In an
incredible coincidence, we start forecasting for a once-in-a-lifetime snowstorm
for New Orleans. The high will occur at the beginning before the start, as cloud
cover and wind prevent radiational cooling. Often, these will lead to more
vertical mixing and warmer surface temperatures than modeled, especially at
night when models often erroneously show some nocturnal inversion.
It will already be
cold (by New Orleans standards) then, but the snow will cause evaporative and
subliminational cooling in the dry low-level air, and temperatures will quickly
drop below freezing. Snow will be heavy at times with stiff northerly winds.
The northerly winds off Lake Pontchartrain (water temperature of ~52F) will
lead to slight moderation of the cold, but it won’t be more than a couple of
degrees given the heavy snow and widespread, deep cold air. The wind off the
lake could also lead to lake-enhanced snow, something that almost never happens
there. The onshore wind also will lead to vertical mixing of stronger winds
aloft down to the surface due to the increased instability induced by the relatively
warm lake water, but counteracted by heavy snow’s tendency to suppress winds a
little. Such enhancement is often not handled by models well, though the low-level
lapse rates might not be quite steep enough for much lake enhancement.
Snow will stop
tomorrow evening, and then skies will clear out, leading to a cooldown to the
low possibly at the end (Wednesday 06z), though the winds off the lake will
remain too strong for good radiational cooling. It might be around the same
temperature as during the heaviest snow tomorrow morning (likely upper 20s F)
when dynamic cooling from strong ascent is the strongest.
| Source: PivotalWeather |
| Source: PivotalWeather |
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