JULY/AUGUST 2019. DISCOVER 73
What’s
in a name?
A tropical cyclone is
the official name for these
swirling systems of storms, but
you’ll hear different names based
on their location; specifically, they’re
hurricanes in the U.S. and typhoons
in countries in the western Pacific.
Other places, like Australia and
India, just call them tropical
cyclones.
Hurricane
season typically
extends from
June through November,
though storms have struck
both earlier and later
than that. Just when you
thought it was safe to
move back near the
water...
The Curious Coriolis Effect
Even standing still at the equator, your body’s actually
moving at about 1,000 mph, thanks to Earth’s rotation.
But that speed changes depending on where you
are. The surface — and you,
standing on it — spins
more slowly the farther
from the equator you
get. But winds aren’t
tethered to the
surface like we are.
So, as a gust of
wind moves away
from the equator, it
begins to outpace
the ground beneath
it because the gust
maintains its original
speed while the Earth
slows down beneath it.
As a result, it bends. This
means the wind sucked
toward the center of a tropical
depression or hurricane bends to its right in the
Northern Hemisphere, and to its left in the Southern
Hemisphere. The tension between this motion and
the pull of the low-pressure system at the center of
a storm creates a vortex that spins counterclockwise
in the Northern Hemisphere and vice versa in the
Southern.
This phenomenon — or the lack of it — also explains
why there’s a hurricane-free zone within 5 degrees of
the equator. Coriolis forces, named for French scientist
Gaspard-Gustave de Coriolis, aren’t strong enough to
form a vortex there.
Wind shear is a difference in wind speed over a
short distance. A lot of wind shear — say, if winds
are slow near the surface but fast up in the clouds
— tears apart rising air. When this occurs over the
ocean, it prevents the formation of low-pressure
systems that spawn hurricanes.
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Cameras on the
International Space
Station captured a
view of Hurricane
Florence the morning
of September 12, 2018,
as it churned across
the Atlantic.
The pressure gradient
sucks winds in (blue)
while Coriolis forces (red)
bend them, resulting
in the characteristic
hurricane spin (black).