Hurricanes Flashcards
Jetstream
- 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
Small-scale wind patterns
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
Fronts
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
Low vs high pressure systems
Tropical storms
- hurricane
- round, no fronts
- warm water, latent heat
- formed in single air mass with a warm core
Extratropical storms
- nor’easter
- comma shape, cold or warm front
- pressure differences “baroclinicity”
- formedw hen two air masses meet, has a cold core
What are hurricanes?
- 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)
How do hurricanes form?
- 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
Hurricanes as heat engines
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
Hurricane ingredients
- warm sea surface temperature (> 26.5, > 80F) over large area, warm water supplies heat and humidity to overlying air
- Instability in atmosphre (rising air mass), fueled by surface warming, whcih decreases air density
- Little/no vertical wind shear through troposphere
- Sufficient lattitude >5-10 degrees off equator such that coriolis kicks in
What can slow a hurricane?
- Intense cyclonic winds generates upwelling in ocean
- If upwelling is strong enough, the colder water rises to the surface, starving the hurricane of energy
Death of a hurricane
energy lost due to friction = dnesity of air * drag coefficient * wind speed^3
Hurricane damage
- high winds
- intense rainfall
- storm surge
Storm surge
- 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