It is important for the forecaster and analysist to distunguish between various low level weather systems that affect South America. In the special session on 13 August, we explored the characteristics of fronts, troughs, and shear lines. In this additional session, we will finish the topics of lines of instability, and the South American Converence Zone. Please connect 10-15 minutes before the session, we will start promptly at 15 UtC.
Prerequisites: If you did not participate in the 13 August session, please review the recording (parts 1 & 2) available here: http://rammb.cira.colostate.edu/training/rmtc/fg_recording.asp