by beaky » Thu Mar 17, 2005 5:18 pm
The "thin streams" in that picture look like vortices that are visible because of the same thing as the "wing-clouds", but I've only seen that off wingtips. A vortex like that is formed because the air underneath the wing is "trying to get out from under" and a great deal of it travels out towards the tips as well as straight to the trailing edge. Once it reaches the end, it tends to curl up and inward. It's a lot like a breaking wave in the ocean- and in the case of a very heavy airplane moving slowly (such as during takeoff climb), they can be almost as powerful. Needless to say, after breaking free of the bottom surface of the wing, that airflow is going to speed up for a bit as it releases its energy, which could produce that acceleration-induced cooling I mentioned earlier, as well as a lot of energy. They're usually invisible, but that factor (with high humidity) dust, or passing through smoke or clouds can render them visible. There's a very well-known air-to-air picture of a bizjet skimming clouds and leaving lovely big vortices behind; unfortunately I don't have a link.
Contrails are due to water vapor and possibly other stuff in the exhaust, but the condensation in that case is due to the chilling effect of high-altitude air, as opposed to acceleration. Next time you see a jet laying down contrails, watch them for a while... sometimes they "turn into" clouds. They're the same thing: water vapor condensing (and sometimes freezing) due to a drop in temperature.
Last edited by
beaky on Thu Mar 17, 2005 5:26 pm, edited 1 time in total.