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And, don't forget about Saskatchewan Screamers.
Can anyone explain a miller b type of storm they are talking about. Sent from my SPH-L710 using Tapatalk
Eric would you care to explain what gfs feed back problems that hun is sayingSent from my SPH-L710 using Tapatalk
When specific thresholds in the mass fields are met, convective scheme is triggered and then dumps a large amount of QPF over a grid point - releasing so much latent heat over the grid point that the model is forced to adjust the mass fields by producing a local vertical motion max in the mid troposphere (~ 500mb), a corresponding upper level jet max over the vertical motion max - an intense and small scale vort max in the mid levels (MCV).The model scales up the mesoscale circulation at mid levels and holds onto it as a real feature for as long as 3 days. The model can produce precipitation in association with the feature as it tracks along in the flow.
With the Pacific moisture flowing in the west will that limit the movement in the noth pole of the bitter cold? Will it shove the bitter cold to another part of the globe? Lastly how was spring 1986 in general. Thank yourSent from my SPH-L710 using Tapatalk
Back when I was in NJ Miller B's where the systems that constantly screwed us over with snow fall, or better siad, lack there of.