Question:
At 30 degrees below zero, why do we have fog in
Fairbanks, Alaska?
Replies:
Brian,
Fog (or clouds) occur when the temperature reaches the dew point
(or frost point, which may be the case in your situation). For air
with very little water vapor content (low absolute humidity), much
lower temperatures are required to create visible fog. That does not
mean that no water droplets or ice crystals have been forming before
that, but you need a certain concentration of them before visibility
is reduced to the point that it is detected as fog.
The aerosols that water or ice form on in the atmosphere change the
properties of the solution (raise the surface tension) such that it
is more difficult for water vapor in the air to condense on the
water/aerosol solution. This results in a lower temperature than
dew or frost point (which considers only pure water effects) being
needed for visible water droplets or ice crystals to occur.
Ice fog requires particularly low temperatures if the air is very
"dry" (low water vapor content), as it obviously requires lower
temperatures to produce ice crystals than it normally does to produce
water droplets.
It sounds as though the water content in the air at Fairbanks was
extremely low, thereby requiring very low temperatures for a visible
fog (possibly of the ice type) to form.
David R. Cook
Meteorologist
Climate Research Section
Environmental Science Division
Argonne National Laboratory
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