Un organised winds in an upper air profile i.e veering or backing with height in an un organised manner will always be chaotic in nature and difficult to predict than to the organised [definite shear]upper profile winds. Most of the time this type of WINDS produces violent TS with light to moderate rain and becomes [1] micro burst or macro burst.Lines of this cells having un sheared winds with no definite organisation may turn to be a line squall.
Un organised winds in an upper air profile i.e veering or backing with height in an un organised manner will always be chaotic in nature and difficult to predict than to the organised [definite shear]upper profile winds. Most of the time this type of WINDS produces violent TS with light to moderate rain and becomes [1] micro burst or macro burst.Lines of this cells having un sheared winds with no definite organisation may turn to be a line squall.
ReplyDelete