The Physics of Hurricanes

Understanding Tropical Cyclones

© Katharine M. J. Osborne

Hurricanes have hit the popular consciousness hard - the increased hurricane activity has everyone worried - but how do they work?

Hurricanes, which are also known as typhoons in Asia, and are more properly called tropical cyclones, are amongst the most damaging and deadly natural phenomena. Recent years have seen an increase in tropical cyclone activity, due in part to a natural cycle of activity, but likely due to global warming as well. Warm tropical water is key to the formation of tropical cyclones.

Tropical cyclones typical form in the ocean about 5 degrees from the Earth's equator over water heated to about 26 degrees Celsius to a depth of about 50m, though tropical cyclones can form elsewhere. In 1996 for instance, a tropical cyclone briefly formed over Lake Huron in the middle of North America. Typically though, tropical cyclones require the coriolis effect in order to form, which gives the storm it's rotation. This effect is greatest nearer the equator. Cyclones also require low wind shear to form, meaning that wind speeds and directions close to the surface of the ocean aren't much different from wind speed and direction higher in the atmosphere. High wind shear will tear a storm system apart.

The interior of a forming cyclone is like a huge heat engine. Warm surface water evaporates and rises as moist air high into the atmosphere. As it reaches the top of the troposphere, the layer of the atmosphere in which weather takes place, the moist air condenses. This converts heat to a tiny amount of mechanical energy. This mechanical energy adds to a down draft of wind on the outside of the system, which falls to the ocean surface and helps to pick up more moist air. This starts a positive feedback loop that helps to increase the formation of the system.

Tropical cyclones actually help to cool the ocean by drawing heat out and converting it into mechanical energy (wind). They can carry this energy pole-ward, so that along with ocean currents, no one area of the ocean becomes over heated. Even this balance is limited. As the overall amount of energy in the Earth's atmosphere increases, more and more tropical cyclones will form.


The copyright of the article The Physics of Hurricanes in Physics is owned by Katharine M. J. Osborne. Permission to republish The Physics of Hurricanes must be granted by the author in writing.



Comments
Aug 30, 2006 1:30 PM
Joy Butler :
Very interesting. As one who lives in a hurricane area, I was amazed to learn that they can be useful for cooling the ocean. The Gulf of Mexico has been unusually inactive this year but I hope it stays that way!
Sep 3, 2006 7:37 AM
Katharine M. J. Osborne :
The Earth has an elaborate system for distributing heat - hurricanes and other weather systems are a part of that, but most of the distribution happens in the network of linked ocean currents. Warm water at the equator gets pulled along into cooler water nearer to the poles. Meanwhile, cooler water gets pulled towards the equator.

Water actually has a high capacity to absorb heat, higher than many other materials (which is why you can plunge glowing hot metal into water without heating the water significantly). The oceans help make the Earth temperate and friendly to life.
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