How can a LLC continue to exist without convection ?
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How can a LLC continue to exist without convection ?
What are the mechanics involved in continuing the strong circulation in
Franklin, if the main convection is displaced as in current VIS ? I'm just
trying to understand some of the dynamics of what I can see versus fluid dynamics or whatever you'd like to call it. Thanks.
Franklin, if the main convection is displaced as in current VIS ? I'm just
trying to understand some of the dynamics of what I can see versus fluid dynamics or whatever you'd like to call it. Thanks.
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Think of the air in 3D. Just because the convection may be gone along with the feedback mechanisms, you still have a "depressed" pocket of low pressure. You see the proverbial naked swirls in the central Pacific a lot long after their upper support headed for California or the Baja. Eventually they'll fill in or be absorbed into some other energy field.
Steve
Steve
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mike18xx
Pebbles wrote:Imagine you have a top... your fingers spin the top and you let go... top still spins even thought your not giving it energy anymore. The spinning motion takes a while to slow down before the top falls over.
Now imagine a tropical storm, clouds are the fingers. Storm is the top....
If you spin a top in the southern hemisphere, which way does it rotate?
j/k
And why do they call it a "top" anyway?
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