface becomes smoother. It is around 0.5m in a town, around 0.05m in a field, and around 0.0001m over water. --how quickly wind speed increases with height (lower value means quicker increase)   Different roughnesses have different effects on roughness at surface (where effect is greatest), but all lines meet and equal at the PBL (plenetary boundary layer)
Term
 Wind and Topography
Definition
 Hill Flow passing over a hill, stream lines come closer together above the hill (speed up flow) -compressed into this space.   Relative speed up graph (of wind going over a hill) looks like a hill, with disance on x-axis, and the top of the relative speed hill being at 0m from distance of hill crest.   Therefore, ideal spot for a turbine is at the hill crest. Turbulence levels in the lee of the hill would have disastrous consequences for turbines, as relative speed is significantly reduces (shooting wind over crest)   Altering shape of hill/obstruction changes lee and before hill effect. (Taller the hill, longer recovery time).   vertical velocity is greatest directly in lee, and lowest at the crest.   Valley -relative velocity greatest in immediate lee of valley -lowest in middle of depression -upwind edge has fractional speed-up ratio of slightly higher than 0 (0.2), though downwind is significantly higher (0.6-0.8). -Centre is around -0.4   -Greatest erosion occurs at upwind edge -greatest deposition occurs in lee of downwind edge and on the upwind valley slope.
Term
 Relative speed up
Definition
 Relative speedup = uz/Uz
Term
 Wind Power Estimation
Definition
 WP = u3 OR WP= (0.5)*(pa)*(u3)   Often the cube of wind speed is used as a simple estimate of wind power. Inclusion of air density(kg/m3, varies with temperature and time) and a constant provides a  better estimation
Term
 Cubic Power Law
Definition
 Relation between the wind speed and power. Wind power rises as a power function (no pun) relative to wind speed. I.E. as wind speed increases, wind power increases faster.
Term
Definition
 WP = (0.5)*(pa)*(A)*(u3) Where A is the swept area of the turbine (m2)   A is given by (pi)(r2)   The world's largest wind turbine generator has a rotor blade radius of 63m and so the rotors sweep an area of about 12470m2. If we use an air density value of 1.23kg/m3 and a wind speed of 14 m/s we get:   WP= 0.5*1.23*12,470*(143)=21,000,000 watts (21 MW)   **As temperature increases, density decreases in an approximately linear manner   ****Wind power on a really hot day is way less than on a really cold day!!!! (+35C vs -30C = 5MW difference in above turbine)   **What is the Betz Limit??
Term
 Wind Metrics
Definition
 -Turbulence and gusts -Shear stress and shear velocity -Drag coefficient -Wind Direction (wind rose)
Term
 Turbulence
Definition
 The turbulent variations of the wind speed are typically expressed in terms of teh standard deviation, (σu), of velocity fluctuations measured over 10 to 60 minutes, normalized by the wind speed.   The Tubulence Intensity, Iu, is a widely used measure when neutral conditions persis with a logarithmic wind profile over at terain. Turbulence intensity may be derived from:   Iu= (σu)/U   (Dynamic TI) Iu= 1/ln(z/zo) (z-dependent TI)   Typical values of Iu for neutral conditions in different terrains are: Flat/Open grassland: 13% Sea: 8% Complex terrain: 20% or more So.... increasing terrain complexity results in greater turbulence intensity
Term
 Shear Stress
Definition
 stress= force per unit area   Wind shear stress is the force (per unit area) exerted by the moving fluid (air) on an object or surface. The equation for shear stress is given by:   τ= pau*2   Where pz is the density of the fluid (air) in kg/m3, and u* is the shear velocity of the moving fluid, usually measured in m/s   We cannot measure the fluid shear stress directly so we must use surrogate measurements to resolve it.   Why does shear stress matter in wind science?? -Resolves stresses acting on structures -Determines sediment/snow transport -Stresses acting on turbines   **THINGS MOVE AND DEFORM IN RESPONSE TO STRESS
Term
 Air density
Definition
 pa= -0.0047(temp.) +1.2976
Term
 Shear velocity
Definition
 u* (aka friction velocity)   Shear velocity relates the difference of wind velocity at two heights   shear velocity = k(Uz2-Uz1)/ln(Z2-Z1) Were Z1 is below Z2, so that Uz1 is less than Uz2   When calculating shear stress, assume density is 1.22kg/m3   Shear velocity tends to fluctuate between 0 and 1
Term
 Drag Coefficient
Definition
 The drag coefficient is a dimensionless quantity which is used to quantify the drag or resistance of an object in a fluid environment such as air or water.   Cz = (u*/Uz)2   Where Cz - the drag coefficient at height Z   Values usually around 0.002-0.010 ish -not much variation at a given height (shear velocity varies more)
Term
 Global Energy Sources
Definition
 All sources approx 94 quadrillion BTU -One British Thermal Unit is the heat that will raise the temp of one pound of water by one degree F. Approximately the amount of heat generated by burning one kitchen match. One BTU = 1054 Joules = 0.000293 kWh   39% Petroeum 23% Natural Gas 23% Coal 8% Nuclear Electric 8% Renewable -50% hydro -43% biomass -5% geothermal -1% solar   Oil discovery is on a trend of decrease, while production is on a trend of increase. Conventional Oil reserves are mostly in middle east gulf, then in Eurasia.   What to do after the end of cheap energy? -last one standing: the way of war and competition -powerdown: the path of self-limitation -waiting for the magic elixir: false hopes, wishful thinking, and denial -building lifeboats: the path of community   What's the hold-up with renewable energy sources like wind? -electricity in North America is extremely cheap (no incentive) -the grid cannot take it -storage   As for wind energy, Can is 11th in world, with installed capacity of 2,369MW. America is first
Term
 Global Wind Power
Definition
 The most comprehensive study to date found the potential of wind power on land and near-shore to be 72TW, equivalent to 54000 Million tons of oil equivalent (MToE) per year, or over five times the world's current energy use in all forms.   The potential takes into account only locations with mean annual wind speeds greater than 6.9m/s at 80m. It assumes 6 turbines per square km for 77m diameter, 1.5 MW turbines on roughly 12% of the total global land area.   Renewable energy sources in Canada consist mainly of wind and hydroelectric. Interestingly enough, electricity production of these two sources alternate according to seasons: -hydro usefullness peaks in summer, while wind peaks in winter, and the yearly average is pretty much right in between.
Term
 Brief History of Turbines
Definition
 1600s - Windmills in the Neterlands, pumping water and grinding grains   1888 - Charles Brush develops first large wind generator producing 12kW   Early 1900s - Windmills drive pumps and generators across rural North America   1941 - first prototype turbine (Putnam's 1.25 MW turbine) - also demonstrates need for lighter materials
Term
 Primary Components of a Turbine Common on Canadian Wind Farms
Definition
 1)Blade 2)Rotor Hub 3)Pitch Cylinder (in front of rotor hub) 4)Main shaft 5)Gear Box 6)Generator 7)Transformer   The torque shaft integrates with gears in some turbines. The gears connect to another shaft that turns a coil within the generator.
Term
 How do you get electricity from the wind?
Definition
 Most generators have a long, coiled wire on their shafs surrounded by a giant magnet.   When the turbine turns, the shaft and rotor is turned. As the shaft inside the generator turns, an electric current is produced in the wire. The electric generator is converting mechanical, moving energy into electrical energy.   The generator is based on the principle of "electromagnetic induction" discovered in 1831 by Michael Faraday, a British scientist. Faraday discovered that if an electric conductor, like a copper wire, is moved through a magnetic field, electric current wil flow of "be induced" in the conductor. So the mechanical energy of the moving wire is converted into the elecric energy of the current that flows in the wire.
Term
 Start to finish: a wind farm typically takes 12-36 months
Definition
 1)Land acquisition 2)Resource analysis 3)Envioronmental work (EIA) 4)Interconnection 5)Permiting & Public Consultation 6)Secure Equipment 7)Construction 8)Commissioning   Steps 2, 3, 5, 7 typically take the longest.
Term
 Cowley Ridge
Definition
 The Cowley Ridge Wind Plant is the first commercial wind plant in Canada. Phase One was commissioned in 1993 and Phase Two in 1994.   Easily seen off Highway 3 from the town of Cowley, the wind plant features 57 Kenetech turbines, with a total capacity of 21.4 MW. Average production from this wind plant is more than 60 million kWh of electricity per year, which is enough to power 8,400 typical Canadian households.   The wind turbines at Cowley Ridge are mounted on 24.5 metre lattice towers and operate at wind speeds of up to 97 kilometres per hour. Each turbine has three blades and rotors that are 33 metres in diameter. Rotor diameter started at around 20m, is currently around 100 meters, and is projected to reach nearly 140 meters in offshore plants by 2015
Term
 The Betz Limit
Definition
 Albert Betz was a german physicist who concluded that no wind turbine can convert more than 59.3% of the kinetic energy of the wind into mechanical energy turning a rotor.   Wind turbines extract energy by slowing down the wind. For a wind turbine to be 100% efficient it would need to stop 100% of the wind – a theoretical impossibility   The theoretical maximum power efficiency of any wind turbine is 0.59 (i.e. no more than 59% of the energy carried by the wind can be extracted by a wind turbine).   Once you also factor in other aerodynamic inefficiencies the limit is well below the theoretical Betz Limit with values of 30% common even in the best designed wind turbines. Even less power is available when gearing, controls and other components of turbines are considered. Thus, in most cases only 10-30% of the power of the wind is ever actually converted into usable electricity.   Conversion to electricity is 70% of the 60% that is not spilled.
Term
 Power of Wind and Energy Harvested
Definition
 Theoretically, power increases exponentially with wind speed, yet in reality power levels out at a certain windspeed much sooner.   The energy potential per second (the power) varies in proportion to the cube (the third power) of the wind speed, and in proportion to the density of the air.   Turbine output effectively increases with the length of rotors (swept area)   Large rotor radius (63m) WP= 0.5*1.23*12,470*(14^3) = 21,000,000W   Small radius (20m) WP = 0.5*1.23*1256*(14^3) = 2,100,000W (10x less)   Rotor Radius vs Power is a (power/log/exp?) curve -Lec13/sl30
Term
 Reasons for choosing Large Turbines
Definition
 -Larger machines are usually able to deliver electricity at a lower cost than smaller machines. The reason is that the cost of foundations, road building, electrical grid connection, plus a number of components in the turbine (the electronic control system etc.), are somewhat independent of the size of the machine. - -Larger machines are particularly well suited for offshore wind power. The cost of foundations does not rise in proportion to the size of the machine, and maintenance costs are largely independent of the size of the machine. - -In areas where it is difficult to find sites for more than a single turbine, a large turbine with a tall tower uses the existing wind resource more efficiently.
Term
 Reasons for choosing small turbines
Definition
 -The local electrical grid may be too weak to handle the electricity output from a large machine. This may be the case in remote parts of the electrical grid with low population density and little electricity consumption in the area. - -There is less fluctuation in the electricity output from a wind park consisting of a number of smaller machines, since wind fluctuations occur randomly, and therefore tend to cancel out. - -The cost of using large cranes, and building a road strong enough to carry the turbine components may make smaller machines more economic in some areas. - -Several smaller machines spread the risk in case of temporary machine failure, e.g. due to lightning strikes. - -Aesthetical landscape considerations may sometimes dictate the use of smaller machines. Large machines, however, will usually have a much lower rotational speed, which means that one large machine really does not attract as much attention as many small, fast moving rotors.
Term
 Theoretical Wind Power Curve: key features and terms
Definition
 -now power vs windspeed for a while until "cut-in" speed is reached -gradual incline to (carrying capacity graph) peak output -steady here until cut-out of furling speed   furling: the process of forcing, either manually or automatically, the blades of a wind turbine out of the direction of the wind in order to stop the blades from turning. Furling works by decreasing the angle of attack, which reduces the induced drag from the lift of the rotor, as well as the cross-section. A fully furled turbine blade, when stopped, has the edge of the blade facing into the wind.    cut-in speed: the lowest wind speed at which a wind turbine begins producing useable power.   cut-out speed: the highest wind speed at which a wind turbine stops producing power
Term
 Why not an even number of blades?
Definition
 The most important reason is the stability of the turbine. A rotor with an odd number of rotor blades (and at least three blades) can be considered to be similar to a disc when calculating the dynamic properties of the machine.   A rotor with an even number of blades will give stability problems for a machine with a stiff structure. The reason is that at the very moment when the uppermost blade bends backwards, because it gets the maximum power from the wind, the lowermost blade passes into the wind shade in front of the tower.
Term
Definition
 The wind passes over both surfaces of the airfoil-shaped blade, but passes more rapidly over the longer (upper) side of the airfoil, thus creating a lower-ressure area above the airfoil. The pressure differential b/w top and bottom surfaces results in aerodynamic lift.
Term
 Other types of turbine
Definition
Term
 Wind Resource Assessment
Definition
 1)Climatology and Meteorology   2)Quality site plan   3)Energy estimates   4)Economic feasibility     *A change in speed from 12mph to 11mph can lead to a 33% decrease in the energy available in the wind!   CRITICAL TO MONITOR! technical reasons: -wind shear -turbulence -inflow winds -extreme winds/gusts -site design -wake effects   Needed for: -turbine manufacturers and foundation design
Term
 Wind Resource Assessment (Met Tower)
Definition
 Wind is Site Specific!   Met Tower -Wind speed (2 per level on tower) -Wind Direction -Different heights -temperature, pressure -data linked via data logger and cellular to internet connection   Goal: Estimate the energy at the hub height of the wind turbine! -50-60m tall -5x4 steel guy wires -lifted using 'gin pole'   -when evaluating... must have data management -check for errors (sensor failure, missing data, icing, etc)   -want to have it up for a year -inter-annual variation -annual average wind speed -other averages   *Seasonal changes in wind speed are not spatially uniform! (increases in some areas, decreases in others)   Describe wind with a wind speed distribution histogram -wind tends to be around 6-8m/s most of the time. -graph is %time vs wind speed categories   Look at inter-annual variation if possible
Term
 Time series analysis - WHY?
Definition
 To determine range of conditions (at different temporal scales) that occur at the site (how much variation around the mean?)   To determine worst case scenarios (is the site prone to frequent episodes of extremely high winds that might damage the turbine?)   To determine how variable the wind is at different scales (is it more variable during peak demand periods than outside these periods?)   * need lots of recording sites! Data does not correlate if far away
Term
 Roughness
Definition
 WHAT IS ROUGHNESS? -Roughness is considered to be any element that alters wind from its original flow -exists at many scales from micro topographic features (ripples on sand dunes), to land form scale (entire dune)   WHAT DOES ROUGHNESS DO? -extracts momentum -producing turbulence in the form of wakes behind obstacles -breaking down large-cale turbulent eddies into smaller scale motions   FACTORS AFFECTING ROUGHNESS The gradient of the velocity profile within the roughness sub-layer is related to several roughness element length scales: -height -width -spacing -density -geometry
Term
Definition
 WIND EROSIONShear stress partitioning -when the soil surface is obstructed by roughness elements the total force (Fo) of the wind is partitioned b/w the roughness elements (Fr) and the intervening bare soil (Fg): Fo=Fr+Fg -relevant for the fact we must know how much force is extracted by the roughness elements in order to determine how much force is still available to entrain particles.   WIND DEPOSITION Blowing snow/drifting Moisture Capture   WIND POWERAffect on wind speed Roughness elements cause turbulent unstable flow -turbine location selection   MODELLING Atmospheric modelling Pollution modelling
Term
 Roughness Effects on Wind
Definition
 •Flow in the inertial sublayer, over a smooth surface and thermally neutral air follows a logarithmic increase with height (z) above the surface: •In the presence of roughness elements flow is altered, shifting the logarithmic profile upwards (d).  •Aerodynamic surface roughness (zo) is the height at which horizontal velocity is zero. On a perfectly flat surface, the value of zo depends on the grain size of sediment at the surface.
Term
 Flow Regimes
Definition
 Roughness density has a large affect on how wind articulates over the surface. Different densities create different flow regimes, affecting dependants such as wind erosion and particle movement.   -isolated roughness flow -wake interference flow -skimming flow
Term
 Describing roughness
Definition
 Many ways to characterize roughness..   Field measurements -wind profiles -physical measurements   Remote Sensing -laser scanning -LiDAR/Laser Altimetry -Radar
Term
 Field Measurements used to describe roughness
Definition
 The use of anemometers setup at specified intervals demonstrate the roughness length of the roughenss features in the derived wind profile from the gathered data.   Frontal Area Index Defined as Lc=La/SA La is the silhouette area (breadth*height), SA is defined as the number of roughness elements divided by the sample area. With the frontal area index calculated, roughness for sparse array of vegetation can then be calculated through the use of the formula: zo= 0.5hLc Where h is the mean height of the roughness elements.   PROBLEMS associated with field measurements: -How accurate of a representation was obtained through sampling? -Time consuming, field work is expensive to conduct -Measurements often generalize the roughness element.
Term
 Remote Sensing used to describe roughness
Definition
 The LIDAR instrument consists of a system controller and a transmitter and receiver Scanning Mirror sweeps laser beam across the ground. Range to target is determined by measuring the time interval b/w transmission and return of reflected laser pulse. Aircraft position is determined using GPS phase differencing techniques.   LIDAR systems can emit pulses at rates greater than 100k pulses per second referred to as pulse repetition frequency. A pulse of laser light travels at c, the speed of light (3x 108 m/s). LIDAR technology is based on the accurate measurement of the laser pulse travel time from the transmitter to the target and back to the receiver. The traveling time of a pulse of light, t, is:   R=0.5tc   Where R is the range (distance) b/w the LIDAR sensor and the object.   LIDAR/Laser Altimetry -Holland et al. using LiDAR to characterise roughness of urban areas -extract parameters from the LiDAR data required to calculate roughness. zo = 0.5hLc -Filters, creation of raster datasets, feature extraction.   Good for large roughness elements, ineffective for smaller vegetation types (resolution isn't great enough)     Optical Techniques Jansinki and Crago 1999 use canopy area density (total single sided area of all the canoy elements per unit ground area) as a surrogate for the frontal area index in order to determine roughness -generalizations start to be made about stand characteristics -used assumed stand averages and assuming stand homogeneity   Radar -determined relationships between zo and backscatter   LASER SCANNING Same principls as LiDAR Data similar to LiDAR pint cloud data (X,Y,Z) Currently being used for soil surface roughness (physical roughness not aerodynamic roughness) -characterizng surface roughness using RMSH -quantifies the deviation from the mean -Higher RMSH the rougher the surface (look at formula for this)   Have not came across a study using laser scanning to quantify aerodynamic roughness   Benefits of laser scanning: -very high quality data (point cloud resolutions in the order of mm scale) -relatively inexpensive as compared to LiDAR data -no generalization of features -ability to capture very fine features   Drawbacks: -robust datasets -area coverage is somewhat limited -no first and last return data (unlike LiDAR)
Term
 Owen's Research
Definition
 qCurrent methods of determining roughness contain vast generalization, along with many assumptions. qDevelop a methodology to determine accurate representations of roughness. ¨Use of laser scanning to collect data, along with anemometers to develop wind profiles. ¨Creating filtering algorithms to separate ground points from the point cloud. Conduct analysis on separated point clouds. qSurface roughness derivation. qLess complex features (e.g. rocks, soil). qMore complex features (e.g. vegetation). qApplication of methodology to a sand dune environment. qDetermine aerodynamic roughness from extracted parameters, using the wind profile data collected at each scan site. qLook for other ways to describe roughness from the data. Investigate the relationship between RMSH and Zo ¨Determine the best possible method for quantifying roughness ¨Finally apply the developed methodology to a sand dune environment. ¤Scans will be collected over a growing season as vegetation changes. ¤How does this affect the sand dune? nSediment flux nEssential for dune activity
Term
 CanWEA
Definition
 CanWEA is the national association for Canada's wind energy industry (advocacy, communication, education) Represent 340 corporate members -Turbine Manufacturers (GE) -Component Manufacturers (Hitachi) -Project Owners/Developers (Suncor, TransAlta) -Utilities (Hydro Quebec) -Service Providers (Jacques Whitford)   -installed wind capacity is increasing on a yearly basis in Canada
Term
 Future Prospects for Wind Energy
Definition
 1,856MW of installed capacity in Canada Close to 3000MW of signed power purchase agreements in place with construction immanent More than 3000MW of additional power purchase agreements to be signed in 2008 *Quebec is leading the way*   Provincials objectives now represent a minimum of 12000MW by 2016 -Ontario 4600 by 2020 -Quebec 4,500 by 2016 -Alberta examining transmision options for 2000-3000MW -Manitoba 1000MW by 2017 -BC and Labrador have large untapped potential   12,000MW of wind energy in 2016 would: -serve 3.6 million Canadian homes annually -meet 5% of Canada's total electricity demand -represent 30+% of electricity produced from new facilities constructed in 2005-2015 -represent a \$20+ billion investment (2005-2015) -reduce GHG emissions by 9million tonnes/yr   But.. this only scratches the surface of Canada's wind energy potential     ***** Alberta has most installed potential, with Ontario right behind, and Quebec very close in third -AB is frozen... Quebec making HUGE advances   Canadian current installed capacity is 1856MW   AB leading windfarms are Pincher Creek (43%), Willow Creek (29%), Taber (21%)
Term
 Environmental Impact of 100MW Windfarm
Definition
 Electricity Output -Example: a 100MW windfarm averaging 35% capacity -Output = Generation MW x 8760 hours x  % Capacity Factor -100x8760x0.35 - 306,600MWh per year   Households Served -Number of Average Households = Output/7.2MWh -306,600/7.2MWh = 42,580 hourholds -supple enough electricity for over 42000 households   Emissions Displaced -GHG emissions are 0.7 tonnes per MWh -Emissions = electricity output x 0.7 -100MW x 8760 x 0.35 x 0.7 = 214,620 tonnes CO2 -Displace approximately 215,000 tonnes of CO2 or GHG emissions per year   Cars Taken Off the Road -Annually produce approximately 4.78 tonnes of CO2 emissions -Number of Cars = emissions displaced/4.78 -215000/4.78 = 44,979 -Equivalent of taking approximately 45,000 cars off the road each year
Term
 Rural Issues and Development (and how wind plays a role)
Definition
 RURAL ISSUES Low farm commodity prices High farm input costs -fuel prices high and uncertain -high fertilizer prices -lubricants -equipment -high land costs Economic development and diversification Eroding local property tax base Migration of people to cities -hollowing out 20-50 age range Eroding services -healthcare -education -policing Water shortages and drought Forestry:softwood lumber/prices Cattle: BSE/border closing/prices   ECONOMIC DEVELOPMENT Exploration -Landowner payments   Construction -employment -services -windfarm, interconnection, transmission   Operations -employment -services -windfarm, interconnection, transmission -property tax payments -landowner payments   Tourism   LOCAL ECONOMIC IMPACT OF WINDFARM CONSTRUCT. 100MW/500MW Construction 25jobs/125jobs Operations 10jobs/50jobs Property taxes annual 900,000/... landowner royalties annual 400,000/... *the above does not include indirect employment   MD of Pincher Creek Tax Revenues -several groups (transAlta wind, etc) -upwards of 1.5 million dollars per year
Term
 Leasing Wind Lands
Definition
 -Enter into option-to-lease /w landowners ---monitor wind resource, conduct studies -Enter into long-term lease with landowner when windfarm is to be built -No 'right of eminent domain' like subsurface in AB - wind similar to freehold rights - on land by invitation -Landowner receives a royalty based on energy production or per turbine or combination of the two -Royalty is 'Second Cash Crop' - no inputs -Very low impact on operations whether pasture or cultivated ---small footprint ~15m2 per turbine (0.004 acre) ---windfarm footprint uses only 1-2% of land -Complements 'stewardship' approach of many farmers and ranchers -preserves agricultural land and way of life   SETBACKS Setbacks are established to deal with four issues: 1)safety 2)sound 3)environmental impacts 4)communication and Radar Interference   Science and best practices are used to develop a range of setback distances. There is no template or "one size fits all".
Term
 Public Safety
Definition
 Studies into ice shedding and blade failure conclude that risks to objects or individuals directly drop off significantly with increasing distance from the turbine itself.   CanWEA recommmends a distance of blade length plus 10m from public roads, nonparticipating property lines and other developments in an Ontario application   Ice throwing!! -most fragments are small and don't go very far.   AUDIBLE SOUD What concerns are raised: -"turbines emit a horrendous noise that makes it impossible to live anywhere near them"   What we know: -wind turbines do produce sound "swoosh" -actual sound level is influenced by many factors including the type of turbine, wind speed, surrounded topography -Sound often masked by surroundin environment   How we address these concerns: -All projects must meet regulatory requirements -CanWEA Best Practices based on acceptable sound levels outside a dwelling: 40dBA at 4m/s rising to 53dBA at 11m/s (reflects fact that ambient sound tends to rise with wind speed) -Typical resulting separation distances are generally 300-600m (can be less for participating landowners)
Term
 Visual Effects of Windmills
Definition
Term
 CanWEA Response to concerns about wind energy
Definition
Term
 Aeolian sediment transport threshold
Definition
 The minimum wind speed to initiate sediment transport by wind (ut or u*t) It is a critical parameter because it establishes the wind speed above which transport is possible. Due to a number of surface conditions (moisture, temperature, vegetation, bed slope, and crusting) threshold is known to vary over a range of spatial and temporal scales. Much of the focus of threshold research is to resolve the influence of these external controls and thereby increase the accuracy of sediment transport models. Currently, there are a variety of methods and instruments used to measure or derive threshold, but it is now apparent that the application of different methods and instruments imposes ambiguity in the definition of threshold.
Term
 Four forces act on a grain:
Definition
 Lift Drag Gravity Cohesion   The relative magnitude of each force and the grain position relative to other grains is used to derive the fluid threshold for sediment transport.
Term
 Impact and Fluid Thresholds
Definition
 Commonly the impact and fluid thresholds are each defined as a single wind speed (or shear).  However, most sediments are composed of a range of grain sizes and shapes. Thus, for a given surface, variability is expected in the positioning of sediment grains. Because the positioning of grains affects their susceptibility to entrainment, the fluid or impact threshold for a given surface is not easily described only by one number. This has been demonstrated in wind tunnel studies where the measured fluid and impact thresholds could not be reproduced, presumably because it is impossible to replicate grain positioning in each test. As a solution, threshold is best defined as a statistical phenomenon, or as two probability distributions (for the fluid and impact thresholds). The distributions describe the probability of a given threshold value occurring for a sediment surface.   Fluid threshold occurs at a higher wind speed than impact threshold.
Term
 Three approaches to the determination of threshold:
Definition
 1)Grain Scale Sediment transport of particles is reduced to the forces acting on grains and solved mathematically Commonly the bed is simplified as a population of spherical grains of constant size, and the wind is represented as a constant velocity There is disagreement over the relative magnitude of lift and drag forces – this is important because it defines the initial movement of grains.     Observations from Chepil (1959) and Bagnold (1941, 1965) indicate grains slide along the bed prior to sediment transport. Contrarily, results from Bisal and Nielson (1962) and Lyles and Krauss (1971) suggest grains lift off vertically under the influence of lift forces. While the exact mechanism is yet unresolved, it is likely that both processes occur in tandem     Bagnold’s (1941) seminal work showed the presence of two quantifiable thresholds: (i) the minimum wind speed for initiation of sediment transport without antecedent sediment transport, or fluid threshold, and (ii) the minimum wind speed for sustaining sediment transport with the presence of sediment transport, or impact threshold. His data suggest that the impact threshold is approximately 80% of the fluid threshold (Bagnold, 1941). This difference is attributed to the positive feedback wherein the presence of impacting grains ejects more grains into the airstream, thereby sustaining the process at a lower wind speed than that required to initiate grain transport 2)Conrolled Experiment/Setting Quantification of threshold in controlled settings (wind tunnels) requires that wind speed and sediment transport are measured simultaneously The fluid threshold is denoted by the wind speed corresponding to the first measured instance of sediment transport, while the impact threshold is denoted by the wind speed corresponding to the last measured instance of sediment transport as wind speed decreases u is commonly measured with pitot tubes or thermal anemometers – these instruments are situated close to the bed (typically 1 cm or lower) and report instantaneous measurements of wind speed at discrete times. The onset of sediment transport is recorded by visual observation, high-speed camera monitoring equipment, impact sensors, or laser based detection systems. The reductionism inherent in wind tunnels has both advantages and disadvantages. Precise results are possible when the controls of threshold variability can be examined in isolation. However, wind tunnels do not reproduce the turbulent fluctuations in wind speed present in natural settings. Furthermore, reproducing natural surfaces in controlled settings is difficult, thereby challenging the representativeness of wind tunnel experiments 3)Uncontroled experiment   An approach where threshold is measured in the field under natural wind and surface conditions. Due to turbulent fluctuations in the wind speed, sediment transport observed in the field is often intermittent. Threshold wind speed (fluid or impact) is surpassed every instance sediment transport begins or ends. Thus, when sediment transport is intermittent, threshold can be determined repeatedly by measuring the wind speed corresponding to the onset and termination of sediment transport bursts. Advances in datalogger technology and electronic sediment transport sensors have made this approach more popular in recent decades. These technological advances allow investigators to monitor threshold continuously at unattended sites.
Term
 The most common grain-scale formula (Bagnold, 1941, p86)
Definition
 u*t = A(SQRT(((pp-pa)gD)/pa)   where A is an empirical coefficient (0.1 for fluid threshold, 0.08 for impact threshold); pp is the density of quartz sand particles (2.65 × 103 kg m-3); pa is air density (1.22 kg m-3); g is gravitational acceleration (9.81 m s-2); and D is sand grain diameter at study area (0.25 × 10-3 m). These values give an impact threshold of 0.231 m s-1
Term
 What is the calculated threshold?
Definition
 5.6 m/s for bare, dry sand.   bridging: interstitial pore water... cohesion   Entrainment Threshold Seasonal and spatial changes in surface conditions (moisture, vegetation, ground freezing) complicate prediction of wind speed required to entrain soil.   Determining threshold in the field withprecision instruments. Sometimes thresholds remain constant over time, while some increase/decrease depending on what is exposed. For example, threshold increases as moist sand is exposed.
Term
 A combination of factors determine southern alberta's wind erosion risk:
Definition
 High winds Sparse and low vegetation cover Fine-grained soils Aridity
Term
 Drylands and Wind Erosion - SO WHAT?
Definition
 Mainly an issue of land surface sensitivity   Dryland climates are typically associated with thin (ie. grassland) or patchy (ie. creosote) vegetation cover   These vegetation types are more readily affected b drought than forests, and more easily disturbed. Thus, drylands have increased potential for direct exposure of sediment to wind= higher susceptibility to wind erosion.   Vegetation cover is also more susceptible to natural and anthropogenic disturbances (fire, over-grazing, dought, vehicular traffic, etc.)   Dry soils are more readily entrained when exposed by agricultural tilage and land clearing during the initial phases of development.
Term
 Vegetation is an important surface control because it reduces wind erosion in 3 ways:
Definition
 1)It shelters the soil from the erosive force (shear stress) of the wind 2)It reduces the force of wind near the surface by extracting momentum from wind 3)It traps incoming soil particles - also induces deposition.   Once vegetation is removed, soil drifting potential immediately increases, then slowly decreases (finest is blown away, vegetation grows back, etc)
Term
 Seasonal competition - Wind vs Vegetation/Drifting sow
Definition
 Winds capable of eroding the ground surface (>25-30 km/h) occur most frequently when vegetation growth conditions are poorest = prime conditions for blowing soil and snow.   Many of the factors that increase southern Alberta's susceptibility to soil erosion by wind also apply to snow drifting (ie. high wind power, low vegetation cover, aridity)   Without effective roughness elements (fences, wind breaks, building design, etc) snowdrifting can, at times, exceed soil drift rates by orders of magnitude. The effects, however, are short-lived, but they also recur each year if left unattended.   Snow drifting depends on temperature, age of snow, wind speed, and heigh of snow cover above the vegetation roughness elements. As the snow age increases, the drift potential decreases.   Vegetation effectivenes decreases as snow depth increases.
Term
 Module 1 Summary: Future challenges for land development in the (windy) City of Lethbridge
Definition
 wind power is high - our research shows that it drops appreciably only in winter during strong El Nino phases (ie 1998) - otherwise dominated by modest interannual variabilitywind direction is westerly- future land development will occur on the west side, thus wind erosion challenges will persist for some time in this sectorwind power is greatest when natural surface cover is least effecive (ie. outside of growing season)- emission reduction techniques must bear this in mindSouthern AB's landscape is sensitive to disturbance - removal of vegetation cover during initial phases of land development lead to an immediate increase of soil drifting - the bulk of mitigation strategies must focus on this periodthere is a multi-fold effect of our climate that enhances soil and snow drifting - but there is direct correspondence b/w many of the natural factors that control these processes; therefore, mitigation techniques may be complimentary
Term
 Wind erosion, wind speed near ground, and threshold
Definition
 Wind speed decreases towards the ground surface as the height of roughness elements increases (momentum extraction).   It also depends on topography. Wind speed accelerates up to the crest of natural ridges or storage piles= potential for erosion. Deceleration on the lee side = potential for deposition. Artificial ridges or recesed (low-lying) areas can be used strategically to shelter some areas from the wind, but the height and profile geometry must be based on achieving maximum wind speed reduction.   Vegetation acts as a "living" wind shleter, reducing wind speed sppreciably for some distance downwind in the sheltered "wake" region. The effectiveness depends on the porosity, lateral extent, and height [H] of vegetation (flow recovery is usually 25-35 times the H)   When protective vegetation is removed, wind erosion potential increases dramatically, and emissions spike in areas with erodible soils under the right conditions. The goal ust be to limit the exposure time and extent during initial phases of land development, either through adoption of low impact processes or deployment of mitigation techniques.   Threshold wind speed decreases once the surface dries [reduced inter-particle cohesion], or once the protective cover is removed. Thus, it is imperative to ensure that development activities do not unnecessarily reduce the threshold velocity. Mitigation strategies are designed specifically to increase threshold, thereby decreasing the probability of entrainment.   As wind speed [u] increases, the amount of windblown material [q] increases [q=~u3], but there is actually some scatter because the surface conditions change [ie. frozen ground, soil moisture, vegetation growth, etc.]   The challenge for land develoment is how to minimize wind erosion under different wind conditions BUT... We don't want to set arbitrary or unrealistic goals that might be overly restrictive.   Our research shows that there is no single eqution or set of equations that give us the right answer all the time - we need to measure it in the field and develop empirical relations over a broad range of conditions.
Term
 What determines land erosivity (ie probability of threshold exceedance)?
Definition
 Soil Moisture Surface Roughness Particle size and density Air temperature Humidity Wind Turbulence Vegetation heigh and lateral cover Soil crusts Ground temperature Disturbance
Term
 Particle transport modes
Definition
 Creep (>20% of transport) -usually involves the largest particles moved by wind (0.7 - 2.5mm) -no appreciable downwind effect since most grains are trapped a short distance from where they originated by small hollows are furrows   Saltation (50-80% of transport) -particles are generally too large to mobilize more than 1m above the ground surface (0.1-0.7mm)   Suspension (20-50% of transport - considered as air pollution) -Finest particles (0.001-0.1mm) that travel the longest distance because they can bcarried high in the atmosphere -Major concern is related to inhalation of these particles (block lung alveoli and can lead to respiratory disease or enhance pre-existing conditions)   PM10 PM2.5 PM1.0   PM2.5 is less than 2.5 micrometers in diameter -human hair average 70 micrometer diameter
Term
 Canada Wide Standard for Particulate Matter
Definition
 In June 2000 the federal, provincial and territorial governments signed the Canada-Wide Standard (CWS) for PM, thereby agreeing to national ambient standards for PM2.5   Each jurisdiction is responsible for meeting the CWS and reporting on achievement once the target dates are reached. The CSW for PM must be achieved by 2010.   The CWS calls for the development and implementation of jurisdictional implementation plans as the primary mechanism for achieving the CWS, as well as programs for pollution prevention, keeping clean areas clean and continuous improvement to manage ambient levels below the CWS.   Alberta has adopted from the CWS, an AB Ambient Air Quality Objective for fine particulate matter (PM2.5) of 30 micrograms per cubic meter as a 24-hour average concentration. There is no 1-hr objective for fine particulate matter (PM2.5). However, after consultation with a multi stakeholder advisory committee, a 1-hr guideline in AB for PM2.5 was finalized at 80 micrograms per cubic meter. The guideline is based on the statistical equivalent of the CWS.   Action triggers: -mandatory plan to reduce below CWS if goes above 30micrograms or ozone above 65ppb. Below that, have management plan for over 20/58, surveillance actions for over 15, and baseline monitoring below that.   We have measured PM2.5 during blowing dust events associated with land development that exceed these values.   In one case we measured >500 micrograms/cubic meter, averaged over 24 hours. At the local level, land development policies have an important role to play in achieving the CWS.
Term
 Blowing snow effects
Definition
 Driving hazards   Accessibility (drifts blocking pedestrian mobility)   Water damage (build-up next to building - damage from melting/freezing)   Protracted snow cover (limiting spring drainage, landscaping)
Term
 How do we measure wind erosion? (snow and soil)
Definition
 Wind speed and direction   Dataloger and power   Piezoelectric sensor   Other items: -cell phone modem -digital camera -meterological sensors   Use a prototype laser particle counter to measure the onset of particle movement in the field.   Can measure concentration of windblown particles using TSI Dusttrak
Term
 What are the implications of wind erosion?
Definition
 1)Health -in addition to PM levels, there is growing realization that chemicals bonded to particles (pesticides, herbicides, etc) are translocated during wind erosion.   2)Mobility -Mainly an issue of blowing snow, but costs can be high in areas with persistent problems   3)Aesthetics -Residential cleanliness is a high priority for most home owners, including indoor air quality, but persistent build-up of soil and snow requires constant, sometimes costly maintenance.   4)Hazards -Visibility is reduced during blowing dust and snow events.
Term
 What development activities stimulate wind erosion?
Definition
Term
 Module 2 Summary
Definition
 1)Mitigation strategies have a central goal of ensuring the surface has a high wind erosion threshold   2)The most critical time for mitigation strategies is during and shortly after land clearing   3)The success of a mitigation strategy depends on our ability to measure wind erosion, particularly the dust component, which has the most significant downwind effect.   4)An overall goal is to reduce wind erosion (soil and snow) down to the background level (if not better) as quickly as possible)
Term
 Site assessment
Definition
 Identify factors that might contribute to wind erosion during land development.   soil texture - proportion of fine grained sediment (find sand and silt ractions, 100-20 micrometers), organics, chemical analysis   fetch- how exposed is the area to the prevailing wind?   wind patterns - maximum gust recurrence intervals, seasonal patterns, directional variability   proximity - of existing residential or commercial areas   road access surfaces - will construction vehicles be using paved or unpaved roads to access the site?   existing roughness condition - how effective was the pre-development land surface at trapping snow?
Term
 On-site Monitoring
Definition
 An enforceable regulation/bylaw must also contain test procedures in order to determine whether sources are in compliance   real-time meteorological data- air temperature, humidity, soil moisture, wind speed/direction, precipitation   wind erosion rates - passive dust traps (checked weekly), periodic monitoring with automated devices (Dusttrak), snowdrift rates, digital camera (atmospheric opacity)   daily record keeping - observations of dust plumes, snowdrifting, durface dryness and erodibility, activity levels, effectiveness of control measures   talk to local (downwind) residents - they know best whether things are improving or getting worse
Term
 Planning Considerations
Definition
 Planning consideration are factors to minimize downwind and peripheral effects.   timing - Initiate land clearing when the probability of negative effects is lowest (ie. summer).   site design - Optimize site layout to reduce funnelling and accumulation - ie. streets oriented parallel to prevailing wind should have wind breaks at their open end.   building design - how to avoid creating local depositional areas for snowdrift accumulation or throughput areas where wind speed is compressed and accelerated.   wind breaks - height, density, number of rows, species composition, length, orientation, and continuity - determines the effectiveness of a windbreak in reducing wind speed. Upwind and downwind implications, particularly for snowdrifting.
Term
 Physical Control Measures (BACMs)
Definition
 BACMs are methods used to reduce or eliminate windblown dust in areas where natural soils have been disturbed and are thus more prone to erosion by the wind. BACM is defined as the maximum degree of emission reduction feasible for a significant source category. BACM is determined on a case-by-case basis, taking into account technical feasibility, environmental and economic impacts as well as other costs. The process of determining BACM takes into account the most common sources of manmade dust, when they occur, what measures can be used to reduce dust, te relative cost of such measures, and their effectiveness in reducing dust.   For example... roughen surface is 15-64% effective, cross wind ridges (24-93%), increase soil moisture (90%), erect wind breaks (4-88%), prohibit activities during high winds (98%), apply dust supressant (84%), wet suppression (50-90%), minimize trackout onto paved roads (40-80%), pave the surface (>90%), re-vegetate (90%), enclosures around storage piles (75%), limit vehicle speed (44%)
Term
 Various BACMs defined
Definition
Term
 Module 3 closing remarks
Definition
 Minimize negative downwind effects associated with land development   1)Gain experience with BACMs - understand how well they work under different conditions   2)Monitor and document progress/setbacks using different control measures.   3)Timing is everything - implement control measures aggressively during initial stages of development.   Developing a knowledge base for land development in a windy climate -dust control plan, including compliance standards and scheduling -Wind gust recurrence probabilities - like food forecasting -Wind categories - restricting certain activities -Real-time wind information and forecasting -Process monitoring - how much dust, snowdrift, etc., under different development activities? -Testing and evaluation of control methods.
Term
 Owen's Lake, California: Dust-producing engine of the southwest   About the lake.
Definition
 In the late 1800s, Owens Lake, at about 110 square miles, was one of the largest natural lakes in California. It was a saline terminal lake with a salinity about 1.5 seawater.   In 1913, the City of Los Angeles Department of Water and Power (LADWP) completed construction of the Los Angeles Aqueduct. The Aqueduct diverted Owens River water destined for Owens Lake 223 miles south to Los Angeles. With the lake's main source of water diverted, by the mid-1920s, Owens Lake had shrunk to a small hypersaline remnant brine pool of about 103 square km, and less than 1m deep.   Owen's Lake, with its unstable saline soils, began to emit large amounts of fugitive dust in the 1920s and has become the largest single source of particulate matter air polution in the US. -76k tons of PM10 annually. Currently, approximately 65-100 sq km along the eastern shore of the lake bed emits dust regularly.
Term
 Owen's Lake, California: Dust-producing engine of the southwest   Who Cares? and Control measures.
Definition
 The federal 24hr standard for PM10 is 150 micrograms/cubic meter. The "significant harm to health" level is 600 micrograms per cubic meter. ***24hr levels of 3,900 have been measured in Keeler and 12,000 at Dirty Socks.   The US EPA AIRS Data for 2002 show that of the 30 highest PM10 days reported nationally, 28 occurred at Owens Lake. Owens Lake's highest day of 7,915 was over 13 times higher than any other location in the USA (590 in El Paso, Texas).   How will the dust be controlled? A multi-million (100s) dollar project.   In 1998, the District adopted a State Implementation Program (SIP) that required the LADWP to control dust emissions from Owens Lake by the end of 2006. The 1998 SIP required that, within a 90 sq km envelope, 43 sq km of the lake bed had to be controlled by the end of 2003. It also required the District to continue to collect data on those areas of the lake bed that needed dust controls and revise the SIP in 2003 to incorporate the latest information.   ** Three approved methods of controlling dust that are feasible on a large scale: 1)native vegetation 2)flooding with shallow sheets 3)gravel blanket   The Key is....vegetation. Research indicates that if 50% of a dust producing area consists of live or dead vegetative cover, dust emissions will be reduced by 99%.   why? Vegetation is an imporant surface control because it reducs wind erosion in 3 ways: 1)shelters the soil from the shear stress of the wind 2)Reduces the force of wind near the surface by extracting momentum from wind 3)Traps incoming soil particles - induces deposition becuase of (b).   It takes approximately 7 acre-feet of water per acre to reclaim the saline soils and establish vegetation the first year. In subsequent years it takes about 2.5 acre-feed of water per year per acre to maintain the 50% veg cover necessary to control PM10   Saltgrass Is attractive because: 1)it is a locally adapted native species (@ Owens Lake) 2)It is very  salt tolerant 3)It spreads via underground runners and thus new growth is protected from wind damage 4)It creates a surface protecting mat.   ...however.... it is not particularly drought tolerant.
Term
 A new approach for mapping aerodynamic surface roughness
Definition
 Chris and Owen Brown describe a new twchnique where LiDAR is used to estimate aerodynamic roughness over a large area at fine resolution.   Use zo = 0.33h1.07 .
Term
 Boundary layer wind velocity profiles can be subdivided into two regions:
Definition
 1)Inertial sublayer (free stream) - flow above the roughness elements (small change in velocity with height), and   2)Roughness sublayer - lies inside and just above the roughness elements (near surface)   INERTIAL SUBLAYER - FREE STREAM Flow in the inertial sublayer, over a smooth surface and thermally neutral air follows a logarithmic increase with height (z) above the surface: uz = u*/k ln(z/zo), z>zo Recall that shear velocity (u*) is proportional to the rate of change of velocity with height. Aerodynamic surface roughness (zo) is the height at which horizontal velocity is zero. On a perfectly flat surface , the value of zo depends on the grain size of sediment at the surface.   With vegetation or other roughness elements, velocity above the elements follows a logarithmic profile. The logarithmic portion can be extrapolated down to a height where the mean horizontal wind speed (u) is zero. However, with roughness elements the height at which u extrapolates to zero is displaced to the top of the elements (displacement height, d). The wind profile may then be determined from: uz = u*/k ln[(z-d/Zo) Where Zo is the aerodynamic roughness length as defined by the roughness element height, shape, and spacing. It is larger than that of bare soil (Zo>zo) because the roughness elements increase surface drag.
Term
 Surface Drag - the Drag coefficient   (more inertial sublayer)
Definition
 The drag coefficient (Cz) is a dimensionless quantity which is used to quantify the resistance of an object to airflow. Cz= (u*/Uz)2 where Cz = the drag coefficient at height z. Often Cz is considered a constant for a given z; however, computations by Hsu and Blanchard (1991) for C10 showed a variation of from 0.0005 to 0.005. In fact, Cz varies with season and wind direction and cannot be considered constant.
Term
 Lower limit of the inertial sublayer
Definition
 The logarithmic profile often does not work at levels below or even near the maximum height of roughness elements. In the laboratory, experiments show that the logarithmic profile works down to a level of approximately 2 times the height of roughness elemens (z=2h).   In the field, it is found that the lower limit of the inertial sublayer is defined as z=h+1.5D, where h is the mean roughness element height and D is the separation distance b/w nearest neighbour elements.
Term
 Roughness Sublayer
Definition
 Vegetation interacts with wind within the roughness sublayer in several ways: -extracting momentum -producing turbulece in the form of wakes behind obstacles -breaking down large-scale turbulent eddies into smaller scale motions   Flow in the roughness sublayer is complex - further complcates our ability to assess the potential for sediment transport below the displacement height.   The gradient of the velocity profile within the roughness sublayer is related to several roughnes element length scales: -height -width -spacing -density -geometry   Before considering a collection of plants (roughness elements), let's first consider the flow modifications induced by a single plant. -wake region (deceleration) -separation -acceleration -stalling
Term
 Types of flow regime
Definition
 Grasses and crops usually provide continuous cover, but shrubs can provide an interspersed array of vegetation and bare soil (American SW - creosote)   Depending on the spacing of shrubs, three types of flow regimes will develop: 1)isolated roughness flow - wide spacing of elements 2)wake interference flow 3)skimming flow   Shading represents wake region - decelerated/protected; light areas represent region of flow where inertial sublayer might be expectd to penetrate to the bed.   As density increases the surface protected by the decelerated region increases. With decreased spacing the wakes formed by the roughness elements do not fully develop before another element is encountered - wake interference.   In skimming flow the entire soil surface is protected from the recovery of the inertial sublayer even though there may be a considerable portion of bare soil. This is the optimal condition for surface control of wind erosion using vegetation.   2x2cm cubes used to examine effects of element density in a wind tunnel. A cover of greater than 40% results in skimming flow.
Term
 How do we Characterize (and estimate) the roughness effect of vegetation?
Definition
 Several metrics: 1)plant silhouette area - the vertical cross-section of the plant that the wind encounters 2)density - number of individuals (or thir biomass) per unit area 3)Lateral cover - the ratio b/w silhouette are and total surface area   Lc=DAs Where D is density and As is the mean frontal-silhouette area (height x diameter) per area. Roughness density is derived from..   lamda= As/S Where S is he surface area per plant. For sparse arrays aerodynamic roughness can be derived from Z0=lamda/H, where H is the mean height of plants.
Term
 How do you measure vegetation metrics in the field?
Definition
 Use a quadrat (1sq m)   Roughness density is derived from SUM[nh([wl]/2)/a]   Where n is the # of individuals measured for maximum height (h), ength of the longest axis (l), and length of the perpendicular axis (w), and a is the area of each quadrat (1 sq m).   Percentage veg cover is derived from: SUM(wl)/a   ****LAMDA IS THE SYMBOL FOR ROUGHNESS DENSITY*** (baha)
Term
 Shear stress partitioning
Definition
 When the soil surface is obstructed by roughness elements the total force (F0) of the wind is partitioned b/w the roughness elements (Fr) and the intervening bare soil (Fg):   F0 = Fr + Fg   This is relevant because we must know how much force is extracted by the vegetation, and ow much remains to entrain soil at the surface. The effect of vegetation an also be examined from the ratio of the impact threshold with and without vegetation - but this must be measured.
Term
 What are prairie sandhills?
Definition
 After the last iceage, wind reworked the land once the ice and water receded.   There are currently 120 dune fileds (sand hills) and less than 1% are active. -some up north on AB/SK border... cypress hills... south manitoba. These areas are islands of biodiversity for species that require this kind of habitat.   Water tables close to the surface is very common for these areas.   Archaeological evidence exists of aboriginal occupation and exploitation. Dusky Dune Moth is an example of an endangered spp -also Ord's kangaroo rat, western spiderwort, small-flowered sand-verbena, and many others.   ***Of the more than 40 native prairie plant and animal species listed as species at rish in Canada, 25% are found in Prairie Sand Hills -due to changing ecosystem and changing habitat.   used to be... "miles of burning sand"   OVER the last 200 years, prairie Sand Hill ecosystems have transformed. Open-sand habitat has decreased substantially, threatening the survival of a number of endangered species.
Term
 Mitigating the trend of open-sand habitat decline.
Definition
 Wind erosion has a positive role!   Studies have tried to stimulate wind erosion and renew habitat with -fire -artificial wind erosion hollows -grazing attractants   Used post-burn wind erosion monitoring. Unfortunately, everything grew back very quickly. In the spring (after 7 months) ground was almost completely covered with vegetation again.   In artificial wind erosion hollow, after 1 year still fairly exposed.   LESSON LEARNED Fire, artificial hollows and grazing attractants are successful in the short-term, but not in the long-term.   Future Challenges: -Environmental assessment and mitigation of Oil & Gas development in Prairies.
Term
 Environmental Assessment and mitigation of Oil and Gas developent in Prairie Sand Hills
Definition
 1)Critical Habitat Mapping -Remote sensing delineation of sparse-vegetation habitat   2)Terrain sensitivity mapping -Improving the characterization of wind and water erosion risk   3)Water Resources -Sand hill near-surface aquifers: volume, recharge rate, extraction. -Sand hill surficial aquifers: volume, recharge rate   4)Climate Change/Variability -Adapting to future extremes and trends -changing terrain sensitivity -water availability -shorter drilling season
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