Dewpoint
is the temperature at which air becomes saturated and produces dew. A high
dewpoint temperature is indicative of moist warm air. A low dewpoint temperature
indicates relatively dry conditions in either a cold or warm air mass. Prior
to the extensive use of weather balloons, satellite imagery, Doppler weather
radar and other modern remote sensing techniques, the surface dewpoint was
the only method to track moisture movements across an area prior to precipitation
occurring. Hence dewpoint was historically one of the first methods to track
monsoon surface moisture movements into the Southwest. Additionally an increase
in surface moisture rapidly degrades the efficiently of evaporative coolers,
and is immediately noticeable for those without refrigeration air conditioning.
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