Tuesday, January 17, 2017

UWFPS 2017 daily cold-air pool forecast valid Tuesday 01/17/2017 0820 MST (8:20 am local time)

Key summary : Temperature inversion  associated with the persistent cold-air pool has increased in strength and descended overnight. Low clouds cover is less than in previous days, thus no visibility problems are anticipated Tuesday for research flights. Mix-out of this episode at this time expected on Thursday morning with rain and light snow.

Current weather synopsis and short-term forecast (12-36 h forecast from Tues am 17 January-Wednesday am 18th January):

The cold-air pool conditions expected to continue as a positively-tilted ridge of high pressure crosses the over the region through this period. The inversion strength has increased notably over the past 25 hours, and the elevation of the capping inversion has descended around 20 hPa and will continue to descend over next 36 hours. 
 
Satellite fog product at 1400 UTC 17 January. Note that extensive low clouds (yellow) are reduced compared to previous mornings.

 
Salt Lake International Airport Rawinsonde at 1200 UTC 17 January. Note the increase in temperature inversion strength and decrease in the height of inversion compared to 15-16 January.
Visibility/ceiling/clouds: Patchy areas of low clouds with reduced coverage compared to previous days. At this time evening fog formation is not expected in the Salt Lake Valley, but cannot be completely ruled out. Evening fog formation in Cache potential (40%) will need to be monitored.
Winds: light and variable.

PM2.5 Pollution levels have remained steady in the 20 micrograms/m3 overnight in the Salt Lake Valley Much higher PM2.5 continues in Cache Valley (over 45 micrograms/m3).
Pesky low clouds continue across the Salt Lake Basin (yellow color in the image below):

The temperature inversion remains in place across the region, as seen by the 5 am Jan 17th Salt Lake Airport sounding.  Comparing this morning’s sounding to yesterday morning we can see that the mixed-layer is much shallower, allowing the pollution levels to climb overnight into this morning.


Mid-term forecast (Wed-Fri 18-20 January):
 
Moderate cold-air pool conditions continue until end of episode Thursday morning. However, on Wednesday afternoon, a thick mid-level cloud deck is expected, which will start to weaken the inversion (see forecast sounding below):
Wednesday 5 PM local sounding. Note the cloud layer between 500-600 mb and the increasing winds both at mountaintop level and the channelled southerly flow at lower elevations.

 By Wednesday night, the clouds will be thick and light precipitation will be approaching from the west. Thus, we do not expect much nighttime cooling on Wednesday night. On Thursday morning, rain or a rain and snow mix will start by mid-day and continue through the day, potentially changing over to snow Thursday night. A significant snow storm is currently possible for Friday night into Saturday in northern Utah.
1800 UTC sounding nearing "mix-out" time with deep saturated layer and rain/snow mix of precipitation.

Visibility/ceiling/clouds:Mid-level clouds will be on the increase. Fog is not expected to be an issue during this period, but is difficult to forecast and cannot be ruled out.
Winds: Mountaintop winds will be increasing rapidly to35 kts at mountaintop level by 5 am MST Thursday. At the same time, a southerly channeled jet between 300 and 1000 m AGL with speeds of 10-15 kts will develop in the Salt Lake Valley Wednesday evening and continue into Thursday.

Long-term forecast (Sat-Tues Jan 21-24):

While forecast models could change, at this time several storm systems are expected during this time, with several chances of accumulating snow in the Utah and Salt Lake Valley and no persistent inversion or cold-air pool conditions through the period.  Long-range GFS model hints at a ridge of high pressure forming over the Western US around January 25th, but the European Model has the storm track continuing. Check back, as confidence is low on this pattern change this far out in the forecast cycle.

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