chapter 7: clouds Flashcards
The result of condensation may be
fog, dew or clouds
The conditions of formation of condensation are:
- air must be saturated
- there are generally must be a surface on which the water vapor can condense.
- ascent of air
for any form of condensation the must be saturated. Saturation occurs when
the air is cooled below its dew point or
when sufficient water vapor is added to the air
there are generally must be a surface on which the water vapor can condense. This surface may be
an object at or near the ground where dew can form, or suspended particles in the atmosphere
This surface may be an object at or near the ground where dew can form, or suspended particles in the atmosphere (known as
condensation nuclei
define condensation nuclei
serve as surface on which water vapor condenses
fog forms near …………………….. and cloud at ………………….
the ground and clouds at a height
Condensation nuclei may be
dust, smoke and salt particles all of which are suspended in the atmosphere.
hygroscopics:
Particles that make the most effective cloud condensation nuclei
Particles that make the most effective cloud condensation nuclei are called hygroscopics which means
they are water-absorbent.
……………………………….. are also hygroscopics
Some familiar food items, such cracks and cereal
Some of the most common hygroscopic nuclei are
minute crystals of sulfate and nitrate compounds.
Hygroscopic nuclei are produced into the atmosphere by
burning (forest fires, automobiles and coal burning).
In addition salt from breaking ocean waves and
some particles found in ordinary dust can serve as cloud condensation nuclei
The important cloud-formation is the ascent of air. As a result,
, rising air expands and is cooled adiabatically. At a height called the lifting condensation level, the ascending parcel is cooled to its dew point temperature and further ascent causes condensation.
Clouds are one form of
condensation