Carbon Dioxide and Earth's Future Pursuing the ... - Magazooms
Carbon Dioxide and Earth's Future Pursuing the ... - Magazooms
Carbon Dioxide and Earth's Future Pursuing the ... - Magazooms
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www.co2science.org<br />
P a g e | 90<br />
In ano<strong>the</strong>r study, Lewis, et al. (2009a), in a thorough review of <strong>the</strong> scientific literature, noted<br />
that both <strong>the</strong>ory <strong>and</strong> experiments suggest that over <strong>the</strong> past several decades “plant<br />
photosyn<strong>the</strong>sis should have increased in response to increasing CO2 concentrations, causing<br />
increased plant growth <strong>and</strong> forest biomass,” <strong>and</strong> <strong>the</strong>y did indeed find that “long-term plot data<br />
collectively indicate an increase in carbon storage, as well as significant increases in tree<br />
growth, mortality, recruitment, <strong>and</strong> forest dynamism,” that satellite measurements “indicate<br />
increases in productivity <strong>and</strong> forest dynamism,” <strong>and</strong> that five Dynamic Global Vegetation<br />
Models, incorporating plant physiology, competition, <strong>and</strong> dynamics, all predict increasing gross<br />
primary productivity, net primary productivity, <strong>and</strong> carbon storage when forced using latetwentieth<br />
century climate <strong>and</strong> atmospheric CO2 concentration data,” while noting that “<strong>the</strong><br />
predicted increases in carbon storage via <strong>the</strong> differing methods are all of similar magnitude<br />
(0.2% to 0.5% per year).” And so <strong>the</strong>y concluded that “<strong>the</strong>se results point toward a widespread<br />
shift in <strong>the</strong> ecology of tropical forests, characterized by increased tree growth <strong>and</strong> accelerating<br />
forest dynamism, with forests, on average, getting bigger (increasing biomass <strong>and</strong> carbon<br />
storage).”<br />
Contemporaneously, Tans (2009) employed measurements of atmospheric <strong>and</strong> oceanic carbon<br />
contents, along with reasonably constrained estimates of global anthropogenic CO2 emissions,<br />
to calculate <strong>the</strong> residual fluxes of carbon (in <strong>the</strong> form of CO2) from <strong>the</strong> terrestrial biosphere to<br />
<strong>the</strong> atmosphere (+ values) or from <strong>the</strong> atmosphere to <strong>the</strong> terrestrial biosphere (- values),<br />
obtaining <strong>the</strong> results depicted in <strong>the</strong> following figure.<br />
Five-year smoo<strong>the</strong>d rates of carbon transfer from l<strong>and</strong> to air (+) or from air to l<strong>and</strong> (-) vs.<br />
time. Adapted from Tans (2009).<br />
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