University of Otago Logo Energy Studies Program Lightning

About wind speed, air pressure and rain

Measurements

Wind speed is measured with a Vector A101M Pulse Output Anemometer (pictured below). It consists of a wind-driven rotor that creates an electric pulse every complete revolution. The data-logger counts the pulses and calculates wind speed every 20 seconds. The highest of these is the maximum gust, and the average of all of them over five minutes is the average speed. Wind direction is measured by a Vector W200P/L windvane. The position of the vane determines the resistance across a potentiometer. The data-logger calculates the average wind bearing based on these resistance readings.

Air pressure is measured with a Vaisala PTA 427 Barometric Pressure Transducer. It utilises the varying capacitance of a sliver of silicon crystal caused by it flexing due to pressure fluctuations.

Interpretation - WindWind speed and direction instruments

Wind speed is given in kilometres per hour. Interpretation of wind speed is conventionally done using the Beaufort scale, which equates ranges of wind speed with observable effects.

The scale on the chart goes up to 120 km/hr, which equates to a Beaufort force number of 11 (a violent storm). Note that the weather station is considerably elevated, meaning it is likely to get marginally stronger winds than at ground level. Check out the Beaufort scale.

Wind direction is given in degrees of arc, as with a normal compass. The bearing indicated is the direction the wind is coming from. Note that because the scale is circular and 0° and 360° both equate to north, points are likely to occur at the top and bottom of the chart when the wind is coming from approximately that direction. Also note that when the conditions are quite still, wind direction points will be scattered randomly as there will be no strong directional influence on the windvane.

Interpretation - Pressure

Mean sea level atmospheric pressure is 1013 hPa. Pressure readings below this indicate a low pressure air-mass is in the region, and readings above indicate a high pressure air-mass. Low pressure is associated with wet, cold weather and high pressure with fine, warm weather. Rapid change in the pressure reading, along with rapid changes in temperature and wind direction indicates a frontal system is moving in. Note that pressure also decreases with increasing altitude, and elevated as it is, the pressure transducer will read approximately 5 hPa lower than it would at sea-level.

 

 
 
 
 
 
 
 
 
 
   
   
   
   
   
 
 
 
 

 

 

Interested in learning more about the weather, climate change and the processes that power our planet?

Read More>>

Want to know about the Earth's energy resources and how they are utilised?

Read More>>

 
 Design by the web  office Energy Studies