Atlantic hurricanes typically form off the northwest coast of Africa, with winds from inland bringing very hot, dusty air out over the ocean. This leads to upward convection which, if strong enough, becomes sustained. As the upward convection strengthens, storms and precipitation form around it. The storm system reaches a size where the rotation of the planet begins to affect it.
The basic dynamic is the same as with sea/land breezes and
the monsoon: higher-pressure air is moving toward a lower-pressure region.
"The atmosphere is trying to fill the hole," as my professors used to
put it. But The distance the winds are traveling is great enough that the
rotation of the earth diverts them. In the northern hemisphere, the winds are
diverted to the right; in the southern hemisphere, to the left.
The result is a coherent storm structure with an eye, filled
with placid, low-pressure air, extending from a few tens to a few hundred miles
across, surrounded by a cloud wall and then the bands of storm clouds rotating
at high speed. In the northern hemisphere, the storm winds rotate
counterclockwise around the eye; in the southern hemisphere, clockwise. So long
as the storm is over warm water, it can continue drawing on the warm vapor to
sustain and strengthen the convection. It is now a mature hurricane.
The National Weather Service established several categories
for tropical and subtropical storms. Among those are tropical depressions,
storms with sustained winds of 38 mph (17 m/s) or less, and tropical storms,
with sustained wind speeds of 39 mph (17-33 m/s). When a storm has reached
tropical storm strength, it is named by the National Weather Service. When it
passes 74 mph sustained wind speed, it's a hurricane.
Tomorrow: Hurricanes part 2: maturity to dissipation.
Be well!
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