The amount of energy that a storm produces far outweighs the energy produced by one nuclear weapon. Additionally, radioactive fallout from such an operation would far outweigh the benefits while not altering the storm.

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The energy released from a hurricane can be explained in two ways: the total amount of energy released by the condensation of water droplets (latent heat), or the amount of kinetic energy generated to maintain the strong, swirling winds of a hurricane. The vast majority of the latent heat released is used to drive the convection of a storm, but the total energy released from condensation is 200 times the world-wide electrical generating capacity, or 6.0 x 10¹⁴ watts per day. If you measure the total kinetic energy instead, it comes out to about 1.5 x 10¹² watts per day, or ½ of the world-wide electrical generating capacity. While the latent release of heat feeds a hurricane’s momentum, only a small fraction goes into wind energy.  Much more is fed back into the ocean surface as wave energy.

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Throughout the tropical atmosphere there is abundant energy that forces convection.  However, tropical cyclone formation requires other favorable conditions such as low shear, instability, and mid-level moisture. These variables don’t often coincide, which is why cyclogenesis is fairly rare.

These factors vary with the seasons.  In the Atlantic, it is usually in mid-August to mid-October when the subtropical ridge moves northward enough to allow the deep tropical flow to push disturbances off Africa over the warm seas. These African Easterly Waves are pressure fluctuations in the lower troposphere (ocean surface to 3 miles above) that travel from Africa at speeds of about 3mph westward as a result of the African Easterly Jet.  About 85% of intense hurricanes and about 60% of smaller storms have their origin in these African Easterly Waves.  The rest of them form from old frontal zones over warm water or from subtropical disturbances from the mid-latitudes.

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Si un huracán se mueve hacia el oeste, el lado derecho estaría al norte de la tormenta, si se dirige al norte, entonces el lado derecho estaría al este de la tormenta. El movimiento de un huracán puede dividirse en dos partes: el movimiento en espiral y su movimiento hacia adelante. Si el huracán se está moviendo hacia adelante, el lado de la espiral con vientos paralelos y orientados hacia adelante en la dirección del movimiento irá más rápido, porque estás sumando dos velocidades. El lado de la espiral paralelo al movimiento, pero que va en dirección opuesta será más lento, porque debes restar la velocidad que se aleja (hacia atrás) de la velocidad de avance.

Por ejemplo, un huracán con vientos de 90 mph que se mueven a 10 mph tendría una velocidad de viento de 100 mph en el lado derecho (movimiento hacia adelante) y 80 mph en el lado con el movimiento hacia atrás.

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Prior to the late 19th century, hurricane were named after the fact, usually after saints’ feast days or unusual circumstances. In 1896, Clement Wragge, chief of the Queensland Weather Bureau, began using women’s names for tropical cyclones near Australia.  While the practice lapsed for several decades, it was revived by Army Air Force meteorologists during World War II.  The US Weather Bureau adopted woman’s name lists officially in 1953 for Atlantic hurricanes. In 1979, the lists were modified, alternating men and women’s names.

Today, name lists are maintained by the United Nations World Meteorological Organization for multiple oceanic basins. Most lists rotate every few years.  In the Atlantic, it rotates every six years.

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