click below
click below
Normal Size Small Size show me how
BIO II: Exam 2
Carbon Cycle Intro
| Term | Definition |
|---|---|
| Name all 6 Pools of Carbon | - Rocks/Fossil Fuels - Soils - Atmosphere - Biosphere (anything alive) - Ocean (surface & deep ocean often considered separately) |
| Pool | How Carbon is stored |
| Processes (Flux) | How Carbon moves between pools |
| Name all 8 Processes/Flux | - Photosynthesis - Respiration - Soil Respiration - Combustion - Vulcanism - Decomposition - Diffusion - Sedimentation |
| What are NOT related to climate (4 things) | - Hole in ozone layer - Smog/Pollution - Acid Rain - Ocean Acidification |
| Climate (w/ example) | An upward trend in the 30 year average of the frequency & intensity of hurricanes (Ex: average date of the last freeze in the spring continues to get earlier) |
| Weather (w/ example) | Short-term day-to-day atmospheric conditions (Ex: Severe thunderstorms or hurricane/ a late spring freeze event) |
| What happens if we INCREASE how much energy is reflected into space | Earth would be COOLER |
| What happens if we DECREASE how much energy is reflected into space | Earth would be WARMER |
| Albedo | Reflectivity of a surface HIGH albedo = HIGH reflectivity LOW albedo = LOW reflectivity |
| Name what is associated with HIGH and LOW albedo | High Albedo: - light colored - reflects more light/energy Low Albedo: - dark colored - absorbs more light/energy |
| What are the TOP 5 GHG's? | 1) Carbon Dioxide 2) Nitrous Oxide 3) Methane 4) Fluorinated Gases 5) Water Vapor (not anthropogenic) |
| Milankovitch Cycles | - Natural and VERY long-term fluctuations in sun intensity - Natural orbital changes (tilt, wobble, shape of orbit) → affect sunlight distribution → ice ages - Responsible for Ice Ages |
| What can alter the greenhouse effect? | - Changing the amount ABSORBED by the atmosphere - Small increases in Greenhouse Gases can increases temperature |
| What are the TWO factors of Global Warming Potential (GWP)? | 1) How well it absorbs light energy (and reemits IR_heat) 2) Residence Time (how long it remains in the atmosphere) |
| What is the baseline greenhouse gas? | Carbon Dioxide (CO2) GWP of CO2 = 1 |
| What are the Global Warming Potential of the 4 anthropogenic GHG's? | 1) Carbon Dioxide (CO2)= 1 2) Nitrous Oxide (N2O)= ~300 3) Methane (CH4)= ~20 4) Fluorinated Gases (CFC's)= Average ~5000 |
| Greenhouse Effect | Process where greenhouse gases (GHGs) trap heat in Earth’s atmosphere |
| Climate Impact | - GWP x quantity of gas - Overall contribution to climate change - CO2 is the HIGHEST anthropogenic GHG |
| Anthropogenic | Human causes |
| What is the contribution of each anthropogenic GHG? | 1) Carbon Dioxide (CO2)= 64% 2) Methane (CH4)= 19% 3) Fluorinated Gases (CFC's)= 11% 4) Nitrous Oxide (N2O)= 6% |
| Carbon Cycle | - How carbon moves and changes - How carbon is converted from one form to another |
| What's going on in the ocean? | 1. CO2 diffuses in 2. Taken up by phytoplankton (photosynthesis) 3. When they die, they sink (sedimentation) 4. After many years, become rock 5. Long-term C storage |
| Long-term Cycle | Involves putting carbon back into the Rock pool and Fossil Fuel Pool (Millions of Years) |
| Short-term Cycle | Involves carbon moving in and out of the atmosphere |
| Volcanoes | Ash and aerosols increase reflection → temporary cooling |
| Source vs Sink | Source: Release (ex: burning fossil fuels, deforestation) Sink: Absorbs (ex: oceans, forests, etc.) |
| Current CO2 Concentration | 425.48 ppm (quiz says 422 or 423) (pre-industrial concentration: ~280 ppm) |
| How does the carbon cycle relate to the greenhouse effect? | Increased atmospheric CO₂ intensifies the greenhouse effect, leading to global warming and climate change |