Archive for the ‘General’ Category

Height of Wind Measurements above Ground

Wednesday, August 12th, 2009

Height of Wind Measurement
Due to surface drag, even over seemingly smooth surfaces laminar wind speed decreases to near Zero at the surface of the earth.3    In fact wind speed on a flat grassy surface under normal non turbulent wind conditions the wind speed can be seen to increase logarithmically with height above the surface.  In flat grassy areas (with low grass height) at standard temperature this change in wind speed as a function of height can be approximated using the formula: V= Vref(H/Href)0.142  and shown in the below chart 4

Figure 2.5 Wind Speed as a Function of Height above Ground

Wind Speed as a Function of Height above Ground

4 Note:  According to one Canadian Study by the CNRC the exponent used above “0.142” should be changed to 0.333 over rough terrain and wooded areas or outskirts of towns and to 0.5 over cities.

As can be seen on this chart wind speed of 12 knots measured at 5 meters above the ground will be 13.3 knots 10 meters above the ground and 8.2 knots 1 meter above the ground due to surface friction creating a boundary layer of air near the surface of the earth.

The international standard height for wind measuring instruments is 10 meters (32.8 feet) above ground level.  Wind instruments sited at lower heights can be corrected for surface friction to a 10 meter equivalent measurement  (providing there is no surface induced turbulence) using the equations similar to the above calculation or sited higher than 10 meters and corrected to the lower speed that would be measured at 10 meters. This effect is considered negligible above 300 meters in most terrain.  Keep in mind that differences in surface roughness and temperature will require modification of this calculation to more precisely correct wind speed for height above the earth’s surface.

3 Now you know why it seems warmer when you lay down close to the ground on a cold windy winter day.

Point to Ponder: Why are airport wind socks at 16 feet above the ground and airport anemometers at 33 feet above ground level?

Surface Wind Modifiers/ Wind Flow Over & Through Trees

Wednesday, August 12th, 2009

Wind Flow Over & Through Trees
Wind flow through trees (even relatively widely spaced trees) can be substantially decreased by the surface friction effect of the trees.  Below the tree tops decrease in wind speed on the leeward side of a thin forest may be less than half the wind speed on the windward side.

Point to Ponder: Where can you site a wind instrument on Manhattan Island, NY or in a heavily forested area to measure synoptic wind?

What Causes Surface Winds/Mountain Winds/Katabatic or Anabatic Winds?

Wednesday, January 28th, 2009

Katabatic and Anabatic Winds:

Local Surface winds are sometimes more a function of Temperature Differences between mountain tops and lower elevations than overriding Synoptic winds.  These winds are sometimes called Mountain Winds as they occur most frequently in mountainous areas, meteorologist call them Katabatic or Anabatic Winds (more…)

What Causes Surface Wind/Thunderstorms/Wind Shear?

Friday, January 16th, 2009

Mature Thunderstorm Wind:

Thunderstorms are primarily local thermal weather phenomena (usually less than  5 miles to sometimes more than 30 miles in diameter), that are caused by either local surface heating , Air Mass Thunderstorms , or by weather systems such as fronts, converging winds, or troughs aloft that force upward motion of the surrounding air.  From a surface wind perspective, thunderstorms, regardless of their cause can quickly and substantially modify wind direction and speed.  (more…)

The Airlines’ Eye on the Sky

Friday, June 15th, 2007

The Airlines’ Eyes on the Skies By Del Quentin Wilber The Washington (DC) Post

FORT WORTH — Airline meteorologist Mark Mabey stares at four computer screens on his desk. They are filled with data, charts and radar images. All seem to suggest a different potential for thunderstorms — the airlines’ enemy during the hectic summer travel season. (more…)