climate change
- Created by: Elin jennings
- Created on: 16-03-13 15:06
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- climate change
- what is it?
- its a contiinuous cycle of warming and colling of the planet, and the changing weather patterns.
- past evidence for climate change
- rocks
- the characteristics of different rocks depend on the environment in which the sediment were deposited.
- fossils
- different species of plants need different conditions to survive. some plants and animals are sensitive to climate and do not adapt easily to change
- pollen and spores
- plants produce pollens and spores that are particularly useful in helping to determine climate.
- microfossils
- they require a specific living conditions, but they are more abundant and are found in many types of sedimentary rocks.
- rocks
- evidence
- ice cores
- +6oo,ooo years of evidence
- tree rings
- +larger rings represent warmer/wetter years.
- +provides 100's of years of climate evidence
- butterflies
- all species of animals and plants are sensitive to changing climate especially butterflies
- eg mountain ringlet butterfly (uk)
- all species of animals and plants are sensitive to changing climate especially butterflies
- historical evidence
- past evidence for climate change
- rocks
- the characteristics of different rocks depend on the environment in which the sediment were deposited.
- fossils
- different species of plants need different conditions to survive. some plants and animals are sensitive to climate and do not adapt easily to change
- pollen and spores
- plants produce pollens and spores that are particularly useful in helping to determine climate.
- microfossils
- they require a specific living conditions, but they are more abundant and are found in many types of sedimentary rocks.
- rocks
- paintings of thames ice fairs in the 18th and 19th century.
- past evidence for climate change
- sediment cores
- we study oxygen isotopes.
- there used to be no oxygen in the atmosphere.
- oxygen isotopes tells us how much oxygen was in the air and tells us about the the developing climate change.
- there used to be no oxygen in the atmosphere.
- this gives us evidence of past temperatures.
- we study oxygen isotopes.
- there used to be no oxygen in the atmosphere.
- oxygen isotopes tells us how much oxygen was in the air and tells us about the the developing climate change.
- there used to be no oxygen in the atmosphere.
- we study oxygen isotopes.
- we study oxygen isotopes.
- ice cores
- greenhouse effect
- increase in greenhouse gases
- human causes
- agriculture
- increase in agriculture such as ranching gases such as methane as does paddy rice fields
- defforestaion
- less trees means less co2 can be absorbed
- amazon rainforest 'lungs of the earth'
- industry and powerstations
- burning fossil fuels to meet our growing demand for electricity and consumer goods. coal, gas, oil, powerstations emit: co2, co, so2 and noxides
- transport
- cars, ships, planes, and trains, all use (mostly) fossil fuels to run
- economic development
- people and countries become wealthier more consumer products and more infastructure (airports, roads waterpipes etc..) means more energy used.
- agriculture
- natural (physical) causes
- the green house effect
- greenhouse effect
- increase in greenhouse gases
- human causes
- agriculture
- increase in agriculture such as ranching gases such as methane as does paddy rice fields
- defforestaion
- less trees means less co2 can be absorbed
- amazon rainforest 'lungs of the earth'
- industry and powerstations
- burning fossil fuels to meet our growing demand for electricity and consumer goods. coal, gas, oil, powerstations emit: co2, co, so2 and noxides
- transport
- cars, ships, planes, and trains, all use (mostly) fossil fuels to run
- economic development
- people and countries become wealthier more consumer products and more infastructure (airports, roads waterpipes etc..) means more energy used.
- agriculture
- natural (physical) causes
- the green house effect
- more green house gasses = warming
- less green house gasses = cooling
- volcanic eruptions
- lots of ash can lead to cooling
- many years of eruptions will increase greenhouse gasses = warming
- the earths tilt, wobble and orbit changes
- the green house effect
- human causes
- increase in greenhouse gases
- more green house gasses = warming
- less green house gasses = cooling
- greenhouse effect
- volcanic eruptions
- lots of ash can lead to cooling
- many years of eruptions will increase greenhouse gasses = warming
- the earths tilt, wobble and orbit changes
- the green house effect
- human causes
- increase in greenhouse gases
- what is it?
- sun
- ground
- outgoing terrestrial radiation
- gets bounced back into the atmosphere
- this is a continious effect
- this is a continious effect
- greenhouse gases
- gets bounced back into the atmosphere
- outgoing terrestrial radiation
- ground
- incoming solar radiation (insolation)
- greenhouse gases
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