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Maclean et al. - 2002 - Rice almanac source book for the most important e

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Sun<br />

Chlorofluorocarbons attack <strong>the</strong><br />

stratospheric ozone layer<br />

Ozone<br />

filters UV<br />

radiation<br />

Visible light<br />

passes through<br />

greenhouse<br />

gases<br />

Heat trapped by greenhouse<br />

gases warms Earth and<br />

decreases rice productivity<br />

in <strong>the</strong> tropics<br />

Flooded rice fields<br />

emit m<strong>et</strong>hane<br />

<strong>Rice</strong> fields<br />

Greenhouse gases in<br />

atmosphere are increasing:<br />

• carbon dioxide<br />

• m<strong>et</strong>hane<br />

• nitrous oxide<br />

Carbon dioxide<br />

increases<br />

rice growth<br />

Fig. 1. How glob<strong>al</strong> climate change affects tropic<strong>al</strong> rice. Greenhouse gases trap heat and warm Earth's<br />

surface. Higher temperatures reduce <strong>the</strong> productivity of tropic<strong>al</strong> rice. The two <strong>most</strong> <strong>important</strong> greenhouse<br />

gases <strong>for</strong> rice are CO 2<br />

, which may enhance rice growth, and CH 4<br />

, which is emitted by flooded rice fields.<br />

Degradation of <strong>the</strong> atmospheric ozone layer <strong>al</strong>lows more biologic<strong>al</strong>ly destructive UV-B radiation to reach<br />

Earth's surface. The effects of UV-B on rice are not known.<br />

Oxygen<br />

(O 2<br />

)<br />

M<strong>et</strong>hane<br />

(CH 4<br />

)<br />

<strong>Rice</strong><br />

plant<br />

(CH 4<br />

)<br />

(CH 4<br />

)<br />

Ebullition<br />

Diffusion<br />

Water<br />

(CH 4<br />

)<br />

O 2<br />

CO 2<br />

Oxidation<br />

(CH 4<br />

)<br />

Decomposition of<br />

soil organic matter<br />

Fig. 2. M<strong>et</strong>hane gas escapes into <strong>the</strong> atmosphere from flooded rice fields in three ways. Up to 80% travels<br />

through <strong>the</strong> plant from <strong>the</strong> roots. Ebullition, in which gas bubbles up to <strong>the</strong> water surface, and diffusion<br />

each contribute sm<strong>al</strong>ler amounts.<br />

Internation<strong>al</strong> issues 39

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