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2012 Winter Banter Thread #3


yoda

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The RGEM seems to always show the snowiest solution possible.

A very general bias amongst the RGEM is it has a tendency to be very "amped" under stronger magnitude systems although the bias isn't as bad as the NAM sometimes. It can be highly useful with very intense systems (think Groundshog Day Feb 1 2011...it was the best guidance within day 2). I do, once again, under general guidelines, think thr RGEM is a much better numerical model than the NAM, but it is prolly a bit too intense here.

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  • ddweatherman algorithm:
    IF
    >GFS is solid hit
    THEN
    >NO errors in model or int.
    IF
    >GFS further south
    <AND/OR>
    >GFS shows sharp cutoff >SOUTH of ddweatherman
    THEN
    >GFS has int. errors OR convective feedback OR missing ROAB data OR GFS node infected by ILOVEYOU virus.
    :lol:

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ddweatherman algorithm:

IF

>GFS is solid hit

THEN

>NO errors in model or int.

IF

>GFS further south

<AND/OR>

>GFS shows sharp cutoff >SOUTH of ddweatherman

THEN

>GFS has int. errors OR convective feedback OR missing ROAB data OR GFS node infected by ILOVEYOU virus.

lolz

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we won't have 10:1 ratios thru the event.. maybe in solid banding etc (should it occur). so i think to get to 4-5" we'd need like .6-.75" qpf or something. that seems a pretty far stretch based on the euro and gfs. not to say it's impossible but it seems unlikely.

Ooops, you caught my typo...I meant 2.4 - 3.5.

I fully expect error-laden snow though. Make no initialized mistake about that.

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ddweatherman algorithm:

IF

>GFS is solid hit

THEN

>NO errors in model or int.

IF

>GFS further south

<AND/OR>

>GFS shows sharp cutoff >SOUTH of ddweatherman

THEN

>GFS has int. errors OR convective feedback OR missing ROAB data OR GFS node infected by ILOVEYOU virus.

Oh skippy :lol:

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