3. _Thunder may be expected_ when cumuli of hemispherical form are
characterized by an extreme silvery whiteness.
4. _Rain may be expected_ when cumuli increase in number towards
evening, sinking at the same time into the lower portions of
the air.
[Illustration: 46.
Stratus.]
STRATUS.—As its name implies, this is a horizontal sheet of cloud
formed near the earth at night (whence it has been called “the night
cloud”) by the condensation of moist air from rivers, lakes, and
marshes, or damp ground which has lost its day-heat by radiation,
especially in calm clear evenings, after warm days. It appears as a
white mist near, and sometimes touching, the earth. It attains its
maximum density about midnight, but is dissipated by the rays of the
morning sun. Its formation, watched from a height over a large city, is
highly interesting, and is attributed by Sir John Herschel to the soot
suspended over such localities, each particle of which acts as “an
insulated radiant, collects dew on itself, and sinks down rapidly as a
heavy body.” Still more interesting is it to observe from a similar
elevation the dissipation of this cloud when the sun has attained such
an altitude that its rays fall on the upper surface of the stratus
cloud, which then heaves like the billows of the ocean, while the whole
mass seems to rise spontaneously from the earth, and speedily vanishes
“into air, into thin air.”
1. _The finest and most serene weather may be expected_ when
stratus clouds present the appearances just described.
CIRRO-CUMULUS, or “mackerel sky,” is a well-known form of cloud
occurring in small roundish masses, looking like flocks of sheep at
rest, and often at great heights. It is seldom seen in winter.
1. _Increased heat may be expected_ when cirro-cumuli appear.
2. _A storm or thunder may be expected_ when cirro-cumuli occur
mingled with cumulo-stratus in very dense, round, and close
masses.
3. _Warm wet weather, and a thaw, may be expected_ when
cirro-cumuli occur in winter.
CIRRO-STRATUS “appears to result from the subsidence of the fibres of
cirrus to a horizontal position, at the same time approaching
laterally. The form and relative position when seen in the distance
frequently give the idea of shoals of fish.” It is called “the vane
cloud” and “mackerel-backed sky.”
1. _Rain, snow, and storm may be expected_ when _cirro-stratus_ is
seen alone or mingled with cirro-cumulus, especially if the
cirro-cumulus passes away.
2. _Fair weather may be expected_ when from a mixture of
cirro-stratus and cirro-cumulus the former disappears, leaving
the latter in possession of the sky.
3. _Thunder and heat_ are generally attended by waved cirro-stratus.
Public-domain text, read in full here on John Shaqi.
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