Wind resource assessment and site development
Wind resource assessment is the critical first step in wind farm development. This unit covers how to evaluate a site's wind potential, understand long-term variability, and manage the uncertainties inherent in early-stage project planning.
- Mast data versus model data
- Long-term wind variability
- Shear and turbulence at hub height
- Wake and directional effects
- Planning and noise assumptions
ON THIS PAGE
- Decisions and thresholds
- Why wind decides this work
- The decisions and the numbers
- Height and where the wind is actually measured
- Gusts, turbulence and timing
- Reading the odds: ensemble forecasts for long-term variability
- Ireland specifics: resource, planning, and grid
- A worked day: early-stage site evaluation (example)
- How to set this up in the instrument
- Questions
- Sources
Decisions and thresholds
| The question | Metric | Commonly cited thresholds* | Instrument |
|---|---|---|---|
| Is the site's wind resource strong enough? Compare long-term climatology, shear, and wind rose for the site. Cross-check models against any available observations. Use the Weibull view to estimate energy yield potential, focusing on the P50 (median) and P90 (90% probability of exceedance) estimates for robust financial modelling. | Mean speed |
| windops mode |
| What is the long-term annual energy production (AEP)? The Wind Agent provides long-term climatological data and Weibull distributions for a given location and height. This allows for the calculation of an estimated Annual Energy Production (AEP) by integrating the power curve of a prospective turbine with the site's wind speed distribution. Consider the P50 and P90 values from ensemble forecasts for risk assessment. | Mean speed | No numeric threshold — read against the site. | windops mode |
| How does wind shear affect hub height wind speeds? Utilise the Shear Glass and shear heatmap to understand the wind profile from 10 m up to proposed hub heights (e.g., 80 m, 120 m, 180 m). Significant shear can mean lower-than-expected hub height wind speeds or increased fatigue loading on turbine blades. The power law exponent can be calculated from the Shear Glass data. | Delta-T | No numeric threshold — read against the site. | windops mode |
| What are the dominant wind directions and their variability? The wind rose chart illustrates the frequency and strength of winds from different directions. This is crucial for optimising turbine layout, understanding wake effects, and assessing potential noise impacts on nearby receptors. Compare the wind rose across different seasons using the monthly climatology. | Direction | No numeric threshold — read against the site. | windops mode |
* Commonly cited — not a statutory limit. Thresholds are attributed to who commonly uses them. Set your limit from your own procedure, equipment document or instructor; the instrument opens with the first figure only as a starting point.
01Why wind decides this work
Wind resource assessment is the foundational element of any wind energy project. The economic viability of a wind farm hinges directly on the quantity and quality of the wind resource at the proposed site. A small difference in mean wind speed can translate into a substantial change in projected Annual Energy Production (AEP) and, consequently, revenue.
For instance, a 10% increase in mean wind speed can lead to a 30% increase in power output due to the cubic relationship between wind speed and power. Therefore, accurate assessment reduces financial risk and attracts investment.
This early-stage work involves:
- Site prospecting: Identifying locations with high wind potential.
- Measurement campaigns: Deploying meteorological masts or remote sensing devices.
- Data analysis: Characterising the wind regime, including speed, direction, shear, and turbulence.
- Energy yield assessment: Estimating future electricity production.
- Uncertainty quantification: Understanding the range of possible outcomes.
The Wind Agent provides the modelled climatological data to support these initial assessments, offering insights into long-term averages and variability before significant on-site investment.
02The decisions and the numbers
The primary decision in resource assessment is whether a site possesses a sufficiently strong wind resource to be economically viable. This is typically quantified by the mean annual wind speed at prospective hub height.
Commonly cited benchmarks for onshore wind development include:
- 6.5 m/s at 100 m hub height: This is often cited as a minimum threshold for initial project viability in many regions, including Ireland. Below this, projects may struggle to achieve competitive returns without specific subsidies or low development costs. This figure is a mean annual average.
- 7.5 m/s at 100 m hub height: Sites achieving this mean speed are generally considered more attractive and competitive, offering a stronger business case. Such sites typically benefit from better capacity factors.
- 9.0 m/s at 100 m hub height: These represent high-resource sites, often found in exposed coastal or elevated inland locations. They are highly sought after and can support larger, more efficient turbines.
These thresholds are illustrative and not statutory limits; your project's specific financial model, turbine technology, and market conditions will dictate the true viability threshold. The Wind Agent's climatological data, including the Weibull distribution, allows for a granular assessment against these benchmarks.
The Weibull distribution shows the frequency of different wind speeds, crucial for calculating Annual Energy Production (AEP). The chart also shows the typical power curve of a modern turbine.
03Height and where the wind is actually measured
Wind speed varies significantly with height above ground, a phenomenon known as wind shear. Modern wind turbines have hub heights ranging from 80 m to over 180 m, far above the standard 10 m reference height for meteorological observations.
Resource assessment typically involves:
- Meteorological masts: These are physical towers equipped with anemometers at multiple heights (e.g., 30 m, 50 m, 80 m, 100 m) to capture the vertical wind profile. Data from these masts are considered the most reliable for site-specific assessment.
- Remote sensing devices: LiDAR (Light Detection and Ranging) and SODAR (Sonic Detection and Ranging) systems can measure wind speed and direction at various heights without a physical mast, offering flexibility and covering a wider range of heights.
- Model data: Numerical Weather Prediction (NWP) models, like those used by The Wind Agent, provide modelled wind speeds at different atmospheric levels. These are invaluable for initial prospecting and for 'filling in' gaps in measurement campaigns, as well as for long-term correlation.
The Wind Agent's Shear Glass provides modelled wind speeds at 10 m, 80 m, 120 m, and 180 m, allowing developers to visualise the wind profile up to typical hub heights. This is crucial for understanding how the wind resource measured at a lower height translates to the turbine's operational height.
This heatmap visualises wind speed changes with height over time, highlighting periods of strong or inverse shear. Look for consistent shear patterns at proposed hub heights.
04Gusts, turbulence and timing
While mean wind speed drives energy production, gusts and turbulence are critical for turbine design, fatigue loading, and operational safety. Turbulence is the rapid, irregular fluctuation of wind speed and direction, often quantified by the turbulence intensity (TI), which is the ratio of the standard deviation of wind speed to the mean wind speed.
High turbulence can:
- Increase fatigue loads on turbine components, reducing operational life.
- Lead to higher noise emissions.
- Cause more frequent turbine shutdowns for safety.
Resource assessment must consider not only the magnitude of gusts but also the prevailing turbulence characteristics, particularly at hub height. The Wind Agent provides gust forecasts at 10 m, which, while not directly applicable to hub height turbulence, indicate the general gustiness of the atmospheric boundary layer.
Timing is also crucial. Wind resources can vary significantly by season and even hour of the day. Understanding these diurnal and seasonal patterns helps in optimising project scheduling and predicting energy delivery profiles. The monthly climatology chart can help identify seasonal variations.
This chart shows the average monthly wind speed and direction, revealing seasonal patterns that influence energy production and development timelines.
05Reading the odds: ensemble forecasts for long-term variability
Wind resource assessment extends beyond a single mean annual value; it must also account for year-to-year and decade-to-decade variability. The long-term mean wind speed is derived from climatological datasets, often spanning 20–30 years or more (e.g., ERA5 reanalysis).
However, individual years can deviate significantly from this mean. Year-to-year variability around the long-term mean can be 10% or more, impacting project revenues. Ensemble forecasts, while primarily for short-term prediction, illustrate the inherent uncertainty and range of possible outcomes.
For long-term resource assessment, this translates to:
- P50 (Median) AEP: The estimated Annual Energy Production with a 50% probability of being exceeded. This is the most likely outcome.
- P90 (90% Exceedance) AEP: The estimated Annual Energy Production with a 90% probability of being exceeded. This conservative estimate is often used by lenders and investors to assess downside risk.
The Wind Agent's ensemble plume and exceedance curve charts, while typically applied to short-term forecasts, conceptually demonstrate how a range of possibilities is presented, which is analogous to the P50/P90 concept in long-term assessment. For resource assessment, the focus is on historical and modelled climatology rather than daily ensemble forecasts.
The climate band chart indicates the typical range of wind speeds for a given location, helping to contextualise current conditions within long-term variability.
06Ireland specifics: resource, planning, and grid
Ireland possesses a robust wind resource, particularly in its western and northwestern counties such as Cork, Kerry, Galway, and Donegal. These regions benefit from direct exposure to Atlantic weather systems, resulting in strong mean wind speeds that make them highly competitive for onshore wind development.
However, the primary limitations for wind development in Ireland are often related to planning permission and grid access rather than the wind resource itself. The planning process can be protracted, involving environmental impact assessments, public consultation, and addressing concerns such as visual amenity, noise, and ecological impacts.
Grid infrastructure also poses a challenge. While the resource may be excellent, connecting new wind farms to the national grid, especially in remote areas, requires significant investment and upgrades. EirGrid's Grid Development Strategy outlines the necessary expansions.
Year-to-year variability in Ireland's wind resource can be 10% or more around the long-term mean, as evidenced by Met Éireann's climatological reports. This variability necessitates robust financial modelling that accounts for P50 and P90 AEP estimates to manage revenue uncertainty. The Wind Agent provides the detailed climatological data to support these assessments.
The wind rose displays dominant wind directions and speeds, essential for understanding site characteristics and potential wake effects in Ireland's prevailing south-westerly winds.
07A worked day: early-stage site evaluation (example)
Consider an initial evaluation for a potential wind farm site in County Kerry, focusing on a proposed 120 m hub height. The development manager uses The Wind Agent to assess the long-term wind resource.
- Climatological mean: The monthly climatology chart for the site indicates an annual mean wind speed of approximately 8.2 m/s at 120 m. This is above the 7.5 m/s threshold for competitive projects.
- Directional persistence: The wind rose shows a strong prevalence of winds from the south-west and west, accounting for over 60% of annual wind hours. This suggests consistent wind flow but also highlights the importance of optimising turbine layout to minimise wake effects from these dominant directions.
- Shear assessment: The Shear Glass and shear heatmap show a typical power law exponent of 0.15–0.20, indicating moderate shear. During night-time inversions, the shear exponent can increase to 0.30, meaning wind speeds at 120 m are significantly higher than at 10 m, which is favourable for energy capture.
- Weibull distribution: The Weibull distribution for 120 m shows a k-factor of 2.2 and an A-factor of 9.0 m/s. Integrating a typical 3 MW turbine power curve with this distribution yields an estimated P50 AEP of 10.5 GWh/year, with a P90 AEP of 9.8 GWh/year. This provides a solid basis for initial financial modelling.
This example demonstrates how the instrument's data supports early-stage decision-making by providing a comprehensive understanding of the site's wind characteristics.
08How to set this up in the instrument
The Wind Agent is configured to support wind resource assessment and site development through several features:
- Persona selection: Select the 'Wind Operations' persona to access relevant metrics and visualisations tailored for energy professionals.
- Height matching: Use the Shear Glass to set your analysis height to typical turbine hub heights (e.g., 80 m, 120 m, 180 m). The instrument will then provide height-matched wind data.
- Limit setting: While resource assessment focuses on averages, you can set example limits (e.g., a minimum viable mean wind speed) to visualise how the climatological data compares. The exceedance fan can then show the probability of exceeding this limit over long periods.
- Evidence records: For due diligence, the instrument allows you to generate and export evidence records of historical wind conditions and modelled climatology for specific locations and periods. These records are timestamped and verifiable.
- Fleet board: If assessing multiple potential sites, the fleet board provides an overview of key wind metrics across all locations, facilitating comparative analysis and prioritisation.
- Alerts: While less critical for long-term assessment, alerts can be configured for specific short-term conditions during site visits or mast installation, such as high wind events or prolonged calm periods.
The exceedance fan shows the probability of exceeding user-defined limits at specific heights, useful for risk assessment in resource evaluation.
Questions
What is the difference between mean wind speed and gust speed in resource assessment?
Mean wind speed is the average wind speed over a period (e.g., 10 minutes, hourly, annually) and is the primary driver of energy production. Gust speed is the peak wind speed over a very short duration (e.g., 3 seconds). While mean speed determines energy yield, gusts and turbulence influence turbine design loads, fatigue, and operational safety. Resource assessment focuses on mean speeds for energy, but also considers turbulence intensity for structural integrity.
Why is it important to consider wind shear in wind resource assessment?
Wind shear describes how wind speed changes with height. Wind turbines operate at hub heights far above the standard 10 m measurement height. Accurately characterising shear is crucial because it directly impacts the wind speed at the turbine rotor, affecting power output. Incorrect shear assumptions can lead to significant over or underestimation of Annual Energy Production (AEP) and can also affect turbine loading.
How does long-term wind variability affect project financing?
Long-term wind variability refers to the natural fluctuations in annual mean wind speed from year to year. This variability introduces uncertainty into projected revenues. Financial institutions and investors typically require conservative estimates, such as the P90 AEP (90% probability of exceedance), to account for periods of lower-than-average wind. Understanding and quantifying this variability is essential for securing project financing and managing risk.
What is a Weibull distribution and how is it used?
The Weibull distribution is a statistical function commonly used in wind resource assessment to describe the frequency distribution of wind speeds at a site. It is characterised by two parameters: the shape factor (k) and the scale factor (A). By fitting measured or modelled wind data to a Weibull distribution, developers can estimate the Annual Energy Production (AEP) of a prospective wind turbine by integrating its power curve with the site's wind speed distribution. It provides a more complete picture than just a mean speed.
Can The Wind Agent replace a meteorological mast for resource assessment?
No, The Wind Agent provides high-resolution modelled climatological data and forecasts, which are invaluable for initial prospecting, screening, and understanding long-term trends. However, for definitive financial investment decisions and detailed energy yield assessments, on-site meteorological mast data or validated remote sensing measurements are typically required. Model data serves as an excellent complement, providing context and long-term correlation for measured data, but not a full replacement for site-specific measurements.
SOURCES
- Met Éireann - Climate of Ireland
- EirGrid - Grid Development Strategy
- SEAI - Ireland's Energy in 2022
- European Centre for Medium-Range Weather Forecasts (ECMWF) - ERA5
Thresholds on this page are commonly cited figures, attributed to their source — never statutory limits. Modelled forecasts are planning support, not on-site measurement.