Convective Storms Flashcards

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

A

30 minutes

22
Q

Ordinary cells only produce heavy rain if tied to

A

Orography

23
Q

Ordinary cells have ___ vertical wind shear

A

Weak

24
Q

Vertical wind shear is important for ___ deep, moist convection

A

Organised

25
Q

Multicell convective storm

A

Organised cells at different life stages

26
Q

How one cell initiates another

A

Convergence along the gust front lifts air to the LFC

27
Q

Downdrafts of cold, moist air produced by evaporating rainfall

A

Cold pools (gravity currents, gust fronts)

28
Q

Vertical wind shear separates the

A

Updrafts and downdrafts

29
Q

Quasi-linear mesoscale convective systems

A

Squall lines

30
Q

Squall lines are sometimes forced by

A

A front

31
Q

Supercells have a

A

Steady, rotating updraft

32
Q

Supercell low level wind shear causes a

A

Cyclonic rotation

33
Q

Supercell clouds

A

Anvil, overshooting top, mammatus, cumulonimbus