I made a more basic introduction to Skew T, Log-P diagrams for meteorological analysis that might be helpful for beginners to watch before diving into this video. It can be viewed here: ru-vid.com/video/%D0%B2%D0%B8%D0%B4%D0%B5%D0%BE-7p7c85hhgOo.html
Patrick! You produced a great video clarifying the basic principles and how the five lines on the graph illustrate atmospheric tendencies. For all who have question marks in their heads or are struggling to put together this Wx info, above, skip over to Patrick’s video to reinforce how all this stuff works, then move on to the next video in this series. Thanks, Patrick!
@@yodingdongyo the bare basics are. To fully understand is a bit beyond freshman. But being so incredibly smart Jim, I am sure it is elementary for you
It is likely the parcel path. On this Skew T (see the link below) for example, the yellow line is the path that the rising air parcel takes as it ascends. The parcel path follows the dry adiabatic lapse rate until the LCL and then follows the moist adiabatic lapse rate thereafter. vortex.plymouth.edu/cgi-bin/upa/gen-raobplt.cgi?id=KOKX&pl=skewt&cu=la&pt=parcel&size=640x480&pg=web
Need a little more help with SKEW-Ts? First watch Paul Castleberry’s digestible series and THEN come back to this briefing. I promise it’ll make more sense. ru-vid.com/video/%D0%B2%D0%B8%D0%B4%D0%B5%D0%BE-VrBVFmALnvo.html
