The leeβeffect describes how wind speed increases when a steady airstream is forced to flow around a protruding landform such as a headland. As the wind encounters the obstacle, the air is displaced upward and then accelerates on the downstream (lee) side, creating a zone of higher velocity that can significantly affect vessel handling and wave generation.
The magnitude of this acceleration depends on several key parameters: the ambient wind speed (Uβ), the height of the headland (H), the distance measured downwind from the headland crest (x), and the angle (ΞΈ) between the wind direction and the normal to the headland face. A steeper headland, a stronger onβshore wind, or a wind direction more aligned with the headland normal all tend to increase the leeβside wind speed.
Because the acceleration term (H/x)Β·cosΞΈ diminishes with distance, the leeβeffect is most pronounced close to the headland and gradually fades offshore. Mariners use this relationship to anticipate localized wind gusts, adjust sail plans, and evaluate wave growth in coastal passages.
What is the Lee Effect Wind Calculator used for?
How does the Lee Effect impact vessel handling?
What parameters are needed for the calculation?
Can this calculator be used for any landform, or just headlands?
How accurate is the Lee Effect Wind Calculator?
Is there a maximum distance for which this calculation is valid?
Can I use this calculator for planning my route around headlands?
Results are for informational purposes only and do not constitute professional advice.
