Mesoscale Circulations during VTMX John Horel Lacey Holland, Mike Splitt, Alex Reinecke...
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Transcript of Mesoscale Circulations during VTMX John Horel Lacey Holland, Mike Splitt, Alex Reinecke...
![Page 1: Mesoscale Circulations during VTMX John Horel Lacey Holland, Mike Splitt, Alex Reinecke jhorel@met.utah.edu.](https://reader030.fdocuments.us/reader030/viewer/2022032800/56649d485503460f94a22dbf/html5/thumbnails/1.jpg)
Mesoscale Circulations during VTMX
John Horel
Lacey Holland, Mike Splitt,
Alex Reinecke
![Page 2: Mesoscale Circulations during VTMX John Horel Lacey Holland, Mike Splitt, Alex Reinecke jhorel@met.utah.edu.](https://reader030.fdocuments.us/reader030/viewer/2022032800/56649d485503460f94a22dbf/html5/thumbnails/2.jpg)
Overview
• Temporal and spatial context for VTMX IOPs
• Synoptic and mesoscale conditions during IOPs
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October 1999500 mb geopotential height
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October 1999500 mb geopotential height anomaly
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October 2000500 mb geopotential height
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October 2000500 mb geopotential height anomaly
Cooler and wetter thannormal
PM-10 concentrationshalf those inOctober 1999
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MesoWest
• Data available from January 1997 to present
• www.met.utah.edu/mesowest
• Paper describing MesoWest submitted to BAMS
9 Oct. 0900 UTC
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Diurnal Temperature Range: Fall
Alex Reinecke
MesoWestObservations
1997-2000
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Diurnal Temperature Range- FallLatitude vs. Elevation
SLC
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Diurnal Temperature Range: October 2000
RushValley
TooeleValley
Salt LakeValley
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October 2000: Salt Lake Valley
SLC
U42
Great Salt Lake: 21C- 10C
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Surface Wind Convergence in Salt Lake Valley
IOP
1
IOP
2IO
P 3
IOP
4
IOP
5IO
P 6
IOP
7
IOP
8IO
P 9
IOP
10
Mike Splitt- Linear regression fit
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Stability and Wind
• Surface-based inversions (greater than 5C in the lowest 100 mb) observed during 15 of the 31 morning (1200 UTC) soundings at the Salt Lake City International Airport
• Weak surface inversions with stable layers aloft below the crest of the Wasatch Mountains on 5 other mornings
• Well-mixed conditions present during the other 11 mornings
• Winds at 700 mb (near the crest of the Wasatch Mountains) were less than 10 m/s in 19 of the 31 morning soundings.
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IOPs with Well-Developed Drainage Circulations
• 5 (14-15 October)• 6 (15-16 October)• 8 (19-20 October) • Clear skies, weak winds aloft at crest level, strong
nocturnal radiational inversions• Limited moisture in the boundary layer• Pronounced drainage flow into the Salt Lake Valley from
the west, south, and east• Surface based inversions and drainage circulations
developed after sunset and persisted without significant interruption until sunrise
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IOP-8: 9 UTC 20 October
SLC
500 mb
700 mb
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IOPs Modulated by Synoptic and Mesoscale Systems
• IOP 1 ( 2-3 October) • Test operational procedures • During evening:
– clear skies with drainage flows developing as the evening progressed• Synoptic-scale northerly pressure gradient developed overnight
– Northerly winds penetrated into northern end of the Salt Lake Valley before midnight
– Eventually reversed the down-valley (southerly) flow through the center of the valley
– Drainage circulations down into the valley from the Oquirrh and Wasatch Mountains were largely unaffected
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IOPs modulated by synoptic and mesoscale weather systems
• IOP 4 (8-9 October), IOP 7 (17-18 October) • Similar boundary-layer structure to that in IOPs 5,
6, 8 until early morning• Prior to that time, clear skies, weak winds aloft,
and strong surface-based radiational inversions • As a result of approaching upper-level troughs
from the west, the nocturnal inversions eroded both by surface heating and by mixing due to the downward penetration of southerly winds
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IOP-4 9 October
SLC
500 mb
700 mb
Wheeler
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IOPs Modulated by Synoptic and Mesoscale Systems
• IOP 2 (6-7 October) and 3 (7-8 October)• Split flow aloft with weak upper-level short waves to the southwest and
northeast of Utah• Strong outbreak of cold air to the east of the continental divide
progressed westward after 0 UTC• After 1000 UTC, the depth of the cold air to the east of the Wasatch
Mountains built to sufficient height to spill over the lower terrain from Mill Creek Canyon to near the University of Utah in the northeast corner of the Salt Lake Valley
• IOP-3 began at 2200 UTC 7 October and was terminated before midnight
• Strong downslope conditions persisted into the evening in the northeastern corner of the Salt Lake Valley
• Winds in the western part of the valley were turbulent
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IOPs Modulated by Synoptic and Mesoscale Systems
• IOP 9 (20-21 October ) and IOP 10 (25-26 October) • Affected significantly by approaching upper-level
troughs. • weak short-wave ridge aloft initially• Skies were broken to overcast • Weak nocturnal surface inversion and drainage
circulations • Cold-front at 1200 UTC 21 October • Southerly surface winds were enhanced during IOP
10
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IOP 9- 3UTC 21 October
500 mb
700 mb
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Summary
• Mountain/valley circulations and radiational inversions occurred on over half of the days
• Local circulations dominated several IOPs (5, 6, 8)- but each had unique characteristics
• Synoptic and mesoscale influenced IOPs:– IOP 1: interruption of drainage circulations in the north
end of the Salt Lake Valley– IOPs 2, 3: downslope wind event– IOPs 4, 7: erosion of invesion from aloft– IOPs 9, 10: approaching weather systems
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IOP-1 300 UTC 3 October
6UTC
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IOP 2: 1200 UTC 7 October
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IOP 3- 300 UTC 8 October
0Z
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IOP-4 9 October
SLC
500 mb
700 mb
Wheeler
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IOP 5 600 UTC 15 October
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IOP 6 12 UTC 16 October
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IOP 7 600 UTC 18 October
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IOP-8: 9 UTC 20 October
SLC
500 mb
700 mb
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IOP 9- 3UTC 21 October
500 mb
700 mb
0Z
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IOP-10 600 UTC 26 October