The wave behind the Isabel is rapidly weakening. Why?
IMHO it is because the electrical capacitive coupling over Isabel was
too strong for the wave.
Let's review. A tropical storm is a point EMF negative ionospheric
event. This event couples with the ocean in a capactive manner. The
other charge is attracted. So under the center the ocean becomes
relatively POSITIVELY charge. The other charge is then attracted
around the POSITIVE charges and hence the oceans become strongly
negatively charged. This COULD strenghten the wave except for one
thing--the nearby land--Africa. The large degree of negative charges
in the oceans results in the coast having an electrical difference
with the ocean, and the ocean being much more conductive than the
land. The clouds appear, then, to peel off the wave north to the
You could see it on the loops with Fabian as it melted wave after
wave behind it . . .
As I have mentioned here several times, pertaining to Dr. Gray's
failed West African rainfall statistics, the dams have shifted and
intenstified the CV season.
As Isabel eats up the wave behind it and strengthens, the mechanism
is clear. A delay when sed and flow occurs behind a dammed river in
West Africa changes the season for the blooms. This delays it to time
with tropical storms and off shore blooms and warmer, more conductive
and energitic periods. It is actually the thing of climate shifts,
such as the difference between a Sahara desert and a Sahara monsoonal
condition . . . all it would take is a coastal biosphere such as
blooms and hydrate fields and the entire Med becomes convective.
As Isabel eats the wave, what it is doing is sending a relatively
strong negative charge that rings the storm at ocean level not just
to the wave behind it but to the West African shore. This in turn
causes a difference, electrcially, between ocean and land. With any
convection, then, particularly along the shoreline, shorts to ground
occur on the land side, and make for positive voltages in the
ionosphere to further support the relative negative differential of
the point event. So essentially the shoreline based strikes on the
West African coast power up the point negative center, largely at the
expense of the electrical pattern of the wave behind the storm, and
there you go. Isabel strengthens as the wave becomes EMF unstable and
disapears, seemingly wisked northeast along the African coast.
Meanwhile, the monsoon electrically heats up southwest of here in the
four corner states. This causes patterns of colder air to be blocked
and drops colder Arctic air down south. Soon it will be the rainy
Consider the neo glacials. Extremely electrified states causing
blockages and Arctic drop downs--glaciers are first built,
historically, along the Canadian coast. That's the problem--the
monsoons can actually be TOO strong . . . on a living earth.