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Measuring weather

measure Atmospheric visibility, a measure of how far one can see in given conditions, is useful information for a variety of daily human activities, especially in the area of transportation. On the ASOS, a forward scatter sensor is used to measure visibility. The sensor works by flashing a Xenon light using wavelengths in the blue part of the visible spectrum into air in front of a detector. The detector faces north to minimize solar glare and measures the amount of light scattered off the air and any particles within. This measurement is related to how far one can see in such air, up to a maximum of 10 miles. It will include the effects of precipitation, sand, dust, and smoke.

Present weather is what the weather is doing right now. This includes
  • is it precipitating and what kind of precipitation is it, including freezing rain
  • is there lightning
  • is it windy

 

measure Finally, Surface Radiation observations are important for constructing energy budgets and keeping records of sunlight duration and intensity (flux density in Watts per square meter). Pyranometers are used to measure incoming solar radiation on a plane surface from the whole 180 degree sky. Pyrgeometers do the same for longwave radiation. Pyrheliometers measure the direct solar radiation, neglecting shortwave radiation reflected off other surfaces like buildings or the air itself. Most useful for radiation budgets are net radiometers, which simultaneously measure upward and downward directed shortwave and longwave radiation. Using this instrument, the surface albedo can also be determined.

Next page   -> in situ, surface observations, radiation & clouds

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