quiz 5 Flashcards
(39 cards)
Carbon on the Planet
- Movement of carbon between the crust, oceans, atmosphere, plants, soil, and animals
- Most of the Earth’s carbon is stored in the planet’s crust
- Carbon dioxide is the most common gaseous form of carbon
- Photosynthesis: Conversion of carbon dioxide into organic compounds by plants.
Changing CO2 Content of the Atmosphere
- ~2 billion years ago
- CO2 was up, O was down
- Cyanobacteria a few billion years later
- CO2 down, O up
- Human Activities
- Human activities are contributing a lot to the increasing carbon dioxide
- Burning fossil fuels from the industrial revolution kickstarted all of this
- Agricultural practices
Natural and Human Carbon Exchange
- Carbon exchange is a natural phenomenon but is also human
- The more we urbanize, the more carbon dioxide in the atmosphere.
Measurement of CO2 in the Atmospheric: The Keeling Curve
- Direct measurement of CO2 concentration in the atmosphere from the 1950s to present
- Recorded from a Hawai‘ian island
- Overall increase in CO2 emissions
- Annual fluctuations due to northern hemisphere seasons (different landmass and vegetation)
- Northern spring: More CO2 absorbed
- Northern fall: More CO2 released
Measurement of CO2 in the Atmosphere: Proxy Records
- Proxy records estimate the Earth’s temperatures for thousands of years prior to direct measurement
- Tree rings
- Ice cores
- Sediments cores
- Corals
- Indicates there have been climate fluctuations in the past, but temperatures and the rate of change are higher than ever
The Greenhouse Effect
- The greenhouse effect is the process by which gases in the atmosphere trap heat
- Shortwave solar radiation (ultraviolet, visible light) enters the atmosphere, is absorbed by the earth, and then is re-radiated as longwave radiation (heat)
- The greenhouse effect is both natural and necessary for life on Earth!
- https://www.youtube.com/watch?v=SN5-DnOHQmE So, what is the problem?!
Greenhouse Gases
- Are rising higher and faster than ever before in a short amount of time, leading to socio-environmental changes
- Greenhouse gases comprise of:
- Carbon dioxide
- Water vapour
- Methane
- Nitrous oxide
- Chlorofluorocarbons
Increasing Greenhouse Gas Emissions and Changes in Climate
- Global average temperatures are rising, but the amount and rate of change varies
- Global warming → Climate change
- Doesn’t fully capture the whole scope with global warming
- Changes in precipitation patterns
- Sea level rise
- Droughts
- Melting ice caps
Variability
Magnitude (frequency and amplitude) of the changes that can occur
Risk
Potential to create adverse consequences for human or ecological systems
Vulnerability
People’s exposure and lack of protection towards environmental changes and extreme events
Impact
Damage (or positive effect) resulting from an event
Climate Change Impacts
- Potential agricultural losses
- Islands and coastal areas lost to sea level rise
- Species extinction
- Ecosystem collapse
- Increase in disease incidence
- Impacts will be felt most strongly by those who contribute little to global greenhouse gas emissions. They are mostly vulnerable populations who are too poor to mitigate or adapt to these impacts
Extreme Weather Events and Climate Change
- Emissions from the burning of fossil fuels have been trapping heat in the atmosphere since the Industrial Revolution
- This has increased global average temperatures by 1.1°C
- The additional energy stemming from the increasing temperatures is unevenly distributed causing some locations to experience extreme weather events compared to others WEATHER IS
- WHAT YOU GET AND CLIMATE IS WHAT YOU EXPECT!
More Persistent Droughts
- Less rain between heatwaves
- Water supplies and ground moisture run dry more quickly
- Ground heats up quicker = warming the air above = more intense heat
More Fuel for Wildfires
- Can be sparked by human activities, but also by natural events
- Related to heatwaves and droughts – the longer the heat lasts, the more moisture is drawn out, making the land tinder dry
- These tinder dry conditions help fuel wildfires which can spread very quickly
- Can lead to another weather system – pyrocumulonimbus clouds – that produces lightning, thus igniting more fires
More Extreme Rainfall
- More heat means more evaporation
- Warmer air can hold more water vapour
- For each temperature degree of warming, the air’s capacity for water vapour goes up by 7%
More or Less Hailstorms?
- Changes to atmospheric factors (atmospheric instability, temperature, and wind shear)
- But these atmospheric factors vary across the globe due to changes in weather patterns from climate change
- Future decrease in hailstorm frequency in East Asia and North America
- Future increase in Europe and Australia
Stronger Typhoons/Hurricanes/Cyclones
- Warming sea surface temperatures and higher subsurface sea temperatures removes the natural buffer on typhoon strength occasioned when cold water up wells from below the ocean’s surface
- Stronger typhoons carry more moisture, move faster, track differently, and will be aggravated by sea level rise
Climate Change Communication
- On the surface, climate change communication is about educating, informing, warning, persuading, mobilizing, and solving the socio-environmental problem.
- At a deeper level, climate change communication is shaped by our different experiences, mental and cultural models, and underlying values and worldviews
- Four factors contribute to how climate change communication is constructed, disseminated, and understood
- Scientists
- News media
- Politicians
- Social media
Scientists
- Initially communicated among scientists or climate specialists
- Technical language
- Quantitative
- Charts
- Graphs
News Media
- News media began to take climate change reporting seriously in the 1990s and continues today
- But there are peaks and troughs based on global climate events
- Climate reports more common in developed versus developing countries
- While the news media is great source for climate information, there are three common distortions of climate coverage
Three Common Distortions**
- Factual misrepresentation
- Get info as fast as they can before they do thorough research
- Scientific to laypeople language
- Journalistic timing
- Human-Interest Narratives
- Centres primarily on controversy, timeliness of events, and celebrities
- Alarmism
- Use of doom-and-gloom narratives
- Written in 1902, they were well aware about the temperature changes back then,
- coal consumption affecting the climate, written in 1912
- regions that are affected the most are talking about it more i.e., Latin America, Africa, etc.
Politicians
- As representations of climate change throughout the news media gradually captured public interest, politicians introduced various agreements and policies – some non-binding in scope – to govern how it was to be framed and communicated to the general public
- Climate change communication moves from technical (scientific) to narrative (media) to political (politician)