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Climate and Energy

The Earth gets energy from the sun and core of the earth is still quite hot. The energy from the sun is the main driver of the climate on Earth. The energy from the sun is not evenly distributed over the Earth’s surface. The equator gets more energy than the poles. The energy from the sun is absorbed by the Earth and then re-emitted as infrared radiation. The Earth’s atmosphere absorbs some of this infrared radiation and re-emits it back to the Earth’s surface. This is the greenhouse effect. Without this greenhouse effect, we would be living in a much colder world.

Relatively recently, the concentration of atmospheric carbon dioxide has been increasing, although the concentration of CO2 has been estimated to be higher in the past. It is believed that the recent increase in CO2 is due primarily to burning of fossil fuels.

Heat from the Core of the Earth

The core temperature of the Earth is estimate to be 6,000 C under very high pressures, composed primarily or iron (Anzellini et al. (2013)). The heat flux to the surface from the core is on average 0.1 W/m^2.

Heat from the Sun

The heat flux from the sun is approximately 1360 W/m^2 (oscillating every 24 hours depending a little on the time of year and latitude). The Earth’s surface temperature is about 15 C. The Earth’s surface temperature is determined by the balance between the energy from the sun and the energy from the core.

Earth's Heat Balance

Figure 2:Image of the Earth’s heat balance. Similar images and information in https://earthobservatory.nasa.gov/features/EnergyBalance/page2.php.

The energy incident on the atmosphere from the sun, is absorbed and re-emitted by the Earth’s surface, primarily as infrared radiation. That incident radiation has a wide range of wavelengths. Water, a very powerful greenhouse gas varies from 1-4% of the atmosphere (depending on many factors). The concentration of CO2 is about 0.04% or 400 ppm of the atmosphere.

Mass Balance

The mass of the atmosphere is estimated to be 5.15e18 kg. The amount of fossil fuels burned by the world is approximately 136 terawatt-hours. If the average energy density of fossil fuels is 40 MJ/kg, then the mass of fossil fuels burned is approximately 1.2e10 kg.

atmosphere = 5.15e14 #kg, low, only including a portion of the atmosphere
molesinatmosphere = atmosphere/0.029 #moles
energyff = 136e6 #megawatt-hours, energy from fossil fuels burned
energyff_SI = energyff*3600 #Mega-Joule
ffburned = energyff_SI/40 #kg of fossil fuels burned
print(f'The approximate mass of fossil fuels burned is {ffburned:0.3e}, kg')
#If 1 mole of fossil fuel reacts to form one mole of CO2 and the average molecular weight of 
# fossil fuels is 0.17 kg/mol
molesCO2emitted = ffburned/0.17 #kg fossil fuels to mole of fossil fuel which is equivalent to moles of co2
print(f'The approximate moles of co2 emitted per year is {molesCO2emitted:0.3e}, mol/year')
print(f'The moles in the atmosphere is {molesinatmosphere:0.3e}, mol')
The approximate mass of fossil fuels burned is 1.224e+10, kg
The approximate moles of co2 emitted per year is 7.200e+10, mol/year
The moles in the atmosphere is 1.776e+16, mol
dnCO2dt=nCO2innCO2out\frac{dn_{CO2}}{dt} = n^{in}_{CO2} - n^{out}_{CO2}
dnco2dt = molesCO2emitted/molesinatmosphere*1e6 #ppm of CO2 emitted per year
print(f'The estimated rate of change of CO2 in the atmosphere is {dnco2dt:.2f} ppm/year')
The estimated rate of change of CO2 in the atmosphere is 4.05 ppm/year

Currently the rate of increase of ppm of CO2 is about 2 ppm/year. Thus, the approximately other half of the CO2 is absorbed by the oceans and elsewhere.

Global Fossil Fuel Consumption

Figure 3:Global fossil fuel consumption as a function of time from https://ourworldindata.org/grapher/global-fossil-fuel-consumption.

Carbon Cycle

Carbon dioxide is produced by the oxidation of carbon. Many sources of oxidation occur naturally including:

  • respiration of animals

  • decomposition of organic matter (aerobic bacteria)

  • volcanic activity

  • forest fires

  • oceanic release of CO2

  • weathering of rocks (carbonate rocks)

Carbon dioxide is removed from the atmosphere by:

  • photosynthesis

  • oceanic uptake of CO2

  • deposition of carbon in sediments

Oxygen Cycle

Oxygen is produced when water is split by photosynthesis or through other reduction mechanisms. Oxygen is consumed by respiration of animals and decomposition of organic matter. The oxygen cycle is closely linked to the carbon cycle.

Water Cycle

Water is evaporated from the surface of the Earth and then condenses in the atmosphere. The water cycle is driven by the energy from the sun. The water cycle is closely linked to the amount of energy incident on the Earth’s surface and the amount absorbed and reflected by the atmosphere.

Industrial Revolution and Energy Needs

The industrial revolution began in the 18th century in England. The industrial revolution was driven by the need for energy to power machines. The primary source of energy was coal. As more people have come to earth, the energy needed to support each other has increased together with our quality of life. More energy use correlates with a higher quality of life.

Energy Balance

With the same energy input and output, the Earth’s temperature is stable. It is estimated, that the increase in green house gases, primarily CO2 (and water) is causing the Earth’s temperature to increase. The Earth’s temperature is increasing at a rate of about 0.2 C per decade. The Earth’s surface atmospheric temperature has increased by about 1 C since the industrial revolution (in the last 150 years). The Earth’s temperature has been higher in the past, but the rate of change now is much faster.

dnUdt=nin(Hin+1/2Mvin2+Mgzin)nout(Hout+1/2Mvout2+Mgzout)+Q+Ws\frac{dnU}{dt} = n_{in}(H_{in} + 1/2Mv_{in}^2 + Mgz_{in}) - n_{out}(H_{out} + 1/2Mv_{out}^2 + Mgz_{out}) + Q + W_s

What does a simple mass balance of the atmosphere yield in terms of a temperature change if there is an increase in the Earth’s surface radiation of 1 W/m^2?

Correlation

Increasing concentration of CO2 appears to be correlated (with causation) with the burning of fossil fuels for our energy needs.

There is correlation with that increasing concentration of CO2 and the Earth’s temperature. It’s also correlated with the rise in sea levels, melting of glaciers, and other changes in the Earth’s climate.

What should be done?

References
  1. Anzellini, S., Dewaele, A., Mezouar, M., Loubeyre, P., & Morard, G. (2013). Melting of Iron at Earth’s Inner Core Boundary Based on Fast X-ray Diffraction. Science, 340(6131), 464–466. 10.1126/science.1233514
  2. Guymon, C. (2025). Foundations of Spiritual and Physical Safety: with Chemical Processes.