(Sc)
|
Height of base: |
Between 600 and
2000 m (2000-6500 ft) (low-level clouds) |
|
|
Description: |
Distinct layer of
heaps and rolls, dark shading in
base; bright on top loose layers,
elements are touching >5º across,
larger than the width of 3 fingers across at 30º above horizon |
|
|
Occurrence: |
World-wide; most
common cloud genus |
|
|
Made of: |
water droplets |
|
|
Precipitation: |
Mostly none; occasionally
light rain or snow reaching ground |
|
|
Formation: |
-
cumulus
can join by accumulating under a temperature inversion -
stratus
can develop thermals by preferential temperature increase at bottom versus
colder tops |
|
|
Species: |
Stratiformis, lenticularis,
castellanus |
|
|
Varieties: |
Opacus,
translucidus, perlucidus, undulatus, duplicatus, radiatus, lacunosus |
|
|
How to
distinguish from … |
Cumulus (Cu) |
Cu do not touch,
Sc has flatter top |
|
Altocumulus (Ac) |
Cloud elements are
smaller than 3 fingers width at 30º above horizon Higher than 2000
m |
|
|
Stratus (St) |
St indistinct
layer with much less variation in tone than Sc layer |
|
|
Stratocumulus with embedded
congestus and Calvus (see rain core) Morris, Sep06 |
Stratocumulus stratiformis
perlucidus (Morris, November 2006) |
Stratocumulus stratiformis
opacus (Morris, January 2007) |
|
Stratocumulus, End of passage of a warm front Glenwood, Sep 08 |
Stratocumulus castellanus Morris, July07 |
|
|
|
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Last
modified: 1/18/2008
Maintained
by Sylke Boyd
The views and opinions expressed in this page are strictly those of the page author. The contents of this page have not been reviewed or approved by the University of Minnesota.