Carbon Cycle and Climate Change PDF

Document Details

TenaciousMahoganyObsidian

Uploaded by TenaciousMahoganyObsidian

Texas A&M University - College Station

Tags

carbon cycle climate change greenhouse gasses environmental science

Summary

This document details concepts related to the carbon cycle and climate change. It covers topics like emissions, radiative forcing, and the effects of climate change, including ocean acidification, coral bleaching and increased temperatures.

Full Transcript

# Carbon Cycle and Climate Change ## Carbon Cycle - **Starts with carbon cycle:** - **Carbon cycle buckets:** - Oceans - Land biosphere - Atmosphere - **How carbon in atmosphere:** - Exhale - Burn fossil fuels - Livestock - Volcano - **How carbon out:**...

# Carbon Cycle and Climate Change ## Carbon Cycle - **Starts with carbon cycle:** - **Carbon cycle buckets:** - Oceans - Land biosphere - Atmosphere - **How carbon in atmosphere:** - Exhale - Burn fossil fuels - Livestock - Volcano - **How carbon out:** - Plants - Dissolves in ocean - **Carbon into living things:** - Cellular respiration - **Carbon in ocean:** - Dissolves - **Emission of CD lead to beat:** - CD are higher now - Added CD make the world get warmer - As long as the CD level is higher than the industrial base level the world will continue to warm. - Even if emission input stopped temp would still rise - Using models to predict climate change - Concentration pathways of CD - The numbers - CD would cause mean radiative forcing - Socio economic pathway - Story lines, actions we take - Different futures how they effect all CD - Things that directly effect - Different ways we could handle Pop / GDP - Math / Numbers ## Climate Change - **There is no difference between the 5 pathways for the first 10 years because change takes time.** - **1.5° is not a goal we can stay below, but...** - **Impact** - Going up - Population is going up - Affluence is going up (standard of living continually increases) - Technology impact on emissions, brings it down - Carbon intensity - Energy intensity - **Heating is uneven.** - **The Arctic is heating the most** - **Cause of CC in the past and future:** - Strength of the sun. - No, - Volcanic activity - No, cooling effect - Orbital changes - No, too slow - Greenhouse gasses - Yes, it traps the heat in the atmosphere and acts relatively fast - Water vapor feedback - Yes - **Impacts of CC** - Worse near the Gulf of Mexico / Southern U.S. - Because of sea level rise (flooding, loss of infrastructure, salt water intrusion, severe droughts) - Tourism - Habitat loss ## Effects of Climate Change - **Direct and indirect effects of CC:** - Ocean acidification - Carbon is added to the atmosphere, then dissolves in ocean - Coral bleaching - Ocean temp changes (too warm) - Bigger crops - Increase in CD - Less water / less energy produced by hydroelectric farms - Rain is falling in unusual places - An effect US would face if an artic ice sheet melts - Increase sea level - **Organizations taking CC seriously:** - Oil and gas companies - Lots of people with good quality information - Military - Stock trading companies - **What does an exponential graph increase greatly?** - Because it multiples by what's already there. - Climate change exponential growth: - Water vapor feedback - Temperature - Population - GDP - Diseases - **Social cost of carbon** - Interest rate (rate of growth) - Carbon can cost farmers their jobs when they can no longer grow that crop - The impact of CC affects society in webs. ## Understanding Climate Change - **Radiative forcing:** - Changes that alter the energy absorbed or emitted by the Earth and its atmosphere - The amount that the energy balance is disrupted by a change in a climate input: - A change in Earth's energy balance: Energy in - Energy out - Positive forcing example: Decrease in atmospheric aerosols - Positive feedback example: If a radiative forcing decreases energy coming into the Earth, a positive feedback would result in... - A temp decrease - Ice-albedo effect is a feedback - CO2 and methane and equally emitted and absorbed without human activity - Raising livestock increases the amount of methane in the atmosphere - Carbon dioxide - Natural contributions to the atmosphere are much larger than human inputs - Lasts a much longer time in the atmosphere - Methane - More powerful greenhouse gas - We know that volcanoes are not responsible for carbon dioxide increase by measuring the amounts of carbon 12 and carbon-13 isotopes in atmospheric carbon dioxide - We don't know if there is a limit CD in the biosphere and ocean can remove - Temperature variations on a scale of decades: - Internal unforced variability - Changes in the Earth's orbit - Changes in greenhouse gasses - Natural cycles are not a cause of climate change because... - There is not a physical mechanism that explains how these natural cycles could be causing the warming. ## Modelling Climate Change - Scientists have not been able to simulate a climate model in which natural cycles cause overall warming - There is no evidence that these cycles have caused past climates to warm or cool outside of the ups and downs within the cycle - Scientists don't attribute modern global warming to changes in solar radiation because they have observed and measured changes that are either too long-term or cyclical - Ways continental drift can cause climate change: - Continents located where ice sheets can form - Blocking or allowing North / South ocean currents - Exposing new rock to weathering. - Human greenhouse gas emissions are responsible for modern global warming because it is unequivocal that humans have increased greenhouse gas concentrations and warmed the atmosphere - Factors that influence human greenhouse gases and aerosol emissions: - GDP - Population - The major differences in climate forecasts: - Changes in greenhouse gas emissions - Representative Concentration Pathways (RCP): Predicted radiative forcing in 2100 - Shared Socioeconomic Pathways (SSP): Choices that humans make regarding society and development - Biggest inaccuracy in how climate models predict the future climate.. - They don't show realistic year to year variability - What helps to decrease "IPAT": - Switching from fossil fuels to renewable energy sources - Using more energy efficient machines and processes

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