Convective Storms Flashcards
Impacts of deep moist convection
Heavy rain, hail, winds, tornadoes, lightning
What is convection?
Rising warm air that releases an unstable thermodynamic profile
Three ingredients for deep, moist convection
Moisture, conditional instability and lift
What is conditional instability?
Γm < Γ < Γd
Absolute stability
Γ < Γm
Absolutely unstable
Γ > Γd
Condensation produces
Latent heat
Equilibrium layer is when
Γ becomes less than Γd (no longer buoyant)
Level of free convection is when
Γ becomes bigger than Γd (buoyant)
LCL is when
Parcel begins following moist adiabat
Convective inhibition suppresses the growth of
Small cells
CAPE is related to the stength of the
Updraft
Why is CAPE usually an overestimation of updraft strength?
Water loading & the entrainment of dry air
Maximum vertical motion equation
wmax = (2 x CAPE)^0.5
Latent heat releases provides the updraft
Bouyancy
Deep moist convection requires moisture at the
Mid-upper levels
Ordinary cells have
One updraft and one downdraft
Towering cumulus stage
Air has passed LFC and begins rising
Mature cumulonimbus stage
Precipitation, dry air entrainment, evaporatively cooled air descends
Dissipating stage
Bubble reaches EL and isn’t bouyant, cell dissipates
Timescale for an ordinary cell
30 minutes
Ordinary cells only produce heavy rain if tied to
Orography
Ordinary cells have ___ vertical wind shear
Weak
Vertical wind shear is important for ___ deep, moist convection
Organised
Multicell convective storm
Organised cells at different life stages
How one cell initiates another
Convergence along the gust front lifts air to the LFC
Downdrafts of cold, moist air produced by evaporating rainfall
Cold pools (gravity currents, gust fronts)
Vertical wind shear separates the
Updrafts and downdrafts
Quasi-linear mesoscale convective systems
Squall lines
Squall lines are sometimes forced by
A front
Supercells have a
Steady, rotating updraft
Supercell low level wind shear causes a
Cyclonic rotation
Supercell clouds
Anvil, overshooting top, mammatus, cumulonimbus