METEOROLOGIST JEFF HABYMorning condensation (dew) is very common in part regions and can conveniently be forecasted. The favorable weather elements for dew encompass clear skies, irradiate wind, decent floor moisture, and low night-time dewpoint depressions. Dew forms when the temperature becomes equal to the dewpoint. This frequently happens an initial at ground level for two reasons. First, longwave emission reasons the earth"s surface to cool in ~ night. Condensation requires the temperature come decrease to the dewpoint. Second, the soil is frequently the moisture resource for the dew. Warm and moist soils will assist with the development of dew together the floor cools overnight. The cooling of warm and moist soil during the night will reason condensation specifically on clear nights. Clear skies enable for the maximum relax of longwave radiation come space. Cloudy skies will reflect and absorb if re-emitting longwave radiation back to the surface and that avoids as lot cooling native occurring. Light wind avoids the mixing of air appropriate at the surface ar with drier wait aloft. Heavier dew will tend to occur when the wind is light together opposed to when the wind is strong. Particularly when soils are moist, the humidity concentration will certainly be higher near the earth"s surface than higher above the earth"ssurface. As the waiting with greater moisture concentration cools, this air will develop condensation first. Soil moisture is EXTREMELY crucial to producing dew (especially heavy dew). Dry regions that have not obtained rain in end a mainly or two room much much less likely to have actually morning dew (especially a heavy dew). When the soil gets a great soaking native a rain, the takes numerous days for the floor to lose the moisture v evaporation. If nights are clear ~ a an excellent rain, dew can be expected every morning because that the next few days (especially in areas with abundant vegetation, clean skies and light wind). The dewpoint depression is important since it determines exactly how much the air will need to cool to with saturation. V a big dewpoint depression (greater than 25 systems of F), rather a bit of night-time cooling will must take location in order to develop dew. A short dewpoint depression through the other determinants favorable for dew is much more likely to produce heavy dew. Dew is necessary to forecast due to the fact that it impacts people. Dew can create a thick film of water almost everywhere the vehicle in the morning (can be specifically annoying for human being that don"t have actually a garage). Time needs to be invested wiping the water turn off the windows in stimulate to view on-coming traffic. Dew is additionally important to agriculture. Dew recharges the soil moisture and also limits evaporation indigenous the soil throughout the time the dew is forming. Dew deserve to make the mowing the the lawn much more difficult. That is much simpler to mow the lawn in the so late afternoon when the dew has actually evaporated than it is in the morning. Wet grass clumps together and also sticks come everything.