Airalways moves from high pressure to low pressure
Trade winds
Air flowing from high pressure to low pressure, deflected by Coriolis effect
Ocean currents
Move heat from equator to poles, preventing overheating of the planet
Rainfall zones
Rain falls in areas of low pressure where air is rising, no rain in high pressure areas where air is sinking
Hot deserts
Form in high pressure zones at the tropics
Cold deserts
Form in high pressure zones at the poles
Volcanic eruptions release sulfur dioxide and ash, causing global cooling in the short-term
Asteroid collisions throw up dust, blocking solar radiation, causing global cooling in the short-term
Sunspot activity
Periods of more/less sunspot activity cause long-term heating/cooling of the planet
Orbital theory
Changes in Earth'sorbit and axis tilt cause long-term heating and cooling of the planet
Circular orbit
Orbit around the sun where the distance to the sun is equal at any point
Elliptical orbit
Orbit around the sun where the distance to the sun varies, sometimes further away (cooler) and sometimes closer (hotter)
Axis tilt
The planet's axis is not straight, it is on an angle and this wobbles over a 41,000 year period, causing the planet to be closer or further from the sun
Ice cores contain trapped carbon dioxide, which indicates past climate conditions
High levels of carbon dioxide in ice cores indicate it was warmer in the past, low levels indicate it was colder
Tree rings
The gaps between tree rings indicate past growing seasons, with wider gaps showing warmer periods and narrower gaps showing cooler periods
Historical sources like old photographs, drawings, and written accounts are less reliable for determining past climate as they may involve artistic license or exaggeration
Satellite images are very reliable for determining current climate conditions
Greenhouse effect
Greenhouse gases in the atmosphere trap outgoing long-wave radiation, causing the planet to heat up
Some greenhouse gases are naturally occurring, but human activities are enhancing the greenhouse effect and causing global warming
Thermal expansion
As the oceans heat up, the water molecules expand, causing sea levels to rise
Climate change will bring more frequent and severe weather events like flooding, hurricanes, and changes to farming
Tropical cyclones/hurricanes/typhoons
Powerful storms that form within the tropics, measured on the Saffir-Simpson scale from 1-5 based on wind speed
Tropical cyclones
Require warm sea surface temperatures of around 26.5°C
Form either north or south of the equator due to the Coriolis effect
Bring hazards like strong winds, storm surges, coastal flooding, intense rainfall, and landslides
Formation of hurricanes
1. Warm water required
2. Coriolis effect
3. Storms form over West Africa
4. Storms merge due to Coriolis effect
5. Low wind shear in upper atmosphere required
6. Sea surface temperatures of 27 degrees required
7. Occurs over oceans
8. Dissipates when hits land
Hurricanes
Swirling winds and clouds due to Coriolis effect
Very low pressure, often below 1000 millibars
Lower the pressure
Stronger the winds
Hurricanes have greater impacts in low-income countries
Bangladesh
Very low-lying, only 2 metres above sea level
Located on a river delta
Coastal location
Impacts are less in high-income countries, but can still be severe
Impacts in USA
Hurricane Katrina in 2005 - Levees broke, flooding large areas, high death toll, criticism of government response
Warning systems use foreign satellites, more effective in urban areas, issues with rural literacy and electricity access, shelters built but some reluctance to evacuate
Forecasting and warning
Satellite tracking to predict hurricane path, warnings via TV, radio, mobile phones - more effective in high-income countries
Earth's layers
Crust
Lithosphere
Asthenosphere
Upper mantle
Lower mantle
Inner core
Outer core
Continental crust
Thick, buoyant, light, made of granite, what we stand on