OmCheeto said:
Lesson #1: I've decided that trying to describe the complex dynamics of the Earth's atmosphere would probably take me 100 years, so I gave up on that.
About all you can do, is look at local phenomena, and try and come up with explanations for "why" "that" is happening "there".
One way to look at fluid air movement due to solar heating versus coriolis, is to take a very general, simple macroscopic view.
First, hot air rises. So one may assume that lighter warmed air in the most direct sunlight, that of the equatorial regions, is generally rising. Second, one may assume that heavier cold air in polar regions is generally sinking. Third, since the Earth is turning, there is a centrifugal force in the mix. The lost "airs" must be replaced to maintain equilibrium, so there is a general centrifugal flow of "heavy" cold air along Earth's surface from polar regions towards the tropics while lighter warm air travels towards the polar regions along the upper atmosphere to replace the "lost" arctic air. In other words the heavy cold air is apparently slung to the outside of the merry-go-round by centrifugal force causing lighter warm air to float both to the top and the middle (polar axis). But this movement is all then affected by the coriolis force.
(photo, caption, courtesy of wikipedia)
In the inertial frame of reference (upper part of the picture),
the black ball moves in a straight line. However, the observer
(red dot) who is standing in the rotating/non-inertial frame of
reference (lower part of the picture) sees the object as following
a curved path due to the Coriolis and centrifugal forces present in this frame.
By viewing the planet from the poles, one may think of the individual molecules of air all behaving like the black ball in the Coriolis animation. If one imagines the disc populated with these loose "balls", and a couple of rules whereby they lose density at the outer circumference and cannot escape from the rotating disc system, it becomes self-evident that the heavier dense balls will continuously flow outward from center, while the lightened balls are forced to return to the center axis. And, while this certain flow occurs, the balls(molecules) will all be observed to curve against the direction of rotation. It does seem that in this context, that solar induced convective air flow may counter and even impede the direction of 24 hour Earth rotation via prevailing trade winds at the equator. I am still thinking about that novel possibility. But more than that, it should represent a seriously influencial overview of our atmospheric wind patterns.
Of interest in the above "air fluid" scenario, water is also a fluid, and a similar convective flow occurs within our oceans called
Thermohaline circulation. Basically colder, heavier salt water is slung towards the equator and lighter warm salt water flows towards the poles to replace it. Since the warm water is lighter, it flows along the surface (warming our breezes) and the "slung" cold water currents flow underneath. It may strike the reader that cold arctic air generally travels down along Earth's surface from the poles "rubbing" against warm water headed the other way and this is so. Regarding this combination, we possibly now have a seriously influencial overview of our earthly weather patterns versus just wind patterns. And in vogue lately, it is supposed in some circles, that rapidly melting fresh water at the poles, could interfere with ocean currents by replacing heavy, cold saltwater, with lighter mass cold fresh water. If the light, cold polar freshwater is lighter than warm equatorial salt water, the entire polar-bound flow of warm surface water could abruptly stop. Without the precious coastal flow of warm water, coastal regions will, at least, assume the bitterly cold winters we in the continental centers (such as North Dakota) suffer. Probably worse, all temporate regions would
again tend to get colder, coast and continent alike, as the Earth suddenly reverts back to it's normal, untempered climate,
that of an ice age. Hot equatorial belt... and huge cold planetary ice caps extending far from the poles. Brrr. Well, maybe this idea is wrong. North Dakota was apparently warmer than the east coast this year.
OmCheeto said:
Although the "Coriolis effect" has been mentioned regarding the forward, backward, and circular motions of parts of the atmosphere, I'm curious:
Q: what factor do fluid shear forces play?
It may be that most of the "frictional heat" energy of wind is dissipated this way rather than planetary surface friction. Since it seems more a widely varying momentary local phenomena, it seems incredibly difficult to model in general terms.
Wes
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