The answer is snow because snow is a type of precipitation.
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∙ 14y agoSnow is not a type of condensation fog. Condensation fog includes cloud and dew, where water vapor condenses in the air to form droplets that can then accumulate to form clouds or settle on surfaces as dew. Snow is formed by the direct transformation of water vapor into ice crystals in the atmosphere.
Frost is to dew. Frost forms on surfaces when the temperature drops below freezing, while dew forms on surfaces when the temperature cools enough to cause condensation.
When water vapor cools and condenses into a cloud, this process is called condensation. This happens when the water vapor reaches its dew point temperature and changes back into liquid water droplets, which then cluster together to form clouds in the atmosphere.
Condensation occurs when water vapor in the air cools and changes into liquid water droplets. It happens at the cloud base because that is where the air temperature drops low enough to reach the dew point, causing the water vapor to condense into visible droplets that form clouds.
An approximate value can be calculated by the following expression: Condensation Level (in feet) = [Surface Temperature(F) - Surface Dew Point Temperature(F)]*(1000/2.2) or Condensation Level (in meters) = [Surface Temperature(C) - Surface Dew Point Temperature(C)]*(200) Solution: Dry Adiabatic Lapse Rate (DALR) => -5.5 F/1000 ft of altitude (-1C/100m) Saturated Adiabatic Lapse Rate (SALR) => -3.3F/1000ft of altitude (-0.5C/100m) The SALR is not linear and varies with the initial surface temperature The Level of Condensation will occur at the altitude where the Air Temperature is equal to the Dew Point temperature at that altitude. Setting the two equations equal to each other will give an approximate value. TA: temperature at altitude; TS: temperature at surface; DA: dew point temperature at altitude; DS: dew point temperature at surface TA = TS-(5.5F/1000ft)*altitude or TS-(1C/100m)*altitude DA = DS-(3.3F/1000ft)*altitude or DS-(0.5C/100m)*altitude Setting TA = DA and rearranging quantities gives the equations given above The level of condensation derived by the above method will only yield an approximate value.
dew point temperature. It is the temperature at which the air reaches its saturation point and condensation begins to form, leading to the formation of dew or fog.
No, dew is not a cloud. It is condensation on cold surfaces. In the winter it freezes and forms frost.
Condensation
1. fog 2. cloud 3. frost 4. dew. 5.drizzle 6.rain shower 7.Thunderstorm
This will cause condensation. You could get a cloud or dew.
Condensation
Condensation is the process by which water vapor changes into liquid water, while dew is liquid water that forms on surfaces as a result of condensation when the temperature drops. Dew is a type of condensation that specifically occurs on surfaces such as grass or leaves.
The dew point is the temperature at which the air becomes saturated with moisture, leading to condensation. If the air temperature is below the dew point and no cloud forms, it could be due to a lack of condensation nuclei - particles in the air on which water vapor can condense. Without these particles, the process of cloud formation may be inhibited even when conditions are otherwise conducive.
Precipitation is rain, sleet, snow or dew formed by condensation of water vapour in the atmosphere
the realationship between condensation and dew point is that condensation occurs when it reaches the dew point.
Frost is to dew. Frost forms on surfaces when the temperature drops below freezing, while dew forms on surfaces when the temperature cools enough to cause condensation.
Condensation occurs as water vapor changes into cloud droplets. This is the process by which gas or vapor transforms into liquid when cooled.
Well dew is a form of condensation. That being said a dry climate is less likely to produce dew.