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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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