字幕表 動画を再生する
>> This animation is going
to describe how precipitation
happens at what are called
cold fronts and warm fronts.
These are weather systems
that develop wherever masses
of cold air collide
with masses of warm air.
And the name actually comes
from war where armies would
meet along a battle line
called a front, and one way
to think about the difference
between cold fronts
and warm fronts is to think
about which mass
of air is going
to win the battle.
So, we'll start
with a cold front.
This is a situation
that happens
where cold air moves
in like a big wedge underneath
warm air.
Cold air is always heavier
than warm air
and so it's denser
and it's going to tend
to slide under the warm air
and push the warm air upward.
Anytime you have air rising
upward, it's going to expand
and cool and lose its ability
to hold moisture
and this will give you a band
of clouds and precipitation
along a cold front.
On weather maps,
if you watch the weather
on the news,
you can see cold fronts marked
by lines of blue teeth
that point
in the direction the cold air
is moving.
Along cold fronts,
you typically have very
intense local thunderstorms
and rainstorms.
So, it might pour rain
for a short time
but then quickly--usually
within an hour
or so--the front will have
moved on.
So, cold front is
where the cold air pushes
underneath the warm air
and you have high rainfall
and usually
intense thunderstorms.
Now, the warm front has
in common a couple of things
with the cold front.
One is that the warm air still
goes up on top
of the cold air,
but in this case the warm air
is actually pushing the cold
air out of the picture,
so the warm air is winning
and that's how you can
remember if it's a warm front.
The warm air pushes
against the cold air squeezing
it out like imagine squeezing
a watermelon seed
between your fingers,
it kind of squeezes out,
right?
And as the air pushes,
it also rises
up over the cold air.
Rising air again loses its
ability to hold moisture
and you tend
to get clouds and rain.
Along warm fronts you
typically have more mild,
more mellow, more spread
out rainstorms rather
than really local
intense thunderstorms.
And if you're looking
at the weather on the news,
they mark warm fronts on maps
with red half moons that point
in the direction
that the warm air is pushing
the cold air.
So, that's cold fronts
and warm fronts,
major precipitation belts
in many places on the Earth.