METEOROLOGIST JEFF HABYMorning condensation (dew) is very common in part regions and also can conveniently be forecasted. The favorable weather facets for dew include clear skies, light wind, decent soil moisture, and low night-time dewpoint depressions. Dew develops when the temperature becomes equal to the dewpoint. This frequently happens an initial at soil level for two reasons. First, longwave emission causes the earth"s surface to cool at night. Condensation requires the temperature come decrease to the dewpoint. Second, the floor is often the moisture resource for the dew. Warm and moist soils will assist with the development of dew as the soil cools overnight. The cooling of warm and moist soil throughout the night will cause condensation specifically on clear nights. Clean skies enable for the maximum relax of longwave radiation to space. Cloudy skies will certainly reflect and absorb while re-emitting longwave radiation earlier to the surface and that stays clear of as lot cooling native occurring. Light wind prevents the mixing of air right at the surface with drier air aloft. Heavier dew will often tend to occur when the wind is light as opposed to when the wind is strong. Particularly when soils are moist, the moisture concentration will be higher near the earth"s surface ar than higher above the earth"ssurface. As the air with higher moisture concentration cools, this air will produce condensation first. Floor moisture is EXTREMELY an essential to developing dew (especially hefty dew). Dry areas that have actually not got rain in end a main or two are much much less likely to have actually morning dew (especially a hefty dew). When the soil gets a good soaking from a rain, it takes several days for the floor to shed the moisture through evaporation. If nights are clear after a good rain, dew deserve to be expected every morning because that the next couple of days (especially in areas with abundant vegetation, clear skies and also light wind). The dewpoint depression is important because it determines just how much the wait will need to cool to reach saturation. With a huge dewpoint depression (greater than 25 systems of F), fairly a little bit of night-time cooling will need to take place in stimulate to develop dew. A low dewpoint depression v the other components favorable for dew is an ext likely to produce heavy dew. Dew is necessary to forecast because it impacts people. Dew can create a thick film of water all over the automobile in the morning (can be particularly annoying for world that don"t have actually a garage). Time has to be spent wiping the water turn off the windows in stimulate to see on-coming traffic. Dew is also important come agriculture. Dew recharges the floor moisture and also limits evaporation native the soil during the time the dew is forming. Dew have the right to make the mowing of the lawn more difficult. The is much much easier to mow the lawn in the so late afternoon when the dew has evaporated than it is in the morning. Wet grass clumps together and also sticks to everything.

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Also, you are much more prone to obtaining a dirty shoe when walking top top dew extended grass as compared to dried grass.