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The Climate Surprise

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Figure 5.2: World map depicng the pH of the oceans, including the large area of lower pH seawater off the west coast of South<br />

America. To be correct, the scale of ocean pH on the right should read “More Basic” and “Less Basic.” From Scienfi c American,<br />

March 2006.<br />

life, and that there has been no detectable trend<br />

from into the tweneth century.<br />

<strong>The</strong>re is every reason to believe that computer<br />

models are exaggerang the “sensivity” of ocean<br />

pH to CO levels in the same way as the models<br />

purporng to predict global temperature from<br />

increasing levels of CO have done.<br />

<strong>The</strong> most “acidic” (that is, least alkaline)<br />

area of the world’s oceans produces 20 percent<br />

of all the world’s wild fish catch. In the<br />

Humboldt Current off Peru 5 million tons of<br />

anchovies are brought aboard in a good year.<br />

<strong>The</strong> pH of this cold, upwelling water, rich in<br />

CO, is 7.7, lower than the probably inflated<br />

predicon for 2100. <strong>The</strong> source of this high<br />

producvity are the ny coccolithophores,<br />

phytoplankton that lap up the dissolved CO<br />

and turn it into food for zooplankton that feed<br />

the fish and whales and everything else in the<br />

sea. It turns out that seawater high in CO<br />

with a lower pH is the perfect environment for<br />

phytoplankton and corals, and, contrary to the<br />

alarmism touted by publicly funded sciensts,<br />

CO is ferlizing the oceans just like it is greening<br />

the earth (see Figure 5.2).<br />

Fourth, all organisms are able to control the<br />

chemistry of their internal organs and biochemical<br />

funcons. <strong>The</strong> term “homeostasis” means that<br />

an organism can maintain a desirable state of<br />

chemistry, temperature, etc., within itself under<br />

a wide range of external condions. This is especially<br />

necessary in a marine environment because<br />

the salinity of the ocean is too high to allow the<br />

metabolic processes that take place in an organism.<br />

<strong>The</strong> general term for an important part of<br />

homeostasis is “osmoregulaon.”<br />

And fih, if the present -year warming<br />

trend connues and the oceans warm, they will<br />

tend to release CO into the atmosphere because<br />

warm seawater at degrees Celsius can dissolve<br />

only about half as much CO as cold seawater at<br />

degrees Celsius. This would be balanced against<br />

the tendency of increased atmospheric CO to<br />

result in more absorpon of CO by the oceans.<br />

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