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Botkin Environmental Science Earth as Living Planet 8th txtbk

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12.1 Forests and Forestry 241<br />

FIGURE 12.5 Forest ownership in the lower 48 states of the United States in 2008.<br />

(Source: U.S. Forest Service, Northern Research Station.)<br />

As we mentioned, wood is a major energy source in<br />

many parts of the world. Some 63% of all wood produced<br />

in the world, or 2.1 million m 3 , is used for firewood. Firewood<br />

provides 5% of the world’s total energy use, 10 2% of<br />

total commercial energy in developed countries, but 15%<br />

of the energy in developing countries, and is the major<br />

source of energy for most countries of sub-Saharan Africa,<br />

Central America, and continental Southe<strong>as</strong>t Asia. 11<br />

As the human population grows, the use of firewood<br />

incre<strong>as</strong>es. In this situation, management is essential, including<br />

management of woodland stands (an informal<br />

term that foresters use to refer to groups of trees) to improve<br />

growth. However, well-planned management of firewood<br />

stands h<strong>as</strong> been the exception rather than the rule.<br />

How Forests Affect the Whole <strong>Earth</strong><br />

Trees affect the earth by evaporating water, slowing erosion,<br />

and providing habitat for wildlife (see Figure 12.6). Trees<br />

can also affect climate. Indeed, vegetation of any kind can<br />

affect the atmosphere in four ways, and since forests cover<br />

so much of the land, they can play an especially important<br />

role in the biosphere (Figure 12.7):<br />

1. By changing the color of the surface and thus the<br />

amount of sunlight reflected and absorbed.<br />

2. By incre<strong>as</strong>ing the amount of water transpired and<br />

evaporated from the surface to the atmosphere.<br />

3. By changing the rate at which greenhouse g<strong>as</strong>es are<br />

rele<strong>as</strong>ed from <strong>Earth</strong>’s surface into the atmosphere.<br />

4. By changing “surface roughness,” which affects wind<br />

speed at the surface.<br />

In general, vegetation warms the <strong>Earth</strong> by making the<br />

surface darker, so it absorbs more sunlight and reflects less.<br />

The contr<strong>as</strong>t is especially strong between the dark needles<br />

of conifers and winter snow in northern forests and between<br />

the dark green of shrublands and the yellowish soils<br />

of many semiarid climates. Vegetation in general and forests<br />

in particular tend to evaporate more water than bare<br />

surfaces. This is because the total surface area of the many<br />

leaves is many times larger than the area of the soil surface.

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