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I've seen this effect many times in Australia. Kept finding
lift over small irrigation ponds (altitude several hundred feet). Decided to do an experiment whilst awaiting a buddy who was interminable slow to get airborne. There was an irrigation pond about 1km from the airfield. After losing sufficient altitude doing aero, spoilered down to several hundred feet over this pond, then climbed out and repeated the procedure. Four or five times (like I said, he's slow). The interesting features here (and in Arizona) a - very dry air, and - shallow irrigation tank/pond subject to good heating (warm water) Don't know that I understand the physics, but extremely consistent. Beaver Pond Lift is however a different phenom... Best Wishes for 2004 to all, Dave "YO" Peter Creswick wrote in message ... Mike Rapoport wrote: The moisture doesn't really help lift until the air is fuly saturated and starts condensing releasing heat. Also, the air above the water is cooled by evaporation and is cooler than the surrounding air. I will never say never and I don't dispute your or others experience, but the explanation doesn't make sense to me. Mike MU-2 "Kirk Stant" wrote in message om... "K.P. Termaat" wrote in message ... My experience is that it works, especially on days with very low humidity, but no boomers and only low. "Mike Rapoport" schreef in bericht ink.net... You will find less lift over water of any kind, even if it is contained in vegetation. The best lift is always over the highest, dryest, darkest surface around. The water vapor idea is...well...it is hard to find a place to start...but it won't work Mike MU-2 Have to disagree with you, Mike - out here in Arizona, in the desert areas that are not irrigated, we often find good lift directly over small cattle "tanks" - small shallow ponds that are scattered around. A lot of us have noticed this and compared notes, and it works; if too low to get to high, dark ground, I'll head for the nearest pond and it will usually turn up a nice thermal. We think it may be due to the fact that the ponds are in a natural low spot, and coupled with the little bit of moisture, could be the necessary trigger for a thermal. Now obviously, large irrigated farm fields or river basins are death to thermals - but a local lake (reservoir) seems to have little effect on thermal activity - could it be all the drunk boaters? What's the old saying about never saying never? Kirk LS6-b Have seen similar effects over the small dams on farms here too. My idea is that the air over the water cools by evaporating water out of the pond. In so doing it looses more heat and hence contracts more (gets denser) than it gains buoyancy by water vapour increase, ie, it gets both colder and denser overall than the surrounding surface air. As the dense pool of air becomes greater, it spreads out, ie, sort of collapses on itself, and pushes out over the edges of the pond / dam, particularly down slope over the dam wall, creating a miniature equivalent of a valley wind in the creek or down the slope, thus acting as a wedge trigger to lift the warm dry air off the ground. |
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