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The 1998 hurricane season is passing its prime with new hurricane candidates forming for the CAMEX-3 team to study. Meanwhile, the CAMEX team plans a set of flights with the DC-8, ER-2, and Citation aircraft to take measurements in support of the Tropical Rainfall Measuring Mission (TRMM). Right: A rainbow brushes the propeller tips on an Air Force WC-130 Hurricane Hunter. This picture was taken as the crew returned from a day of patrolling Hurricane Frances which, by Monday morning, had worn itself down to a tropical depression (see GOES image, below left) soaking the coast of Texas. (Click here for information of the Hurricane Hunters) On Monday, the DC-8 and Citation flew through convective weather cells off Cape Canaveral while the ER-2 stayed at Patrick AFB, Fla., because of strong crosswinds. "Climatologically, we are nearing the end of the Cape Verde (Africa) season," wrote meteorologist Ed Bensman in today's forecast. The Atlantic Ocean off Cape Verde is where a large number of hurricanes are spawned in the late summer (in addition to those that form over the Gulf of Mexico). They then pick up energy as they range westward and then slam into the American southeast.
In the tropics, the 1008mb low northwest of the Cape Verde Islands moved to the north and dissipated. To the south of the islands a new, better-organized low emerged off the coast of Africa overnight. Satellite animation of this feature clearly shows low-level organization and rotation. The system is currently near 10 deg. N, 20 deg. W and is moving toward the west. This is the most impressive wave in the last few weeks to emerge from west Africa. Left: An infrared image from GOES-8 Monday shows rainstorms, but no large, organized activity. Closer to the U.S., a system continues to feed convection from the Gulf of Mexico northward into the remnants of Hurricane Frances. In the western Caribbean moderate to strong convection continues in this region, but still with little sign of organization. However, most models continue to develop a system in this region with motion toward the Yucatan Channel and then into the central Gulf of Mexico. Over the next 1 to 2 days, the National Hurricane Center will monitor the area of convection off the west coast of Africa. This system should continue to move to the west and may undercut the trough in the central Atlantic. If it does not, it will be sheared by this trough and will likely recurve in the central Atlantic. If this system does move under the trough, it will likely make it to the Lesser Antilles by the end of the forecast period.
Finally, over the next 3 to 5 days, a low off Africa - if it survives the trough in the central Atlantic - will be nearing the Lesser Antilles islands. Given the latitude (10N) that this system emerged from the coast at, it is likely that this low would move across the Caribbean Sea south of the northern Lesser and Greater Antilles. At such long lead times it is impossible to say the exact track of this low. Meanwhile, the CAMEX-3 team is staying busy working as the TEFLUN team - Texas and Florida Underflights - supporting validation of the instruments on TRMM.
CAMEX-3 - the third Convection and Moisture Experiment - is an interagency project to measure hurricane dynamics at high altitude, a method never employed before over Atlantic storms. From this, scientists hope to understand better how hurricanes are powered and to improve the tools they use to predict hurricane intensity. An overview story (Aug. 12, 1998) describes the program in detail. The study is part of NASA's Earth Science enterprise to better understand the total Earth system and the effects of natural and human-induced changes on the global environment. A midterm story (Aug. 31, 1998) reviews the first month of operations and the windfall of data. Because meteorology and aeronautics first used modified nautical charts, their data bases are in nautical miles and knots (nautical miles per hour). In these stories, we use Standard International ("metric") units first, and give more familiar measurements in English units and the original measurements in nautical units. Because of rounding and because the wind speeds originally are expressed in knots, km/h speeds to knots may be slightly different from the numbers in the story.
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Authors: Robbie Hood, Ed Bensman, and Dave
Dooling
Curator: Linda
Porter
NASA Official: Gregory
S. Wilson