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The biosphere is also the source of aerosols, such as spores, pollen, bacteria, and other particles. These aerosols scatter incoming radiation, affecting the energy budget. And some marine organisms produce sulfate particles, which act as condensation centers for cloud formation. As the number of such condensation centers increases, more, and consequently smaller, cloud droplets are formed. A cloud made of many small droplets is highly reflective and prevents solar radiation from reaching the earth. Any anthropogenic (human) production of sulphur could produce a similar effect, moderating a warming trend. |
Evidences and Uncertainties |
Many species live in very sensitive ecological niches, so even small changes in temperature or precipitation could drastically alter their ability to survive. Oak trees in the midwestern U.S., for example, may not tolerate an average temperature only a few degrees higher than current temperatures. And even increases in ocean temperatures of as little as 1°C over two or three days can cause coral—organisms particularly sensitive to long-term variations in climate—to lose their symbiotic algae, which are essential for their nutrition. When the algae die, corals are “bleached” and appear white. (See “Current Coral Bleaching Hot Spots” on this site to learn more.) Because all species are linked in complex webs of predator, prey, and habitat, impacts on one species always affect others—and it’s extremely difficult to predict how those effects will manifest themselves. Changing the life cycles of key species in food chains may well affect an entire ecosystem. |
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