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A brief synopsis of Johnson and Mapes: Mesoscale Processes and Severe Convective Weather. From Severe Convective Storms sections 3.3b, 3.3c.1, 3.4 By Matt Gough. overview. Advective Processes and examples that lead to severe weather Dynamical Processes and examples - PowerPoint PPT Presentation
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A brief synopsis of Johnson and Mapes: Mesoscale Processes
and Severe Convective Weather
From Severe Convective Storms sections 3.3b, 3.3c.1, 3.4
ByMatt Gough
overview
• Advective Processes and examples that lead to severe weather
• Dynamical Processes and examples
• Convective triggering mechanisms
Advective Processes
Moisture Advection• Increases CAPE and lowers LFC
Synoptic scale Differential Advection• Destabilizes atmosphere• Provides vertical wind shear• establishes capping inversions
Convergence Lines• Preconditioning and triggering convection
Examples of mesoscale Differential Advection
• Low-level jets with high θ(e) overrunning fronts and cold-pools (bow echoes).
• Flow of moist boundary layer air out from beneath an inversion
• Transport of clouds and moisture aloft downstream of mountain barriers (dry microbursts)
• Short periods of jet streak circulations and boundary layer heating
Examples of Convergence Lines• Warm and cold fronts – associated with
Mesoscale cross-front circulations.• Precipitation driven downdrafts (gust fronts)• Drylines – usually needs to be coupled with
other mechanisms.• Land and Sea breezes – convergence of
offshore or onshore flow.• Mountain/Valley breezes – upslope flow in
western US providing convergence and lifting.
Off the east coast of Florida in the morning.
Dynamical processes
• Upper level jets
• Lower level jets
• Coupling of upper and lower level jets
Dynamical processesUpper level jets
Dynamical processesLower level Jets• Enhancement of moisture and temperature
advection.• Increased low level convergence• Increase in vertical wind shear
Coupling of upper and lower level jets• Upper level conv. forces low level jet Coupling between indirect circulation and
cold cold front.
Triggering of convection
Mechanisms can operate in isolation
• Storms along a gust front
or in combination
• Gust fronts colliding with each other
Triggering of convection
Local Processes
Buoyancy driven circulation
• Thermals, horizontal convective rolls, overshooting buoyant eddies.
Terrain Forcing
• Lee-side convergence, thermally-induced lifting, flow deflection, and surface inhomogeneities.
Lee side convergence
Triggering of convection
Advective Processes
• Convection along convergence
• Cold/warm front lifting
• Gust fronts, sea breezes, and drylines
Usually the intersection of these features cause severe convection.
Cold front lifting
Triggering of convection
Dynamical Processes:
• Horizontal Convective Rolls (operate in conjunction with other processes)
• Gravity waves (in tropics – small CIN)
• Horizontal shear
Triggering of convection
Combined Lifting Processes:• Boundary layer rolls intersecting with
convergence lines • HCRs intersecting with sea breezes.• Dryline convection: mesoscale lows, HCRs,
fronts, and gravity waves.• Gust fronts with terrain, gravity waves, etc.
Denver, CO, 17 Jul 1987