National Weather Service United States Department of Commerce

Overview

From 1/21 to 1/22, strong low pressure tracked from the central Gulf of Mexico northeast to about 150 miles off the Carolina coast. At the same time, 1040+mb Arctic high pressure slowly built from the southern Plains to the Lower Mississippi/Tennessee Valleys. Aloft, a sharpening but positively tiled shortwave trough crossed the area during the evening of the 21st through the early morning of the 22nd. Mid level clouds (and forcing for ascent) had already overspread the entire area by the afternoon of the 21st in advance of that shortwave. The very cold, dry low level Arctic airmass was in place over the entire area, with temperatures in the lower-mid 20s (with dew points around 0F!) during the afternoon before any snow had started to fall.

Even though the surface low tracked well to the southeast of the area, mid to upper level forcing for ascent was strong given decent WAA aloft. More importantly, the sloping mid/upper level frontogenesis zone was over the area, with the strongest FGen in the dendritic growth zone (700-550mb) residing over SE VA during the evening-early overnight. Despite the very cold/dry antecedent airmass, light snow began falling as far west as the Richmond Metro by 7 PM. The low-levels then quickly saturated area-wide by 8-9 PM. Most of the snow was light in intensity, but a band of moderate to heavy snow (likely with 1-2”/hour rates) set up across extreme SE VA and NE NC on the warm side of the mid-level FGen zone (see Environment section for more details). In addition, given the very cold temperatures (and forcing for ascent concentrated in the DGZ), snow liquid ratios were 15-20:1 even across NE NC! Also, as the low-levels were so cold (925mb temps were -13 to -16C) and the flow was initially out of the north…some additional enhancement of the snow was observed across Norfolk due to moisture flow off the bay. This is rare in our area, but is exactly like lake enhancement which occurs often in the snowbelt regions of the Great Lakes. The steady snow ended between midnight and 4 AM as the shortwave quickly pushed to our SE, but totals in NE NC were an impressive 3-7” (locally 8”). Southern portions of Hampton Roads saw around 3”, with localized totals around 4” in that area of Norfolk that saw “bay enhanced” snow.

After the steady, synoptic snow ended, a “bay effect” snow band developed as there was very little shear from the sfc to 900mb with the top of that layer in the DGZ. In addition, the difference between the water temperature (38F/3C) and the 900mb temperature (~-15C) was much more than enough for a few hundred J/kg of “bay induced” instability. This combination of factors set the stage for a true bay effect snow event that likely produced localized snow totals of 0.5” on top of what already fell. Radar imagery showed 25dBz echoes in the middle of that (very narrow) bay effect snowband for a short period of time, which likely corresponded to 1”/hour snowfall rates. The bay effect band drifted west and weakened by 5-6 AM as the fetch over the bay was disrupted with the low-level flow shifting from 360° to 010-020°. We hypothesized that if the flow had remained due north, the band could have produced an additional 2-3” of snow over a 5-10 mile wide area.

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