最終更新日:2022/12/22
例文
The
direct
heat
of
the
sun,
shining
through
so
thin
an
atmosphere,
must
be
considerable
wherever
the
sun
is
at
a
sufficient
elevation;
and
of
course
the
very
tenuity
of
the
air
renders
vaporization
so
much
the
easier,
for
the
boiling
point
(and
consequently
all
temperatures
of
evaporation
at
given
rates)
would
be
correspondingly
lowered.
Accordingly,
during
the
greater
part
of
the
Martian
day,
the
hoar
frost
and
whatever
light
snow
might
have
fallen
on
the
preceding
evening
would
be
completely
dissolved
away,
and
thus
the
ruddy
earth
or
the
greenish
ice-masses
of
the
so-called
oceans
would
be
revealed
to
the
terrestral
observer.
復習用の問題
The direct heat of the sun, shining through so thin an atmosphere, must be considerable wherever the sun is at a sufficient elevation; and of course the very tenuity of the air renders vaporization so much the easier, for the boiling point (and consequently all temperatures of evaporation at given rates) would be correspondingly lowered. Accordingly, during the greater part of the Martian day, the hoar frost and whatever light snow might have fallen on the preceding evening would be completely dissolved away, and thus the ruddy earth or the greenish ice-masses of the so-called oceans would be revealed to the terrestral observer.
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