The earth's surface is warmed by the Sun at the equator. The Earth transmits heat to nearby air. This air gets hotter and rises. The rising, hot air forms a low-pressure belt. As the hot air rises, the air will begin to cool, with water vapor condensing, creating rain and clouds.
The rising air cools and moves away from the equator towards 30 C north and 30C south.
Global Atmospheric Circulation (2):
At 30C North and South:
The air is further away from the equator and cold air forms, resulting in a high-pressure belt with minimal rainfall and no clouds
Global Atmospheric Circulation (3):
At 60C North and South:
Cold air blown from the poles meets warm air surface winds as the warmer air is less dense, it rises and forms a lower pressure belt
Global Atmospheric Circulation (4):
At the poles:
At the north and south poles, cold air sinks forming a high pressure belt
This high pressure belt will move back towards the equator, forming as a surface wind.
Extreme weather is a weather event that is significantly different from the average/ usual weather pattern
A drought is a period of time with abnormally dry weather leading to a shortage of water
El Nino:
Sinking air in the western Pacific causes high pressure, leading to unusually dry weather. This can cause droughts and much less rainfall.
Rising air in the eastern Pacific causes low pressure leading to unusually wet weather causing serious floods.
La Nina:
Sinking air in the eastern Pacific causes high pressure, leading to unusually dry weather. This can cause droughts and much less rainfall.
Rising air in the western Pacific causes low pressure leading to unusually wet weather causing serious floods.
CASE STUDY: Big Dry(Non-Uk based extreme weather hazard event):
Causes:
El Nino events led to especially low rainfall in South East Australia
Climate change
Increased temperature than usual in that period
CASE STUDY: Big Dry(Non-Uk based extreme weather hazard event):
Consequences:
Environmental:
Less electricity could be produced using water so more coal had to be burned to produce electricity, producing more CO2
The drought caused vegetation and soil erosion
CASE STUDY: Big Dry(Non-Uk based extreme weather hazard event):Consequences:
Economical:
Farmers had to sell their cattle as they couldn't afford to feed them and food prices increased
caused rural-urban migration which put greater pressure on cities and rural areas
Water bills rose by 20%
Social:
Hundreds of houses were destroyed
8 people were killed
suicide rates of farmers increased due to not being able to provide water to their livestock, which caused them to sell their farms
CASE STUDY: Big Dry(Non-Uk based extreme weather hazard event):
Responses:
The government gave $400 - $600 to farmers per fortnight to compensate farmers for the loss of their livelihood.
The government provided more than 23000 rural families and 1500 small businesses with income support for survival.
A flash flood is a sudden localised flood to heavy rain
CASE STUDY: Bostcastle floods(UK based extreme weather event):
Causes:
Natural:
75mm of rain received in just 2hrs - above average
Rain and risinghigh tide caused the river levels to increase by 2.15m in only 1hr
Geology in the area was impermeable, so there was lots of surface runoff
Human:
Pattern of the streets allowed water to runoff easily
Cars and trees in the flood were trapped under the bridge, which formed a dam, allowing water to go through another route, damaging the buildings and the village more.
CASE STUDY: Bostcastle floods(UK based extreme weather event):
Consequences:
Environmental
Trees destroyed due to flood carried downstream
4 bridges were washed away
Economic:
Had to spend £2billion to sort out the flooding
90% of the economy depended on toursim. 20 hotels were forced to shut
25 businesses were destroyed
Social:
58 properties were destroyed
Some residents suffered mental health problems
1000 tourists and residents were destroyed
CASE STUDY: Bostcastle floods(UK based extreme weather event):
Responses:
7 helicopters and emergency services were sent to rescue the people
Virgin trains had to cancel 20 trains
Destructive plate boundary(convergent):
When two plates are moving towards each other
When an oceanic plate meets a continental plate, the denser oceanic plate is forced down into the mantle and destroyed,forming volcanoes and ocean trenches.
Collision plate boundary(convergent):
Both plates are made from continental crust and move towards each other
Both plates are folded up and forced upwards, forming fold mountains
Constructive boundaries(Divergent):
When two plates are moving away from each other
Magma rises and fills gaps and cools, creating new crust
Conservative Boundary:
Where 2 plates are moving sideways past each other
Crust isn't created or destroyed
The thickness of the oceanic crust is 5 - 10 km thick
The thickness of the continental crust is 25-100km thick
Convection is the process of which the mantle is heated by the core and the heated magma rises towards the crust
An earthquake is a violent shaking in the earth's crust
Shockwaves are the transfer of energy that radiate out of the focus
The focus is the point where the ground snaps and moves
The epicentre is the point on land above the focus
The hotspot is the place in the middle of a tectonic plate where hot magma rises