Saturday, November 21, 2015

Carbon Cycle Part 2

DATA TABLES: CARBON CYCLE


LESSON 2

Lesson 2:
Step 1
Gaseous Carbon
Ocean Water
Biosphere Gaseous Carbon
To Year
Atmosphere
Ocean Surface
Deep Ocean
Soil
Terrestrial Plants
2010
391ppm
1000GT
38,000GT
2000GT
700GT
2060
360ppm
1010GT
38,062GT
1899GT
697GT
2110
353ppm
1007GT
38,089GT
1993GT
692GT














Lesson 2:
Step 2


Gaseous Carbon

To Year
Net Def. Rate
Fossil Fuel % Increase
Atmosphere
Deep Ocean
2010
0.5GT
0.3
391ppm
38,000GT
2060
0.5GT
0.3
478ppm
38,198GT
2100
0.5GT
0.3
536ppm
38,454 GT



Graphs Info:
  1. Atmospheric Carbon Levels Measured in ppm
  2. Everything else measured in GT
  3. Diamonds are points where data was recorded   


        Questions on Step 1:
  1. Unlike what happened in lesson 1 when we had CO₂ emissions, the gaseous carbon levels atmosphere decreased to only 353ppm by 2100. Now, while the CO₂ did not reach the Prue-industrial levels of below 280ppm it did significantly lower over the next 100 years, while I was around with the simulator I ran it to the year 3000 and in the year 2240 atmospheric carbon levels flat lined at 347ppm. 


  2. As you can see, when we have no more fossil fuel consumption there is still an increase in the level of greenhouse gasses in ocean surface and deep ocean, as well as a decrease in soil and terrestrial plants; however, the change is far less drastic than it was in lesson 1. 

    Questions on Step 2: 
    1. A high carbon level will add almost 500GT of CO₂ into the deep ocrean. It is important to keep an eye on the CO₂ levels in the deep ocean because the more CO₂ that is in the ocean the less habitable the deep ocean is.
    2. When decreasing net deforestation to -1.5GT per year and maintaining the 0.3% fossil fuel consumption rate, it actually increases the atmospheric carbon level in 2100 to 540ppm.




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