Air always flows from high pressure to low pressure
Ocean currents
Move heat from equator to poles
Ocean currents prevent overheating of the planet
Rainfall zones
Areas of low pressure have rainfall, areas of high pressure are deserts
West Africa has rainy and dry seasons due to movement in and out of the ITCZ
Natural causes of climate change
Volcanic eruptions
Asteroid collisions
Sunspot activity
Orbital changes
Volcanic eruptions and asteroid collisions
Cause short-term global cooling by blocking solar radiation
Sunspot activity
Causes longer-term heating and cooling cycles
Orbital changes
Cause longer-term heating and cooling cycles due to changes in Earth's distance from Sun and tilt of axis
Circular orbit
Equal distance to the sun at any point
Elliptical orbit
Not round, sometimes further away from the sun (cooler), sometimes closer to the sun (hotter)
Axis tilt
Planet is on an angle, this wobbles, putting us closer or further from the sun over a 41,000 year period
The axis tilt has an impact on heating and cooling over a long period
Ice cores
Contain trapped carbon dioxide, high levels indicate past warmer periods, low levels indicate past cooler periods
Tree rings
Wider rings indicate longer growing seasons and warmer periods, narrower rings indicate shorter growing seasons and cooler periods
Historical sources
Less reliable, may involve artistic license or exaggeration (e.g. accounts of frost fairs on the Thames)
Satellite images
Very reliable, use of technology
Greenhouse effect
Greenhouse gases in the atmosphere trap outgoing long-wave radiation, causing the planet to heat up
Some greenhouse gases are naturally occurring (e.g. from volcanoes, forest fires, rotting vegetation)
Enhanced greenhouse effect
Increased greenhouse gases from human activities (burning fossil fuels, more livestock) leading to greater heat trapping and global warming
Thermal expansion
Warming oceans cause water molecules to expand, leading to rising sea levels
Future climate change scenarios
Option C (best case - low population growth, renewable energy, 30cm sea level rise)
Option B (moderate population growth, some renewable energy, 1.5°C warming)
Option A (worst case - high population growth, fossil fuel use, over 1m sea level rise)
Climate change will bring more frequent and severe weather events (flooding, hurricanes, storms), disruption to farming, and climate refugees
Tropical cyclones/hurricanes/typhoons
Form over warm tropical ocean waters, measured on Saffir-Simpson scale, bring strong winds, storm surges, heavy rainfall, and landslides (especially in poorer regions)
Formation of hurricanes
Require warm ocean water, coriolis effect, form over West Africa and move across Atlantic
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. 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 compared to high-income countries
Bangladesh
Very low-lying, only 2 metres above sea level
Located on a river delta
Coastal location
Storm surges and heavy rainfall
Cause flooding in Bangladesh
Impacts in Bangladesh
Cyclone Aila in 2009 - 190 people died, 750,000 made homeless, crops ruined by saltwater
Impacts in high-income countries like the USA are generally less severe, but there can be exceptions