Lecture 17 Flashcards
What is a hurricane?
Tropical cyclone with sustained winds >119km/h
Convert hot water and heat of tropical ocean to winds
Creates waves, surges and flooding
Energy generation (from latent heat of condensation to form clouds and rain, 2500 joules/g water) is 200 times greater than worldwide capacity to generate electricity
The energy released during condensation is 400 times more than the energy of its winds
Source regions of hurricanes
Cape Verde
Caribbean Sea
Gulf of Mexico
Tropical cyclone
Generic term for a non-frontal synoptic scale low-pressure system over tropical or sub-tropical waters with organized convection (i.e. thunder-storm activity) and definite cyclonic surface wind circulation
What conditions must exist (6)
1) Upper 60m ocean should be at least 27*C
2) Moist convection (a thunderstorm) in an atmosphere that cools quickly with height
3) Moist mid layer in the troposphere (5 km)
4) 500 km from the equator to feel enough Coriolis force to balance pressure gradient winds
5) Upper-level winds should be weak, blowing in direction storm is moving
6) Low vertical shear (winds traveling from sea level to tropopause)
Evolution of a hurricane (6)
1) Tropical disturbance: low pressure zone draws in clusters of thunderstorms, but not fully organized
2) Tropical depression: surface winds strengthen, flow more efficiency around and into centre of storm
3) Cyclonic rotation: counterclockwise
4) Convergence of surface winds: chimney effect, warm moist air to stratosphere, wind spiral up core walls
5) Condensation of vapour: latent heat is emitted during condensation, increases the updraft, increases inward flow of surface winds
6) Tropical storm: sustained winds > 62km/h
Eye
Region of mostly calm weather at the center of strong tropical cyclones. The eye of a storm is a roughly circular area, typically 30–65 km (20–40 miles) in diameter. It is surrounded by the eyewall, a ring of towering thunderstorms where the most severe weather and highest winds occur
Atlantic
Hurricane
North Pacific
Typhoon
South Pacific
Tropical cyclone
Indian ocean
Cyclonic storm
Cape Verde
African Eastern waves Driven by temperature contrasts between the Sahara and adjacent cooler regions Period of 3-4 days, 2000-2500km 60% of all tropical storms 85% of all major hurricanes Almost all pacific cyclones
Latent heat
Heat absorbed or released during phase change
When water vapour cools to form droplets, release latent heat which helps propel more rising of air
Advection
Movement of air of different masses
Wind speed >0
Pressure gradient force
Difference in adjacent barometric pressures, operates perpendicular to isobars and an begin to accelerate winds from zero wind speed
Centrifugal force
(tangential wind velocity)^2/(radius of curvature)
Force that opposes centripetal force
Centripetal force causes an object to bend its trajectory
Centrifugal pulls outward from the centre of a turn
Wind speed >0