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A hazy atmosphere can be often recognized when looking bottom down
during a flight. Mostly the haze consists of aerosol particles,
which have grown because of high humidity in the boundary layer
and becloud the view. Predominantly this occurs in the morning and
the evening, when the air slowly cools down and therefore relative
humidity increases. Under these circumstances the top of the atmospheric
boundary layer can be often noticed as more or less sharp "line".
(See also Inversions and
Status nasc.,
Smog
BL Top.) |
Haze2-5.jpg: This haze which is characteristic for the boundary
layer came up at the descent to Sao Paolo in the late afternoon.
The clouds were formed at the upper limit of the boundary layer.
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Haze1.jpg: S. Borrmann, flight from Frankfurt to Heraklion (Crete),
MINOS Field Campaign, 30 July 2001, 3:00 p.m. to 7:30 p.m. |