Convective Storms Flashcards

(33 cards)

1
Q

Impacts of deep moist convection

A

Heavy rain, hail, winds, tornadoes, lightning

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2
Q

What is convection?

A

Rising warm air that releases an unstable thermodynamic profile

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3
Q

Three ingredients for deep, moist convection

A

Moisture, conditional instability and lift

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4
Q

What is conditional instability?

A

Γm < Γ < Γd

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5
Q

Absolute stability

A

Γ < Γm

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6
Q

Absolutely unstable

A

Γ > Γd

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7
Q

Condensation produces

A

Latent heat

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8
Q

Equilibrium layer is when

A

Γ becomes less than Γd (no longer buoyant)

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9
Q

Level of free convection is when

A

Γ becomes bigger than Γd (buoyant)

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10
Q

LCL is when

A

Parcel begins following moist adiabat

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11
Q

Convective inhibition suppresses the growth of

A

Small cells

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12
Q

CAPE is related to the stength of the

A

Updraft

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13
Q

Why is CAPE usually an overestimation of updraft strength?

A

Water loading & the entrainment of dry air

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14
Q

Maximum vertical motion equation

A

wmax = (2 x CAPE)^0.5

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15
Q

Latent heat releases provides the updraft

A

Bouyancy

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16
Q

Deep moist convection requires moisture at the

A

Mid-upper levels

17
Q

Ordinary cells have

A

One updraft and one downdraft

18
Q

Towering cumulus stage

A

Air has passed LFC and begins rising

19
Q

Mature cumulonimbus stage

A

Precipitation, dry air entrainment, evaporatively cooled air descends

20
Q

Dissipating stage

A

Bubble reaches EL and isn’t bouyant, cell dissipates

21
Q

Timescale for an ordinary cell

22
Q

Ordinary cells only produce heavy rain if tied to

23
Q

Ordinary cells have ___ vertical wind shear

24
Q

Vertical wind shear is important for ___ deep, moist convection

25
Multicell convective storm
Organised cells at different life stages
26
How one cell initiates another
Convergence along the gust front lifts air to the LFC
27
Downdrafts of cold, moist air produced by evaporating rainfall
Cold pools (gravity currents, gust fronts)
28
Vertical wind shear separates the
Updrafts and downdrafts
29
Quasi-linear mesoscale convective systems
Squall lines
30
Squall lines are sometimes forced by
A front
31
Supercells have a
Steady, rotating updraft
32
Supercell low level wind shear causes a
Cyclonic rotation
33
Supercell clouds
Anvil, overshooting top, mammatus, cumulonimbus