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Energy and Human Ambitions on a Finite Planet, 2021a

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9 Climate Change 139<br />

1. mass ratio: how many grams of CO 2 are produced per gram 1 of 1: ...oranymass/weight measure you prefer<br />

input fuel;<br />

2. carb<strong>on</strong> intensity: how many grams of CO 2 are produced per unit<br />

of energy delivered.<br />

While all forms produce a mass ratio of approximately 3 units of CO 2 for<br />

every unit of fossil fuels, the lower energy density of coal together with<br />

its slightly higher mass ratio 2 make it more than twice as carb<strong>on</strong>-intense<br />

as natural gas.<br />

Example 9.1.1 Roughly how much CO 2 is produced from each full<br />

tank of gasoline in a car?<br />

2: Coal produces more CO 2 per gram of<br />

fuel because the other fossil fuels also c<strong>on</strong>tain<br />

mass in the form of hydrogen, which<br />

not <strong>on</strong>ly adds to energy producti<strong>on</strong> but also<br />

does not end up in CO 2 .<br />

A typical tank might hold about 50 L of gasoline (13 gall<strong>on</strong>s). The<br />

density of gasoline is 0.75 kg/L, so that <strong>on</strong>e tank has a gasoline mass<br />

of about 38 kg. Applying the simple <str<strong>on</strong>g>and</str<strong>on</strong>g> c<strong>on</strong>venient factor-of-three<br />

ratio of CO 2 mass to input fuel mass, we see that <strong>on</strong>e tank of gasoline<br />

will produce something like 110 kg of CO 2 —not a small amount!<br />

9.1.1 CO 2 Measurements<br />

Beginning in 1958, Dave Keeling of the Scripps Instituti<strong>on</strong> of Oceanography<br />

began recording CO 2 c<strong>on</strong>centrati<strong>on</strong> in the atmosphere from the top<br />

of Mauna Loa in the middle of the Pacific ocean. 3 In additi<strong>on</strong> to seeing<br />

annual variati<strong>on</strong> due to the seas<strong>on</strong>al cycle of photosynthesis, 4 he began<br />

to see a steady year-by-year increase in the level. The measurements have<br />

c<strong>on</strong>tinued to the present, now known as the “Keeling Curve,” shown in<br />

Figure 9.1.<br />

3: ...farfrom c<strong>on</strong>tinental influences<br />

4: Plants seas<strong>on</strong>ally absorb <str<strong>on</strong>g>and</str<strong>on</strong>g> then release<br />

CO 2 as leaves grow <str<strong>on</strong>g>and</str<strong>on</strong>g> then die.<br />

420<br />

1.2<br />

400<br />

1.0<br />

CO2 (ppmV)<br />

380<br />

360<br />

340<br />

320<br />

300<br />

280<br />

1960 1970 1980 1990 2000 2010<br />

−0.2<br />

2020<br />

year<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0.0<br />

Temperature rise ( ± C)<br />

Figure 9.1: In blue (left axis), CO 2 measurements<br />

from Mauna Loa (Hawaii) for the last<br />

60 years, showing a relentless <str<strong>on</strong>g>and</str<strong>on</strong>g> accelerating<br />

upward trend now at abut 2.6 ppm v<br />

per year [50]. Seas<strong>on</strong>al variati<strong>on</strong>s due to<br />

photosynthesis are seen <strong>on</strong> top of this trend.<br />

Pre-industrial levels were around 280 ppm v ,<br />

so that we have added about 130 parts per<br />

milli<strong>on</strong> (ppm). Red dots (right axis) show<br />

global average mean temperature records<br />

over the same period [51]. Thus far, global<br />

average temperature has risen about 1 ◦ C.<br />

Note that the Kyoto Protocol in 1997 <str<strong>on</strong>g>and</str<strong>on</strong>g><br />

Paris Agreement in 2015 (Box 19.4; p. 320)<br />

do not visibly curb the upward trajectory<br />

of CO 2 emissi<strong>on</strong>s.<br />

© 2021 T. W. Murphy, Jr.; Creative Comm<strong>on</strong>s Attributi<strong>on</strong>-N<strong>on</strong>Commercial 4.0 Internati<strong>on</strong>al Lic.;<br />

Freely available at: https://escholarship.org/uc/energy_ambiti<strong>on</strong>s.

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