NATS 101

Lecture 10
Condensation: Fog
and Cloud Formation

Cloud Condensation Nuclei
Small, airborne particles are necessary on which water vapor can condense to produce cloud droplets
Without such particles, RH>100% would be needed to produce clouds
Such surfaces are called Cloud Condensation Nuclei (CCN)
CCN are light and stay suspended for days

Cloud Condensation Nuclei
Sources
Dust, volcanic ash, smoke, soot, salt, sulfate particles
Concentrations
1,000-10,000 per cc Highest over cities Highest at surface

Cloud Condensation Nuclei
Haze over Melting Snow
Condensation
When air becomes supersaturated from either the temperature cooling or the addition of water vapor, water condenses onto CCN as small cloud droplets
Diameters of droplets are 2-20 microns, (10-100 times smaller than human hair)
Concentrations are 50-1,000 droplets per cc

Size of Cloud Droplets
What is Fog?
Fog - a cloud at the ground
There are four basic types of fog
Radiation Fog
Advection Fog
Upslope Fog
Steam Fog
Combinations exist (Radiation-Advection)

Radiation or Ground Fog
Valley Fog
Radiation Fog in Valley
Fog Dissipation in the Morning
Advection Fog
Advection Fog at Golden Gate
Upslope Fog
Steam Fog or Sea Smoke
Why You See Your Breath        on a Cold Winter Night
Condensation can occur if moist, warm air mixes with cold, dry air.
Temp RH SVP VP
Air 0oC 20% 6 mb 1 mb
(clear)
Breath 36oC 80% 63 mb 55 mb
(clear)
50-50 18oC 140% 20 mb 28 mb (cloud)
90-10 4oC 90% 8 mb 6 mb
(clear)
The 50-50 mix condenses into a cloud that quickly evaporates as your exhalation is diluted further

Steam Fog over Thermal Pool
Precipitation or Frontal Fog
Number of Days with Fog
Summary: Condensation
Condensation
Can occur by cooling or moistening of air
CCN permit condensation at RH near 100%
Small (<0.2 to 1 microns) airborne particles
Responsible for Haze formation at RH < 100%

Summary: Fog
Fog - a cloud at the ground
Composed of small (20 micron) water drops
Four primary types of Fog
Radiation-Advection-Upslope-Steam
Occur under distinct weather conditions

Next Lecture Assignments
Topic - Cloud Types
Reading - Ahrens pp 96-108
Problems - 4.16