Atmospheric Hazards Flashcards
formation of a tropical storm
- air is heated at the surface of warm tropical oceans (27degrees)
- warm air rises under low pressure
3.as it rises it draws up moisture, forming strong winds - winds spin around a calm central eye due to the coriolis
effect - as air rises it cools and condenses- forms torrential rainfall and cumulonimbus clouds
- as the air cools, it gives off heat, which powers the storm
describe how weather changes at different points of a storm
A. temperature falls, air pressure falls
B. temperature falls, air pressure falls, torrential rain, cumulonimbus clouds, strong winds
C. calm, dry storm eye, temperature rises
D. temperature falls, air pressure falls, heavy rain, strong winds
E. temperature starts to rise, rain, air pressure rises
describe the global distribution of tropical storms
over warm oceans (27 degrees)
not along the equator (5-30 degrees north/ south of equator)
areas of low wind shear
low wind shear
if wind shear is high, then winds are strong enough to blow the storm away from the side
not along equator
coriolis effect is not strong at the equator, the storm requires the coriolis effect to spin
warm oceans
27 degrees
air is warmed and evaporates forming water vapour- which acts as energy for the storm
low pressure
describe the effect climate change will have on frequency of tropical storms
as temperatures increase and oceans become warmer and expand, more oceans will reach 27 degrees- there will be more severe storms
describe the effect climate change will have on intensity of tropical storms
cat 1-3 will decrease
cat 4-5 will increase
will be more severe storms as oceans become warmer
what tropical storms happen in the:
-atlantic ocean
-pacific ocean
-indian sea
atlantic ocean- hurricanes
pacific ocean- typhoons
indian sea- cyclones
why are links between tropical storms and climate change uncertain
climate models have wide-ranging impacts
not enough data to make concrete predictions
where is the coriolis effect the strongest
at the poles
give the name of our two case studies
Typhoon Haiyan, 2013
Beast from the East, 2018
describe typhoon Haiyan (location, date, intensity, storm path)
Philippines, November 2013
4:40 am
windspeeds of 314km/hour
winds spinning counter-clockwise
explain why typhoon Haiyan was so severe
made landfall at 4:40am- 6 hours earlier than predicted so people were unprepared
philippines made up of 300 islands- constant water and energy source
5m storm surge- never happened before, was unexpected
primary effects of Typhoon Haiyan (social, economic, environmental)
social:
6300 deaths
4.1 million homeless
economic:
$12 billion damage costs
$53 million damage to rice
environmental:
water contamination- harmed aquatic life
800,000 litre oil leak
1.1million tonnes of destroyed crops
secondary effects of Typhoon Haiyan (social, economic, environmental)
social:
schools closed
people in shelters
economic:
flooded roads- people could not get to work
less tourism
environmental:
wildlife habitats destroyed
immediate responses to Typhoon Haiyan
treat casualties
bury dead (prevent water contamination)
build temporary shelters
access remote islands
long term responses to Typhoon Haiyan
expand shelters
rebuild homes/ roads
build back better
plant mangroves
Typhoon Haiyan protection strategies
plant mangroves- absorb storm surge energy
build back better- raise homes on stilts
Typhoon Haiyan planning strategies
900 trained fishermen- how to make boats stronger
trained families how to cook food without electricity