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#11
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In the Jan. 2004 issue of Model Aviation, in the Radio Control Soaring
column, Real Smart Guy candidate Mike Garton proposes a "condensation analogy" to suggest places to look for thermals to trigger. Imagine water condensing on a ceiling: it drips first from the low spots or tiny bumps. Now imagine heated, but relatively stable, air along the ground. If it's "trying" to rise, might it not "drip up" first from the higher spots, little hills, even trees? If it's moving slowly horizontally, and encounters a tree line, it might be forced up enough to trigger a thermal. His experience with models supports the theory on the small scale. Does y'all's experience support it at the larger scale? Roger Worden Same thing with sandy areas - the books say to avoid them like the plague, but the sandy washes here in Arizona are also consistent thermal sources - and like the ponds/tanks, are low discontinuities in the local terrain. In this case, I'm sure it's not the sand that is causing the thermal, my uneducated guess is that the wash channels (or collects) the incipient themal until it gets big and strong enough to break loose. Any Real Smart Guys out there care to give us a serious possible explanation for these effects? - or maybe we need to keep this to ourselves and let the youngsters figure it out for themselves! Got to keep a few tricks in our bags, you know, something about age and experience beating youth and skill... Kirk |
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