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#1
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On Monday, November 3, 2014 8:33:24 AM UTC-5, Andy Blackburn wrote:
On Monday, November 3, 2014 3:15:06 AM UTC-8, pete purdie wrote: ...An important finding is that above about one-third of the distance to the inversion, there is no significant temperature difference between the thermal and surrounding air; near the inversion the temperature is actually lower since the warmer air above the inversion is being mixed down around the rising air. Humidity is a significant indicator, H2O molecules being lighter than O2 or N2. So thermals rise, not because of the sun heating the ground and making a bubble of warm air that breaks free, but because somehow a more humid bubble of air is created. What mechanism creates the bubble of humidity? 9B Differences in ground surface condition. There is also a variation in electrical potential between thermals and surrounding air. This was explored in the 70's. UH |
#2
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On Monday, November 3, 2014 5:38:09 AM UTC-8, wrote:
There is also a variation in electrical potential between thermals and surrounding air. Enough to charge the batteries on one's FES? ;-) |
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