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Old December 30th 03, 12:33 AM
Dave Nadler YO
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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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