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Central PA Winter 25/26 Discussion and Obs


MAG5035
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0Z TUES UKMET/ EURO ENSEMBLE SNOWFALL MAPS: these maps are based on 10 to 1 snow ratios. Jan 24-25 will see arctic air in Mid Atlantic/ TN valley so these snow maps could be UNDERDONE #wxtwitter #vawx #mdwx #wvwx #dcwx #pawx #phlwx #rvawx #ncwx #rduwx #njwx #nywx #nycwx #ohwx #kywx #tnwx
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4:49 AM · Jan 20, 2026
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1 minute ago, Itstrainingtime said:

Anxiously following and pulling hard for you guys! Can't believe I might miss something special. Reel it in.

48 here in Cocoa Beach. That's not too bad until you factor in a north wind at 17 gusting to near 30. Coldest I've experienced here since 2006.

I think You need to cut your vacation short and head home immediately to potentially enjoy the festivities that mother nature could provide.

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Anxiously following and pulling hard for you guys! Can't believe I might miss something special. Reel it in.
48 here in Cocoa Beach. That's not too bad until you factor in a north wind at 17 gusting to near 30. Coldest I've experienced here since 2006.

When I went to Disney world a few years ago between Christmas and NYE I was terrified I would miss a big storm.
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From Google AI-

Key Methods for Determining Snow Ratios in NBM:
  • Temperature-Based Algorithms: The SLR is highly dependent on boundary layer and low-level temperatures (surface to 850 mb). Generally, colder air results in higher ratios (fluffy, dry snow), while temperatures near freezing produce lower ratios (wet, dense snow).
  • Melting Rates for Marginal Temperatures: For temperatures at or above 32°F, the NBM v4.2 incorporates idealized melting rates. The total SLR is reduced based on the ratio of melting to accumulating snow, effectively lowering the ratio if the snow melts as it falls.
  • Dynamic/Algorithm-Based Ratios: Instead of a default 10:1, the NBM uses algorithms that consider factors such as:
    • Wind Speed: Higher wind speeds can lead to lower ratios due to snowflake fracturing.
    • Cloud Structure: The presence of supercooled water droplets (higher riming) vs. depositional growth influences the ratio.
  • Ensemble Member Blending: The NBM uses output from several models (HRRR, GFS, ECMWF) to calculate a probabilistic snowfall, utilizing the best-performing models to determine the most likely ratio for a given area.
  • Elevation Adjustments: Ratios are adjusted upward at higher elevations to account for colder, drier conditions in mountainous terrain. 
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