Smiling JOe
SoWal Expert
African tropical waves
An tropical wave near 12N 34W, a few hundred miles southwest of the Cape Verde Islands, has a pronounced surface circulation one can see in QuikSCAT satellite data from 3:52am EDT this morning. The amount of heavy thunderstorm activity has decreased since yesterday, and any development should be slow to occur. The thunderstorm activity associated with this wave was being enhanced yesterday by a process known as upper-level divergence. When the the winds at high levels diverge (blow outward from a common center), then air from the surface must rise to fill the vacuum created. As this surface air rises, the moisture in it condenses, fueling thunderstorms. Thunderstorms created by this mechanism make a tropical disturbance look more impressive than it really is. The wave has moved away from this area of upper divergence, reducing the amount of thunderstorm activity.
The large spiral of low clouds near 18N 45W surrounded by a large cloud of dry air and African dust continues to spin, but the thunderstorm activity near the center has dropped to nearly nil this morning. The wave is under a very favorable upper-level environment for development, with low shear and an upper-level anticyclone on top. However, water vapor satellite imagery shows that the air on all sides is very dry. The GFS model is showing that this wave will not be able to find a moister environment until Sunday at the earliest, when it may be near Puerto Rico or the Bahamas.
I'll be back late this afternoon with an update on Ernesto, John, Ioke, and the rest of the tropics.
Jeff Masters
An tropical wave near 12N 34W, a few hundred miles southwest of the Cape Verde Islands, has a pronounced surface circulation one can see in QuikSCAT satellite data from 3:52am EDT this morning. The amount of heavy thunderstorm activity has decreased since yesterday, and any development should be slow to occur. The thunderstorm activity associated with this wave was being enhanced yesterday by a process known as upper-level divergence. When the the winds at high levels diverge (blow outward from a common center), then air from the surface must rise to fill the vacuum created. As this surface air rises, the moisture in it condenses, fueling thunderstorms. Thunderstorms created by this mechanism make a tropical disturbance look more impressive than it really is. The wave has moved away from this area of upper divergence, reducing the amount of thunderstorm activity.
The large spiral of low clouds near 18N 45W surrounded by a large cloud of dry air and African dust continues to spin, but the thunderstorm activity near the center has dropped to nearly nil this morning. The wave is under a very favorable upper-level environment for development, with low shear and an upper-level anticyclone on top. However, water vapor satellite imagery shows that the air on all sides is very dry. The GFS model is showing that this wave will not be able to find a moister environment until Sunday at the earliest, when it may be near Puerto Rico or the Bahamas.
I'll be back late this afternoon with an update on Ernesto, John, Ioke, and the rest of the tropics.
Jeff Masters