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TellicoWx

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Posts posted by TellicoWx

  1. For those new to the hobby, and not quite familiar with the topo and how it greatly impacts the Great Valley hopefully this will help...(and yes there is some truth to the Cattanooga Snowdome lol).

    This generally applies to anafrontal and Northwest Snow Flow Events. Surface LP has a ton of other variables. 

    Think of the atmosphere as a liquid with differing viscosity. Warm is less dense and rises, cold undercuts the warm as if it has a thicker viscosity.

    The Plateau acts like a dam for the denser cold air (Blue Arrows over Middle TN). Just west of Knoxville near Kingston, the Plateau has a natural spillway/funnel that allows as small area for the cold to funnel into the valley (if you watch fronts pass over, you can actually see this occur live on PWS's in the area). There is a much smaller spillway west of Chattanooga, but due to the nature/design of the Plateau, cold must slowly fill the Sequatchie Valley first before trying to continue advancing toward Chattanooga (leaving that area to primarily rely on the Kingston "spillway" to supply it with the cold. As lift generally pulls away from the valley from SW to NE, the column dries the quickest at Chatt. Add in the distance from Kingston to Chatt the slow moving cold air arrives almost too late...hence the Chattanooga Snowdome.

    Other areas of interest due to topo..

    1) Green Box Areas - as the cold naturally pushes SE, it sometimes can force moisture to pool up in these areas, enhancing snowfall output. This is what occurs 9/10x when East of Hwy 411 ends up with greater totals than west side.

    2) Red Boxe Area - The downsloping winds of the Plateau speeds up the drying process further...making the Dome that much stronger.

    962_g_1200x1200.png

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  2. 1 hour ago, PowellVolz said:


    In a anafrontal system, is their elements that can enhance qpf that the mods don’t pickup on? NW flow, steep lapse rates, low level moisture, etc….? I’m assuming it could be rationed higher from cold 850’s?


    .

    In an anafrontal setup some things that models will not have a grasp of at this ramge:

    1) the depth of the shallow low level moisture. This range they have a tendency to sometimes dry the DGZ out to quickly, not picking up on where the moisture banks up against micro climate areas (such as the plateau/foothills etc).

    2) Under estimate how far ahead the shallow arctic air has actually advanced during very powerful cold fronts.

    3) The exact placement of Vertical Velocities. Becomes more important with anafrontal due to having to rely on the UVVs more for the lift, than have the traditional SLP aided lift.

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  3. 5 minutes ago, Knoxtron said:

    Heavy sleet storm just passed Waldens Ridge and put a dusting (?) down really quick. Just east of Dunlap

     

    Edit: Melted quickly, currently 40 and dropping 

    I'm in Madisonville in Monroe Co.. just had quick burst sleet here as well, Temps about same as there

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  4. 1 hour ago, Carvers Gap said:

    It is also very important to look at ensembles.   The means for the 6z GEFS and 0z EPS actually suppress the system like the CMC does, rotate the energy below the forum, and bring it up the coast.  Maybe that is where we want it?  Maybe not.  But I will say, I do think the operationals are driving the bus and catching trends that the ensembles are likely washing out.  Operational trends matter at this point.

    To me there is 2 possible outcomes still being figured out and 1 joker card.

    A) the Hudson Low and 1050+ High dropping down are too far south currently modeled (there placement is what pushes the front thru). Which would mean the Ops are too suppressed. I give that about 40% weight based on this winter of the SE trend, plus climate.

     

    B. Those features are too north and Ops too slow with the front = cold rain, which some ensembles show. Think that is more likely currently on most modeling. 

    And Joker Card...whether or not the wave can generate cyclogenisis along the Gulf. Joker can reck havoc on both A) and B...think that will be an issue foe the next several days.

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  5. 2 minutes ago, Holston_River_Rambler said:

    Euro was pretty close to a storm on the 12th. 

    Jumped the storm SE again, as you guys have said over the past couple days or so, seems to be something this winter to that. With those lofty numbers shown just across the MS river last few days of runs, it will be interesting to see if west TN starts getting into the game for anything within 150 hrs.

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  6. 12z GEFS looks alot better thru the ext (run not complete quite yet), especially for the central and west TN folks. Instead of one storm skewing the mean and the rest kinda of blah, almost each member has some for of storm/s. One member even pushes 2"-4" right to the gulf/FL panhandle area. When ensembles start getting into the 4"-5" means (west/central TN), usually something is coming

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