Clive M. Countryman

Summary

Clive M. Countryman Heat-Its Role in Wildland Fire… (1975)

Variation in radiative heating controls weather The angle at which the sun's radiation strikes the earth's surface varies with the time of year and with latitude. Heating is greatest along a band at the equator, where the incoming radiation is most nearly perpendicular, and least at the poles, where the radiation strikes the earth at a low angle. At any latitude, land masses are heated more than are the oceans. This variation with latitude and between land and water masses creates widespread temperature differences in the atmosphere, thus generating large-scale air circulation patterns.
Source: Wikisource

Clive M. Countryman Heat-Its Role in Wildland Fire… (1975)

Fire is a high temperature heat source—much of its thermal radiation is in the visible wavelengths. When heat is transferred from a fire to unburned fuel principally by radiation, rate of spread of fire is usually slow. However, the characteristics of radiation often make it significant in fire behavior. Because transfer of heat by radiation does not depend on movement of flames and hot combustion products, it transfers heat in all directions and against the wind. Thus, a fire may spread in an unexpected direction when radiation is significant.
Source: Wikisource

Clive M. Countryman Heat-Its Role in Wildland Fire… (1975)

Solar radiation provides the energy for photosynthesis, hence vegetation provides a storage reservoir for the sun's energy. This energy, often accumulated over years, is released quickly when the vegetation burns. In the absence of precipitation, the moisture content of dead fuel is affected to some extent by the fuel temperature, but the effect of relative humidity is much stronger. And for a given air mass, relative humidity is controlled almost entirely by air temperature, which in turn is closely related to solar radiation intensity.
Source: Wikisource

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