2.3. Weather Processes and Phenomena Flashcards
Formation of Mist and Fog
For mist and fog to form, condensation nuclei, such as dust and salt, are needed.
- Fog - condensation must take place near ground level. Condensation can take place in 2 major ways: air is cooled, more water is added to atmosphere.
Mist
Occurs when visibility is between 1000m and 5000m and relative humidity is over 93%
Fog
Occurs when visibility is below 1000m. Dense fog occurs when the visibility is below 200m.
Advection Fog
Warm moist air moves over cold land or cold moist air moves over warm land. Contact cooling at a cold ground surface may produce saturation. As warm moist air passes over a cold surface it is chilled. Condensation takes place as the temperature of the air is reduced and the air reaches dew point.
Radiation Fog
Occurs in valleys with calm, cloudless conditions when the ground loses heat rapidly at night by long-wave radiation due to a lack of clouds. The cold air sinks down to the bottom of the valley, with warmer air on top. This is a temperature inversion. The ground becomes cold. When there is enough moisture, there is radiation fog.
Dew Point
The temperature at which relative humidity is 100% and condensation occurs
Condensation Level
the height at which the relative humidity (RH) of an air parcel will reach 100% and condensation occurs
Dew
Dew is the direct deposition of water droplets onto the surface and vegetation. It occurs in clear, calm anticyclonic conditions (stability) where there is rapid radiation cooling by night. The temperature reaches dew point, and further cooling causes condensation and direct precipitation onto the ground and vegetation
Evaporation
Liquid to gas
Condensation Process
When Relative Humidity reaches 100% saturation. During condensation process, water molecules lose the latent heat that was added during the evaporation process. When latent heat is released it is converted into sensible heat which warms the surrounding air, increasing the temperature.
Condensation Nuclei
Condensation requires particles or nuclei onto which the vapour can condense. These are condensation nuclei.
Humidity
A measure of the water vapour content of the air
Absolute Humidity
The amount of water in the atmosphere, usually measured in units of grams of water vapour per cubic meter of air
Relative Humidity
The water vapour present expressed as a percentage of the maximum amount of air that temperature can hold.
Precipitation
All forms of deposition of moisture from the atmosphere in either solid or liquid states.