"Fog in a Bottle"
Fog is a cloud that
forms just above the ground. It's spooky and neat. Really
thick fog can reduce you to seeing only a few feet in front
of you. It can be a real hazard to cars, planes and
boats.
There are two kinds of
fog, advection fog and radiation, or ground fog.
Advection fog is
common along the pacific coast of the United States. Warm,
moist air over the Pacific Ocean are blown inward. When that
air moves over colder coastal waters, it cools quickly and
fog forms. The fog is moved inland by the same westerly
winds.
Advection fog plays an
important role in the life of California Redwood trees. The
Redwood trees have very shallow roots. They depend on water
from sources other than water deep underground. What the
trees do not get from rain, they get from the fog. Advection
fog deposits moisture on the pine needles which then drips to
the ground and is absorbed by the roots.
The other kind of fog
is radiation, or ground fog. This fog is common lots of
places. It forms when a layer of warm, moist air forms low to
the ground. A layer of cooler, dry air forms overtop. As the
ground cools, the warm, moist air is cooled quickly. As the
air temperature lowers, small droplets of water condense,
which we see as fog.
Radiation fog forms
most often on cool, clear nights with a very slight breeze.
It forms first in low valleys and spreads outward so long as
conditions remain the same.
Make Your own Fog in a Bottle!

It's easy to simulate
the formation of radiation fog. All you need are two bottles
with a narrow enough neck that you can stick an ice cube into
the mouth. Fill one bottle about half way with very hot water
(it doesn't need to be boiling.) Fill the other bottle with
about 1 inch of cold water.
After several minutes,
pour out all the hot water but 1 inch. Now place an ice cube
in the mouth of each bottle. Observe what happens in
both bottles.
So What's
Going on Here?
Why does fog form
most often on autumn and winter nights?
How would a
stronger breeze affect fog formation?
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