Relative Humidity
The actual water vapor in the air to that of which it could possibly present
What determines how much water vapor can be held in the air?
Temperature & Relative humidity
Warmer temps can hold more water vapor
If relative humidity = 100% saturated air
If relative humidity <100% unsaturated air
Dew Point
Temperature in which air must be cooled to become saturated
*as H20 is added to the air, the DP will rise
Temp/Dew Point Spread (SPREAD)
Temp - dew point (T-DP)
Conditions needed for FOG
Condensation nuclei
Microscopic particles which can become condensation surfaces
Supercooled Water
Freezing Rain/Drizzle
Liquid that is below 0 degrees C
0 to -10 degrees C = stratiform clouds
0 to -15 degrees C = cumuliform clouds
Frost may form when the …
… dew point is 0 degrees C or colder
3 types of precip
Cold air over a warm lake = ?
Warm air over a cold lake = ?
showers
fog