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Old 11-04-2009, 02:58 PM   #1
Jody Radzik
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Default Confirmation of Richardson's power laws to make models better

http://www.newscientist.com/article/...ls.html?page=1

These findings might solve the problem of parameterisations, making the models much more granularly accurate.
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Old 11-05-2009, 07:00 AM   #2
Mike Kovalchick
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Default Tomorrow's weather: Cloudy, with a chance of fractals

EDIT: Remove. Existing new thread here:
http://www.stormtrack.org/forum/showthread.php?t=22241


Interesting article that suggests an excellent possibility that forecast models can be vastly improved using fractals.

http://www.newscientist.com/article/...html?full=true

..."The results point to a new view of the atmosphere as a vast collection of cascade-like processes, with large structures the size of continents breaking down to feed ever-smaller ones, right down to zephyrs of air no bigger than a fly...."

..."The implications promise to transform the way we predict everything from tomorrow's local weather to the changing climate of the entire planet. "We may never be able to view the atmosphere and climate in the same way again," says team member Shaun Lovejoy of McGill University in Montreal, Canada...."

Last edited by Mike Kovalchick; 11-05-2009 at 07:08 AM.
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Old 11-05-2009, 11:05 AM   #3
David Wolfson
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Default

Boiled down, the essential point is that many random (in the sense of stochastic) processes are self-dependent over a wide range of scales rather than composed of independent elements following a Random probability distribution. Many statistics of such processes are defined by a skewed "fat tail" distribution rather than the Gaussian bell curve.

The multifractal components of the Earth's atmospheric circulation are clear, i.e. "understood", when you look at the distribution of the model ensemble runs for example. The result of stochastic initialization is a lot more variation and skew than a Random distribution. However the ensemble mean is still an attractor for practical purposes. Theoretically it's possible for a butterfly in the west Pacific to result in an ice-ball Earth but the probability is vanishingly small.

The real question I see that is posed to the modelers is whether some initialization parameters to Bayesian/Monte-Carlo ensembles are incorrectly generated. I'm not in the know on this, but I suspect that this is being considered, because very smart people are involved. For example, snow/ice cover isn't distributed randomly, so its parametric values in Monte-Carlo simulation shouldn't be generated from a Random distribution. FWIW.
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