weather gap filling

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Last updated 4:58 AM on 10/31/25
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4 Terms

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cyclone ingredients

start as disturbances over warm ocean (pre-existing tropical low)

DALR<ELR

warm ocean down to 50m

moist in mid-troposphere

  • moisture and heat deepen and intensify lows

minimal vertical wind shear

> 5 degrees from equato

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extratropical cyclone ingredients

a low pressure system that gets energy from horizontal temperature contrasts

  • cyclogenesis: cold and warm air masses interact in an unstable environment → causes convection

  • large temp. gradients at high latitudes, why antarctic latitudes have lots of cyclogenesis

  • especially when air gets cold over land and warms quickly over the ocean.

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thunderstorm/tornado ingredients

cumulus clouds gradually moistening with lots of convection, reaching lifting condensation level when parcel becomes saturated

LIFT

moisture for clouds

instability (SALR<ELR)

warm moist air at surface, cooler drier air aloft (mexico)

supercell thunderstorms have rotating violent updraft

organised has cells organising in larger group

multi-cell is several cells

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