On Wed, Oct 28, 2015 at 1:11 PM, Phil Pugliese (via tml list) <xxxxxx@simplelists.com> wrote:
 Hurricanes form and are sustained by transport
 of heat in water
 vapour, requiring huge
 areas of fairly deep warm water.  Cool water
 doesn't produce enough vapour to power such
 strong winds, and cool air
 can't carry
 much anyway.  It takes an enormous amount of sunlight
 energy storing enough heat throughout the water
 to set up the required
 conditions.

Okay. No hurricanes, either before going in or after coming out. Except that in the very next paragraph we get . . .

 

 In the long run, winds are
 driven by differences in average heat
 received from the sun between different areas
 of the planet's surface.


Upon coming out of the particle cloud (and it was a particle cloud not a simple eclipse shadow IIRC), you've got a very cold planet of which an initially-slim crecent starts to warm again. The oceans will (as stated) take a long time to warm, but the land and air will warm up much faster.

Since the driving force of winds is average difference in temp - and on the one hand you have frozen oceans which change temp only very slowly and on the other hand air/land masses which can change temp relatively quickly - wouldn't you get hurricane force winds flowing from the rest of the planet into the warming crescent?

Even once the planet is fully out into the sunlight again, you've still got those frozen oceans (which will remain so for how long?) abutting more temperature-volatile air/land. Wouldn't you get continental-scale "on-shore breezes" during the day, followed by a somewhat-lower scale of "off-shore breezes" at night?

And what about vertical air mixing? The air over the frozen oceans may stay relatively cool, but higher air layers will heat normally.

And wouldn't coralis force cause all these various streams of wind to spin?

--
Richard Aiken

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