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Page 1: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

Photo by Patrick Chando

Page 2: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

• What is atmospheric mixing?

• How mixing works

• Evolution through the day

• Case study

• Aviation weather hazards influenced by mixing

o Convective turbulence

o The dry line

o Wildfire smoke

o Haboobs

Learning Objective

Understand the evolution and timing of

atmospheric mixing, so you can better

anticipate the development, intensification

and dissipation of aviation weather

hazards.

Page 3: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

The transfer of momentum from stronger flow aloft to the surface by

thermals and other sources of wind shear (like cold fronts, outflow

boundaries and jet streams).

www.weather.gov/Jetstream/airmass Bubble Thermals

Essentials of Meteorology, C. Donald Ahrens

Page 4: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

https://www.weather.gov/jetstream/heat

Re-radiation

Re-radiation: The ground absorbs then re-radiates

energy at a wavelength air molecules can absorb.

(thermals)

(adapted)

Page 5: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM
Page 6: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM
Page 7: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM
Page 8: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM
Page 9: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM
Page 10: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM
Page 11: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

Adapted from Stull, R. B., 2000: Meteorology for Scientists and Engineers

Surface

Note the nearly calm surface winds

at the bottom of the inversion

and

the region of wind shear

at the top of the inversion

Page 12: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

Adapted from Stull, R. B., 2000: Meteorology for Scientists and Engineers

The descending couplet in

the thermal circulation transfers

stronger momentum aloft downward

causing surface winds to strengthen

Page 13: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

• Today we discuss: o Convective turbulence

o The dry line

o Wildfire smoke

o Haboobs

• On your own consider: o Nocturnal low clouds and fog

o Nocturnal low level jet on the

southern plains

o Some gap wind events, like ABQ’s

notorious east canyon wind

o Thunderstorms

o What else comes to mind?

Many weather hazards

depend on the diurnal cycle

of atmospheric mixing to

develop, intensify, and

diminish

TCC

RTN

LVS

AMA

TAD

11/6/17 (0827-1207Z)

Page 14: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

• Caused by thermals in a well

mixed atmosphere

• To Avoid: o Climb above the cumulus clouds

o Fly before the temperature

inversion breaks

Aviation Weather, FAA AC 00-6A, 1975

Essentials of Meteorology, C. Donald Ahrens

Bubble

Thermals

Chimney

Thermals

Todd Shoemake

Page 15: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

USATODAY.COM

• Dry/moist convergence zone o Daytime advances east

o Nighttime usually retreats west

• Flying hazards o Thunderstorms

o Low Level Wind Shear

• Most common and intense in

spring and early summer

www.tornadochaser.net/dryline.html

Page 16: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

6/24/02 1430Z

6/23/02 1430Z

NWS ABQ Website: www.weather.gov/abq

Mogollon Rim Wildfire

Page 17: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

• Wall of dust that can extend up to

6500 feet high and several

kilometers long o Near zero visibility for up to 45

minutes

o Erratic wind gusts may reach 50

mph or more

• Occur most often when monsoon

thunderstorm outflows merge over

AZ’s central and western deserts

• High risk locations: o Abandoned farmland

o Tilled farmland

o Land disturbed by animals

or ATVs

o Construction sites

o Areas in drought

NWS Phoenix

Page 18: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

• Wall of dust that can extend up to

6500 feet high and several

kilometers long o Near zero visibility for up to 45

minutes

o Erratic wind gusts may reach 50

mph or more

• Occur most often when monsoon

thunderstorm outflows merge over

AZ’s central and western deserts

• High risk locations: o Abandoned farmland

o Tilled farmland

o Land disturbed by animals

or ATVs

o Construction sites

o Areas in drought

Page 19: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

• Wall of dust that can extend up to

6500 feet high and several

kilometers long o Near zero visibility for up to 45

minutes

o Erratic wind gusts may reach 50

mph or more.

• Occur most often when monsoon

thunderstorm outflows merge over

AZ’s central and western deserts

• High risk locations: o Abandoned farmland

o Tilled farmland

o Land disturbed by animals

or ATVs

o Construction sites

o Areas in drought.

Page 20: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

Lubbock, TX, Oct 17, 2011

Emily Davenport

Erin Shaw

• More common with strong back door

cold fronts, especially in drought

• Best developed when buoyant mixing

intensifies mechanical mixing by front

Page 21: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

• What is atmospheric mixing?

• How mixing works

• Evolution through the day

• Case study

• Aviation weather hazards influenced by mixing

o Convective turbulence

o The dry line

o Wildfire smoke

o Haboobs Others to Consider

o Nocturnal low clouds and fog

o Nocturnal low level jet on the southern plains

o Some gap wind events

o Thunderstorms…

Page 22: Photo by Patrick Chando - National Weather Service · 2019-06-11 · Photo by Patrick Chando . Title: Slide 1 Author: Victor.Murphy Created Date: 6/11/2019 12:53:24 PM

(505) 243-0702 ext. 0

[email protected]

Photo by Patrick Chando