I don't understand this whole "chem-trail" thing.
When water vapor (which is about 99 percent of the exhaust) exits from the engine at typical contrail altitudes (30,000 to 38,000 feet) since it's
very cold, it immediately flashes into ice crystals and so you have a little skinny ice-crystal cloud (which, by the way, is what a cirrus cloud
is).
If the temperature is above minus 40 degrees and/or the atmosphere is not saturated, the ice crystals will sublime (go back to vapor without going
through a liquid phase, just like dry ice does) within a minute or so. These are non-persistent contrails.
If, on the other hand, the temperature is below minus forty degrees and the atmosphere is saturated (RH=100%), then the contrail will
not sublime but will stay around, just like a cirrus cloud in a similar environment does. These are persistent contrails.
Indeed, with persistent contrails, the atmospheric conditions are such that the existing contrail will act as a "seed" and will spread as the
adjacent water molecules (remember, the RH is 100% and the temperature is below minus forty degrees) will solidify into ice, which is why often you
will see persistent contrails spread out into cirrus clouds.
Sometimes the aircraft will pass through a patch of sky where the temperature is just a little bit higher than minus forty, or the RH
is just a little bit less than 100%. In that area, the ice in the contrail will sublime rapidly, leaving the observer with those
"dashed" contrails.
[edit on 11-9-2004 by Off_The_Street]











