They just look like persistent contrails to me.
In one case, you see a broken contrail, as it passed theough an area of the atmosphere where the temperature and/or RH was outside the envelope for
formation of persistent contrails, which -- in that location, at least -- simply sublimed from ice crystals to water vapor.
I mean, a contrail will persist if the ambient temperature at the place where the contrail is formed is below minus forty degrees and the
relative humidity is saturated.
If the temperature is ABOVE minus forty degrees or the relative humidity is BELOW 100 percent, then the contrail (which is just ice
crystals) will sublime back to vapor like dry ice does and the contrail will disappear within a minute or so.
What's so mysterious about that? Haven't you studied anything about meteorology at all?


