Cumulus mediocris homogenitusSteam cloud
External Quote:Clouds may also develop as a consequence of human activity. Examples are aircraft condensation trails (contrails), or clouds resulting from industrial processes, such as cumuliform clouds generated by rising thermals above power station cooling towers. Clouds that are clearly observed to have originated specifically as a consequence of human activity will be given the name of the appropriate genus, followed by the special cloud name "homogenitus". For example, Cumulus cloud formed above industrial plants will be known as Cumulus (and, if appropriate, the species, variety and any supplementary features) followed by the special cloud name homogenitus; for example, Cumulus mediocris homogenitus.
Did some looking into the term you quoted Mike and it looks like it, along with Contrails has just been added to the Cloud Atlas in the last few months, one thing that I always thing of when seeing images like the one above and also the one used in the Cloud Atlas, is all the times that TV media when talking of industrial pollution use shots of cooling towers billowing steam into the air as a visual shorthand for 'nasty chemicals'. I think these new clouds are going to have a bit of a perception issue.
It's one of this things that you simply don't notice and yet happens quite often. A few days ago someone asked me about a "odd small black cloud", pointing it out in the sky. It was just a cloud like this - low cloud shadowed by some distant cloud bank.Even small fluffy cumulus clouds look almost black while the more distant ones are bright white.
Yes this one was on a day with lots of towering convective clouds, heavy downpours interspersed with sunshine. Made for some good cloudscapes, but the contrast in colours here caught my attention.It's one of this things that you simply don't notice and yet happens quite often. A few days ago someone asked me about a "odd small black cloud", pointing it out in the sky. It was just a cloud like this - low cloud shadowed by some distant cloud bank.
Cumulus mediocris homogenitus
Panorama showing the extent of the pattern:
I have come to the conclusion by intuition, and observation, that these occur when RHi of the surrounding air is just below 100%, and the 'core' of the contrail is just above. x The plane also needs to be a 'big bugger' x. Edit: It _helps_ if the plane is 'big bugger'.A squiggly contrail...View attachment 6437
And the same area like 2 minutes later:
View attachment 6438
Not exactly correct. Medium-sized planes, like E170 can produce these squiggly trails too:I have come to the conclusion by intuition, and observation, that these occur when RHi of the surrounding air is just below 100%, and the 'core' of the contrail is just above. The plane also needs to be a 'big bugger'.
Not exactly correct. Medium-sized planes, like E170 can produce these squiggly trails too:
Source: https://youtu.be/cqd6sJnQWN4
It all boils to the RHi of the mixture of exhaust and surrounding air at the distance behind the plane, where it got entrained into the wake vortices. The vortex-entrained trails became "insulated" from further mixing and last longer than non-entrained parts. If RHi of the entrained mixture is above 100%, the vortex-entrained trails will eventually end up by the Crow instability mechanism, otherwise they would dissipate before they the vortices break up.
If the surround air is supersaturated too much the resulting contrail will envelope the wake vortices. There still will be more dense trails inside them, which eventually will break up (by the Crow instability) with the formation of contrail pendules.If the surround air is supersaturated too much latent heat is released which breaks up the trail, I think.
Looks like part of a halo, not iridescence.View attachment 30336 Back in Cali for the Holiday...took a post Thanksgiving jaunt to Fallen Leaf Lake (Tahoe area) and noticed this irridesence (i dont think its a sun dog but maybe?)
Looks like part of a halo, not iridescence.