Birthplace of Hurricanes

[C1ay]

"Winds will grow soon to storms in Africa," laments Irish singer Enya in her song, Storms in Africa. She might have added "And hurricanes in the Americas."

 

lefthttp://hypography.com/gallery/files/9/9/8/cyclones_thumb.jpg[/img]Scientists have long known that hurricanes that lash the Atlantic coasts of North and Central America are born in storm systems off the west coast of northern Africa. In an ironic twist, these wettest of storms are driven by weather over one of Earth's driest of places, the Sahara (the name means desert in Arabic).

 

To learn the details of what happens, NASA and university researchers are flying to the west coast of Africa for an international campaign called the African Monsoon Multidisciplinary Analysis, or AMMA. The NASA portion of the campaign is called NAMMA.

 

"We are going to observe the transition of thunderstorms off the coast of Africa into hurricanes that we get in the U.S.," explains Robbie Hood of the Marshall Space Flight Center, a member of the NAMMA science team. "This is an active hurricane genesis region."

 

The scientists will operate during the month of Aug. 15 to Sept. 15 from the Cape Verde Islands, a cluster of 18 volcanic islands in the Atlantic about 300 miles off the west coast of Africa. Dr. Ramesh Kakar of the Earth Science Division, Science Mission Directorate, at NASA headquarters is the program manager.

 

Hurricanes are massive, rotating heat engines powered by the warmth of tropical waters. Category 5 hurricanes can pack winds of 150 mph or more. Hood explained that many of these powerhouses originate with combinations of thunderstorms off Africa. But not all thunderstorms lead to hurricanes.

 

Why not? There's more to the story than warm water:

 

Another ingredient is Sahara dust storms. Dry desert air blowing westward can overrun and weaken Atlantic storm systems. Dust, on the other hand, can serve as nucleation points for water vapor, causing rain. This interplay between ocean and desert is not fully understood.

 

To probe deeper, NAMMA will use NASA's DC-8 Airborne Laboratory. This modified jetliner has been used in NASA's two Convection and Moisture Experiments (CAMEX-3 and -4) conducted in 1998 and 2001. It is equipped with weather instruments to measure winds, water vapor, moisture, atmospheric pressure, temperatures, and the detailed physics of cloud formation and development.

 

NASA will also use weather radar located at both Dakar, Senegal and Praia, Cape Verde, and instruments on NASA satellites such as the Tropical Rainfall Monitoring Mission (TRMM), CloudSat and CALIPSO. The United Kingdom, France and other European nations will operate aircraft and surface instruments out of Dakar, Senegal, on the west coast of Africa. The National Oceanic and Atmospheric Administration's Hurricane Research Division will fly aircraft out of Barbados to measure hurricanes as they approach Caribbean nations, the United States, Mexico, and Central America. During the mission, a Web-based real time mission monitor, developed by Marshall Space Flight Center, will permit scientists to track the progress of the experiment from anywhere on the globe using a standard internet connection.

 

Hood anticipates collecting lots of data. "Our goal is to use the results of this experiment to improve precipitation and hurricane forecasting technology for the future."

 

Source: Science@NASA

[Mercedes Benzene]

I give the article perfect scores... just because it references Enya!

[HydrogenBond]

If one looks at the hot dry air coming off the desert, it is ripe for rapid evaporation when this airs moves over the warm moist eastern Atlantic Ocean. This maximized atmospheric chemical potential (dry-moist) can put a lot of water into the atmosphere is a very short period of time. Once the atmosphere get overdosed with moisture, there is an equally rapid need for condensation into clouds and rain to produce the low pressure disturbances.

 

The dust may play a role after the water content is built up, causing a seeding affect that speeds up the condensation of the clouds. The dust is a bonus that may actually prevent bigger hurricanes from forming. It is analogous to a boiling stone preventing superheating affects, in this case supersatuation affects would build up before the energy could release as storms resulting in bigger storms.

 

This is what is observed. Hurricanes very rarely form off Africa. The dust is a stabilizing affect. After the rains scrub out the dust and if the disturbance remains stable it begins to gather steam closer to the Americas, forming tropical depressions and then hurricanes.