Jump to content
  • Member Statistics

    17,506
    Total Members
    7,904
    Most Online
    SnowHabit
    Newest Member
    SnowHabit
    Joined

January 3-4 Storm Thread part II


rduwx

Recommended Posts

34 minutes ago, PackWxMan said:

Confidence is continuing to increase that a moderate-high impact winter storm will affect east-central North Carolina as soon as late tomorrow and Thursday. A broad area of low pressure is anticipated to form in relatively short order near or just east of north-central Florida and rapidly intensify as it moves north-northeast and gets awfully close to Cape Hatteras and the rest of the Outer Banks some time on Thursday. Meanwhile, a weak trough of low pressure diving out of Saskatchewan/Alberta and into the Northern Rockies will impinge on the incipient low pressure off the Carolina and Georgia coast, ultimately impacting the large-scale steering flow and track of the rapidly intensifying low which may undergo instant occlusion as the upper level trough eventually overruns it. It needs to be stressed that this setup is exceptionally fickle and most of the standard, coarse grid numerical weather prediction computer models most local meteorologists are looking to for guidance in a situation like are likely going to miss very key, subtle features in the overall pattern that will ultimately have a massive impact forecast and be the difference between extremely heavy snow and next to nothing at all. This includes the placement and intensity of clusters of showers and thunderstorms over the Northeastern Gulf Coast that will develop later tomorrow. The reason the convection (i.e. thunderstorms) over the Gulf coast matters a lot for us in determining whether we get a lot of snow or not is because within these large-scale convective clusters, condensation and deposition (process where water vapor turns into snowflakes) is occurring on a mind boggling scale. These processes release heat into the surrounding atmosphere. As many of you are well aware, the heat released allows the surrounding air to expand, which causes the pressure and the density directly within that mass of air to drop. In the most basic sense, this drop pressure within the clusters of storms actually reflects onto the synoptic-scale low pressure system. This may then allow the low pressure center to deepen or change its track in the direction of where the pressures are falling the most within the convection! Furthermore, the winds spiraling around this center of low pressure that's formed in part from the clusters of storms can help advect (or move/push) Atlantic moisture inland into Carolinas over top of the cold, arctic airmass that's been in place recently. This set of ingredients then leads to potentially large amounts of snow and ice. Therefore, it's important for weather models and local meteorologists to properly analyze, forecast, and correct their forecast mistakes for these groups of thunderstorms hundreds of miles away on the Gulf Coast because they're capable of growing upscale and affecting our weather in a short period of time. Essentially, if these thunderstorms aren't properly forecast then what would be a forecast for little-no snow at all in NC could turn into several inches of heavy, wet snow. Thus, as we roll deeper into tomorrow the growing convective cluster along the NE Gulf coast will begin to spread moisture over the Carolinas. The airmass in place will be pretty dry to start so some of the initial precipitation that moves in from the southwest may have trouble reaching the ground. However, as the low pressure center off our coast continues to intensify and slugs copious amounts of Atlantic moisture inland across east-central North Carolina, areas along/east of US Highway-1 (including Fayetteville & Raleigh-Durham) may not have much trouble receiving a significant dose of moderate-heavy precipitation, which will likely be in the form of snow. Some of this snow may be particularly heavy at times, with graupel and even thundersnow possible over the hardest hit areas. However, if the low pressure center moves closer to the Carolina coast as some models are insisting some of the moderate-heavy snow could mix with or change over to sleet especially the further southeast you go in the state. Given how cold the temperatures have been over the past few days, any snow or sleet that falls will immediately stick to the ground and the roads. Therefore, residents in east-central NC should make preparations in case travel is heavily limited by this storm for a few-several days afterwards. I'm currently expecting at least several inches of snow and/or snow/sleet to fall over NC tomorrow night and into Thursday, especially for areas along/east of US Highway 1, with the potential for 4 to 8 inches of snow to fall generally in and around the US highway 1 and I-95 corridors, with locally higher amounts probable-likely. These numbers are highly variable and expect potentially large future changes as we approach this event. The closest analog I can find to this current storm is the January 2000 event which crippled the Triangle Area and the US-1 corridor. Attached below I provide the mid-level voriticity (essentially spin) and radar forecasts for tomorrow's event and compare those w/ the analyses provided by the NWS RAH and ECMWF's 20th Century Reanalysis (ERA-20C), you should note how uncanny the similarities are While it is not safe at all or very wise to currently expect this storm to pan out EXACTLY like January 2000, the similarities between this winter storm and that event are impressive say the least and those who have lived here long enough are well aware of how bad the forecasts were even the night before the storm struck. Thus, take this forecast with a massive grain of salt as it could change a lot between now and tomorrow afternoon/evening. - ERIC WEBB

Thanks for posting this - when I read this, I don't know if he's going to right or wrong (and he's certainly hedging somewhat), but he's at least using his experience and intuition and explaining his thought process out. I feel better informed. I wish sometimes forecasts from local mets and the NWS went into some more detail like this rather than "we're using a blend of X, Y, and Z model" (or worse just going off of whatever the Euro/EPS says).

Link to comment
Share on other sites

  • Replies 2.8k
  • Created
  • Last Reply
2 minutes ago, ajr said:

Thanks for posting this - when I read this, I don't know if he's going to right or wrong (and he's certainly hedging somewhat), but he's at least using his experience and intuition and explaining his thought process out. I feel better informed. I wish sometimes forecasts from local mets and the NWS went into some more detail like this rather than "we're using a blend of X, Y, and Z model" (or worse just going off of whatever the Euro/EPS says).

image.png.b5ab9f118f766a5d680722860e616a59.png

Secretly hoping to get body slammed by 10 inches of pure white crystal colombian bam bam just so GSP eats a fat slice of HUMBLE PIE!

Sec

Link to comment
Share on other sites

The models are going to have a hard time discerning very specific parameters such as convection and/or dry air overcoming.

If anything, convection would release latent heat to fuel more convection, as Eric Webb said.   No reason to panic.  Even spotty precip is fine because anything that falls will stick with these super cold antecedent temps.  We've had just about the best antecedent conditions you can ask for in NC.

Link to comment
Share on other sites

Archived

This topic is now archived and is closed to further replies.

  • Recently Browsing   0 members

    • No registered users viewing this page.

×
×
  • Create New...