Podcast
Questions and Answers
Explain how the hydrological cycle contributes to temperature changes.
Explain how the hydrological cycle contributes to temperature changes.
The hydrological cycle involves the exchange of energy. When water evaporates, it absorbs energy from its surroundings, leading to a cooling effect. Conversely, when water condenses, it releases energy and warms the environment.
How does the melting of polar ice contribute to a positive feedback loop that accelerates warming?
How does the melting of polar ice contribute to a positive feedback loop that accelerates warming?
Melting ice reduces the albedo effect, meaning less solar radiation is reflected back into space and more is absorbed by the darker ocean water. This causes further warming, leading to more ice melt, creating a positive feedback loop.
Describe the potential impact of large-scale freshwater deposits into the ocean as a result of melting ice.
Describe the potential impact of large-scale freshwater deposits into the ocean as a result of melting ice.
Large deposits of freshwater can disrupt the ocean conveyor belt, potentially stalling or reversing ocean circulation patterns. The ocean conveyor belt relies on heavy salt water to transport water, carbon and heat around the globe.
Explain how thermal expansion of seawater leads to sea-level rise.
Explain how thermal expansion of seawater leads to sea-level rise.
Discuss the implications of rising sea levels for coastal communities, particularly citing specific examples.
Discuss the implications of rising sea levels for coastal communities, particularly citing specific examples.
How does the melting of permafrost contribute to climate change, and why is methane a key concern?
How does the melting of permafrost contribute to climate change, and why is methane a key concern?
Explain the concept of ocean acidification and its impact on marine life, particularly organisms with shells and skeletons.
Explain the concept of ocean acidification and its impact on marine life, particularly organisms with shells and skeletons.
Describe how increased ocean acidity reduces the ability of the ocean to act as a carbon reservoir.
Describe how increased ocean acidity reduces the ability of the ocean to act as a carbon reservoir.
How do changes in climate patterns contribute to an increased frequency and severity of weather events?
How do changes in climate patterns contribute to an increased frequency and severity of weather events?
Explain how rising sea temperatures and ocean acidification could impact the distribution and survival of marine species, affecting ecosystems and potentially human food sources.
Explain how rising sea temperatures and ocean acidification could impact the distribution and survival of marine species, affecting ecosystems and potentially human food sources.
How might changes in temperature and rainfall patterns affect the suitability of different regions for agriculture?
How might changes in temperature and rainfall patterns affect the suitability of different regions for agriculture?
In what ways is climate change expected to influence human migration patterns, and what are the potential consequences?
In what ways is climate change expected to influence human migration patterns, and what are the potential consequences?
Explain how climate change can impact human health through various pathways.
Explain how climate change can impact human health through various pathways.
Describe how climate change may lead to geopolitical issues.
Describe how climate change may lead to geopolitical issues.
In what ways will climate change affect tourism?
In what ways will climate change affect tourism?
Flashcards
Global temperature increase: effects?
Global temperature increase: effects?
The increase in mean global temperature's effects include melting ice caps, shifting precipitation, and ecosystem changes.
Climate and weather pattern changes: cause?
Climate and weather pattern changes: cause?
Long-term changes in climate and weather patterns resulting from altered energy balance in Earth's atmosphere and oceans
Hydrological cycle: key role?
Hydrological cycle: key role?
The hydrological cycle involves the exchange of heat energy, which leads to temperature changes
Dark oceans and heat: impact?
Dark oceans and heat: impact?
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Global warming: Effect on water?
Global warming: Effect on water?
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Sea level changes: ice age link?
Sea level changes: ice age link?
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Melting permafrost: environmental impact?
Melting permafrost: environmental impact?
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Ocean acidification effects?
Ocean acidification effects?
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Climate patterns: influence on weather events?
Climate patterns: influence on weather events?
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Climate shifts: effect on species?
Climate shifts: effect on species?
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Warmer climate: impact on soil?
Warmer climate: impact on soil?
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Climate change: Employment impacts?
Climate change: Employment impacts?
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Global warming: social impacts?
Global warming: social impacts?
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Climate change: impacts on health?
Climate change: impacts on health?
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Arctic melt: trade route effects?
Arctic melt: trade route effects?
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Study Notes
Consequences of Global Climate Change
Effects on the Hydrosphere & Atmosphere
- Mean global temperature increases impact ecosystems and shifts precipitation patterns
- Higher greenhouse gas concentrations intensify extreme weather events like hurricanes and heavy rainfall
- Altered energy balance in Earth's atmosphere from long-term climate changes impacts weather patterns
- Thermal expansion of seawater and melting land ice due to greenhouse gases leads to sea level rise
Effects on water stores
- Temperature changes from the exchange of energy influences the hydrological cycle
- Evaporation cools the environment while condensation warms it, influencing local climate
- Reduced polar ice impacts polar ice and the albedo effect
- Ice melt releases fresh water into the oceans, altering the thermohaline pattern
- The thermohaline circulation relies on heavy salt water to transport water, carbon, and heat
- Large freshwater deposits can disturb or stall the ocean conveyor belt
- Dark oceans absorb more heat, boosting evaporation- a positive feedback loop
- Increased evaporation boosts cloud formation- a cooling effect (negative feedback)
- Higher temperatures increase humidity leading to more precipitation
- The atmosphere retains more moisture with higher temperatures
Changes in water availability
- Alterations in precipitation patterns can change water availability
- Some regions may have increased rainfall and floods, while other areas face frequent severe droughts impacting on agriculture, drinking water resources, and ecosystems
Sea-level change
- Thermal expansion of water and melting ice increases volume of water in ocean basins
- During the last Ice Age, sea levels fell, and rose again during the subsequent ice melt
- Greenland and Antarctica ice loss from 1992-2017, totaled 6.4 trillion tones causing a sea level rise of 17.8mm
- Ice sheets contribute to a third of sea level rise compared to 5% in the 1990s
- By 2100, polar temperatures could be 7°C above pre-industrial levels
- Sea levels have a significant affect on low-lying coasts and islands
- Pacific Ocean islands, such as Kiribati and Tuvalu are at risk of being submerged
Coastal flooding
- Coastal flooding and increased vulnerability to storm surges is due to rising sea levels
- Loss of land, infrastructure, and displacement of coastal communities can occur as a result
- Many of the world's densely populated areas are located on coastal lowlands
- New York and Miami are major cities vulnerable to sea-level rise
- Bangladesh is vulnerable because it's densely populated with a swamp forest
Carbon Stores
- Permafrost acts as a carbon sink of partially decomposed organic matter
- Melting triggers methane release as the plant/animal matter decomposes
- Methane is a potent greenhouse gas, creating a positive feedback loop
- There are 5 gigatons of methane in the atmosphere
- The Artic permafrost contains hundreds of gigatons of methane
- Polar ice sheets and glaciers are also stores of carbon
Impact of ice change
- Rising emperatures are causing ice melt across the world
- Glaciers in the Himalayas, Southern Alps, and Rockies are melting rapidly
- Ice melt releases freshwater for people living along rivers
Ocean acidification
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Oceans can absorb more atmospheric carbon and are important for regulating atmosphere
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Carbon is moved through the oceans in both directions
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Phytoplankton uses dissolved CO2 for photosynthesis
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Carbon is transported from the surface to the deep ocean levels
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Organisms sink and release CO2 into deep water stores upon death
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Some material transformed into rocks locks carbon into the long-term cycle
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Increased atmospheric CO2 causes higher CO2 absorption by oceans and leads to acidification
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Ocean acidification harms marine life, like coral reefs and shellfish
Carbon in the biosphere
- The biosphere acts as a large carbon sink
- CO2 is released naturally into the atmosphere through respiration and decomposition
- Humans release extra CO2 in the atmosphere
- Plants/Soils absorb 25% of human released CO2 through photosynthesis
- Too much atmospheric CO2 impairs plantgrowth and storage, and impacts crop yields
- Deforestation leads to CO2 release
Water cycle/carbon cycle feedback loop
- Water absorbs/transfers carbon with oceans absorbing 33% of CO2 emissions
- Oceans absorb most of human-generated CO2 although absorption has slowed
- Melting ice increases carbon storage, but is limited by dropping ocean pH levels which increase ocean acidification
- Warmer temperatures increase phytoplankton
- Phytoplankton releases dimethylsulphide (DMS), leading to increased cloud formation
- Insolation reduction reduces phytoplankton, which lessens cloud cover
- Rising ocean temperatures reduce photosynthesis in phytoplankton in cooler waters.
- Increasing ocean acidity impairs shell-forming marine creatures from extracting bicarbonate ions
Extreme Weather Events
- Changes in climate patterns increase the frequency & severity of weather events
- There has been an increase in extreme weather events Since the 1980s
- Floods, storms, and extreme temperatures are frequently occurring
- The Atlantic hurricane season lasts from June 1 - November 30
- Tropical storms commonly form in the North Atlantic during this time
- Annually 14(avg) named storms occur with six hurricanes (Cat 3), and 3 major hurricanes (Cat 4+)
- 2021 produced 21 named storms (winds of 62+ km/h), with 7 hurricanes (winds of 119+ km/h) of which 4 were major hurricanes (winds of 178+ km/h)
- Drought describes a period of below average rainfall
- Droughts vary from place to place with different vegetation
- Water supplies can be depleted as people abstract water during a drought
- Droughts are often accompanied by rising temperatures and water supplies are depleted
- Length of a drought varies with place
- UK suffered a drought for 16 months (1975-1976)
- In any given year, 14% of the USA is in drought
- The Horn of Africa is experiencing its worst drought in 40 years
- Changes in atmospheric circulation patterns affect precipitation in an area
- An El Niño cycle affects Australia and Indonesia causing droughts
- Weather system and high pressure systems cause rates of evaporation
- A heat wave is when temperatures are higher than average for a prolonged time (UK means 3 consecutive days)
Projected impacts of rising temperatures
Effects on the Biosphere
- Ecosystems play a role in carbon cycling
- The availability of moisture impacts with the animal distribution and importance of growth
- Changes in Temperature/ rainfall and habitat affects species survival patterns and interactions
- Conditions will improve crops and ecosystems, but others will suffer as an affect
- Move north/south because they need specific climate conditions
- Polar/Tundra biomes are at risk as they are move futher N/S
- Rising sea temperatures/ocean acidification has caused coral bleaching
- Migration/ behavior patterns has changed
- Longer distances to find cooler climates, reduced pests, diseases and predators
- Fish species are already moving N/S
- Reduced hibernation time as temperatures are increasing
- Migrations begin annual as birds leave and head north for summer
- Soil erosion reduces fertility because Rainfall/ low vegetation
Impacts on Agriculture
- Suitable areas will change in order for agriculture
- Farmers will change crops
- Areas will grow on areas not used
- Coastal flooding
- Water shortages, irrigation/ limits crops to be chosen
- Food shortages due to malnutrition and Famine
- A rise of 3°C would reduce crop yields to 35% (across Africa and the Middle East)
- A rise of 2°C(200 million) affect the cause of hunger
Effects on People & Places
- Loss of job opportunities due to changes in agriculture/tourism
- Coastal resorts risk as resorts will close because of lack of snow
- Farmers either change crop or leaving farmlands
- Floodings due to sea level rises will leads to displacement of large numbers of people
Homes
- Homes will need additional defences sea level rise
- Moving settlements or improving food levels
- Social migration and the increase of human migration with Lowed islands
Health Hazards
- Climate changes affect human in many ways
- Heatwaves ,weather events, disease negative/ health consequence, respiratory, spreading infectious disease
- Water-borne is spreading and is high in temperature
- Heartstroke
- Dehydration increases skin burns
- Pollution levels high
- Respiratory increased and suffer from asthma
Tourism & Transport
- Ocean transport which 90% of global trade
- Sea routes which 90% open ships will sovereign waters
- routes and the volume of sea vessels by shorter canals
- Arctic ice pack 2009 shipping between Atlantic over the year
- 40% shorter now
- Arctic environments will impact ships
- Egypt could use upto 60% loss
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