Home » Teaching Resources » Past Climate Changes – Module 1 Past Climate Changes – Module 1 Facebook Twitter Pinterest Print Module 1 – the last 2.6 million yearsCore ResourcesClimate graph, 2.6 million years, without uncertainty Disambiguation: Ice Ages, Glacials and InterglacialsPowerPoint explanation of the Milankovitch CyclesCase StudiesToba – a supervolcano and its impact on humans ( a “mystery” resource)The last glacial maximumQuaternary Climate Change in BritainThe Mid-Pleistocene TransitionOther Useful ResourcesMilankovitch interactive animationsBritice modelling projectDiscovering AntarcticaManchester University’s Build your own Earth All Modules | Module 2- the Holocene > Start exploring Search Resources All Levels Primary Secondary Geography Secondary Maths Secondary Science Choose a topic All Topics Air Masses Anticyclones Carbon Cycle Climate Climate Change Climate Zones Clouds Contour Coriolis Depressions El Nino Extreme Weather Flooding Front Global Atmospheric Circulation Hydrological Cycle Microclimates Past Climate Snow Synoptic Charts Tropical Cyclones Urban Heat Island Water Cycle Weather Weather Forecast Weather Map Weather System All Climate Change 1.5 degree target Adaptation Afforestation Agriculture air quality aircraft Albedo Anthropocene anthropogenic Arctic/ Antarctic attribution Biodiversity Biosphere Carbon cycle Carbon dioxide removal/ sequestration Carbon footprint Carbon sinks Causes Climate Climate Crisis/ Emergency Climate justice Climate literacy climate stripes/ visualisation Climate zone shift clouds CO2/ carbon dioxide emissions Communication COP Cryosphere Deforestation Desertification Disaster risk management Drought Ecosystems Electric vehicles Energy Equity Evidence Extreme weather Feedback loops Fire weather Flood defences Flooding/ flood risk Fossil fuels Fuel security Global energy budget/ balance Green climate fund Greenhouse effect Greenhouse gas concentrations Heatwaves/ extreme heat Hydroelectric power Ice sheets Impacts IPCC Keeling curve Mitigation Modelling Nationally Determined Contributions (NDCs) Natural variability Nature based solutions Negotiations Net zero Nuclear power Observations Ocean acidification Ocean warming Per capita emissions Proxy records Regional climate change Renewable/ non fossil fuel energy Scenarios Schools Strike for Climate Society Solar energy Solutions Storms Sustainable Development Goals (SDGs) Temperature/ global warming Tipping points Transport Tropical cyclones Uneven impacts UNFCCC/ governance Urban green infrastructure Urban heat Urbanisation Water cycle Water security Water vapour (H2O) concentrations Weather Wild fires Wind power Choose an age range All ages Primary 0 to 7 7 to 11 Secondary 11 to 14 14 to 16 16 to 18 Latest from blog How climate links to GCSE and A Level Physics specifications The El Nino Southern Oscillation CPD Opportunities Participate in the Climate Literacy Survey 2026 Related resources … Secondary Geography 4. Atmospheric and Oceanic Circulation In this lesson we look at the pattern of circulation of the atmosphere and oceans, driven by the Sun. Secondary Geography, Secondary Science In Depth – The Coriolis Effect As air blows from high to low pressure in the atmosphere, the Coriolis force diverts the air so that it follows the pressure contours. Secondary Geography Atmosphere An atmosphere is defined as the gaseous envelope that surrounds a celestial body. Therefore, the Earth, like other planets in the solar system, has Secondary Geography How did the UK’s Temperature Change? How Did the UK’s Temperature Change Between 1960 and 2009?
Secondary Geography 4. Atmospheric and Oceanic Circulation In this lesson we look at the pattern of circulation of the atmosphere and oceans, driven by the Sun.
Secondary Geography, Secondary Science In Depth – The Coriolis Effect As air blows from high to low pressure in the atmosphere, the Coriolis force diverts the air so that it follows the pressure contours.
Secondary Geography Atmosphere An atmosphere is defined as the gaseous envelope that surrounds a celestial body. Therefore, the Earth, like other planets in the solar system, has
Secondary Geography How did the UK’s Temperature Change? How Did the UK’s Temperature Change Between 1960 and 2009?