Hurricanes Flashcards

1
Q

Jetstream

A
  • Narrow, fast air flow in the upper atmosphere, from west to east
  • At mid latitudes, ~10 km high
  • Can cause unusual weather by steering air masses
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2
Q

Small-scale wind patterns

A

Sea breeze (daytime)
- land warms faster than the ocean
- air rises over the land, sucking in air

Offshore breeze (night)
- land cools faster than the ocean
- air moves back out to sea

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3
Q

Fronts

A

Boundaries between two different air masses, where the colder air always moves underneath the warm air
- warm front - warm air mass moves to colder area
- cold front - cold air mass moves to warmer area

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4
Q

Low vs high pressure systems

A
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5
Q

Tropical storms

A
  • hurricane
  • round, no fronts
  • warm water, latent heat
  • formed in single air mass with a warm core
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6
Q

Extratropical storms

A
  • nor’easter
  • comma shape, cold or warm front
  • pressure differences “baroclinicity”
  • formedw hen two air masses meet, has a cold core
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7
Q

What are hurricanes?

A
  • Large, swirling storms with strong winds and significant rainfall
  • great masses of warm, humid, rotating air, bringing strong winds and torrential rain
  • occur only in tropical oceans
  • sustained winds > 120 km/hr (75 mph)
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8
Q

How do hurricanes form?

A
  • warm ocean, provides heat to evaporate water
  • high to low pressure, picking up moisture from ocean, absorbing latent heat
  • air rises, cools, condendes, releases latent heat
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9
Q

Hurricanes as heat engines

A

Heat energy from the ocean driving mechanical work
- air moves higher to lower pressure
- heat goes from ocean to air via latent heat of evaporation
- air is approx isothermal, nbut wetter and greater volume

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10
Q

Hurricane ingredients

A
  1. warm sea surface temperature (> 26.5, > 80F) over large area, warm water supplies heat and humidity to overlying air
  2. Instability in atmosphre (rising air mass), fueled by surface warming, whcih decreases air density
  3. Little/no vertical wind shear through troposphere
  4. Sufficient lattitude >5-10 degrees off equator such that coriolis kicks in
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11
Q

What can slow a hurricane?

A
  • Intense cyclonic winds generates upwelling in ocean
  • If upwelling is strong enough, the colder water rises to the surface, starving the hurricane of energy
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12
Q

Death of a hurricane

A

energy lost due to friction = dnesity of air * drag coefficient * wind speed^3

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13
Q

Hurricane damage

A
  • high winds
  • intense rainfall
  • storm surge
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14
Q

Storm surge

A
  • Usually the largest on the side of the hurrican where the winds push ocean water onto shore
  • flooding is worse when storm surge combines with high tide
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