lecture 18: hurricanes and tornadoes Flashcards
tropical cyclones
most destructive of weather disasters, affecting huge areas (thousands of km2) with 3 types of hazard:
- high winds (up to 240km)
- storm surges (raising sea level up to 6m)
- heavy rains and subsequent flooding (landsliding)
typhoon mangkut
2018- southern coast of china
120km/h winds
hurricane michael
oct 2018, florida
hurricane formation
tropical cyclones are storms with 1 minute sustained winds >120km/h, form between 5-20 degrees N/S
subdivision of tropical cyclones geographically
hurricanes: south atlantic and mexico
typhoons: southeast asia
cyclones: southwest indian and australia
why arent tropical cyclones formed
S atlantic: high winds
SE Pacific: insufficient water temperature
red sea/persian gulf: insufficient surface area
equator: insufficient coriolis effect
hurricane formation
start by summer heating of tropical oceans with a) warm shallow water >27-50 degrees to enhance evaporation b) unstable air for thunderclouds to form c) weak vertical wind shear to stop storm from breaking up
4 stages of hurricane formation
- tropical disturbance low pressure draws in surrounding thunderstorms with weak winds
- storms coalesce into tropical depression and winds strenghten (37-63km)
- tropical storm has stronger winds that start to form cyclonic pattern, can now be named
- tropical cyclone has winds >120km/h that cannot reach the core due to rotation, forms eye of storm
path of hurricane
follows a curve due to coriolis effect (earths rotation)
- deflected to the right in northern hemisphere and left in southern hemisphere
hurricane decline
winds decline when warm water energy source is cut off as they go over land or reach colder waters
- can interact with other weather systems in mid-latitude and gain strength again
typhoon freda
Oct 1962, killed 46 people in US and 7 in canada
- came up west coast mass of water vapour blew up
- took 2 weeks to travel 8000km across the pacific
3 steps of hurricane
- air moves towards low pressure eye over warm sea, evaporating water
- humid air spirals up the eyewall. Rising water vapor cools and condenses, forming clouds which releases latent heat of condensation intensifying the updrawft
- cold air is sucked down the eye
rotation of hurricanes in hemispheres
anticlockwise in northern
clockwise in southern
eye and eyewall
eye: circular region of calm clear weather at hurricane centre
eyewall: surrounding cyclinder of upward spiralling winds that are the strongest in the entire hurricane
hurricane energy
storm motion speed along its track is added or subtracted from storm wind speed to give the actual wind speed experienced on the ground
storm motion is 30km/h: storm winds 160km/h safe semicircle is 130, unsafe is 190km/h, might be 200km/h in eye