Vietnam War: Forest Fire as a Military Weapon - Paperless Archives
Vietnam War: Forest Fire as a Military Weapon - Paperless Archives
Vietnam War: Forest Fire as a Military Weapon - Paperless Archives
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
SECRET<br />
4. <strong>Fire</strong>storm. Under exceptional circumstances, forest fires may develop into the phenomenon known <strong>as</strong><br />
"<strong>Fire</strong>storm."<br />
Although the term w<strong>as</strong> first used by the Police Commissioner of Hamburg to describe the effects of the<br />
RAF raids of 24-25 July, 1943, the phenomenon h<strong>as</strong> been noted in forest fires in America <strong>as</strong> far back <strong>as</strong> the great Peshtigo<br />
<strong>Fire</strong> of Wisconsin in 187 1. A firestorm occurs when a large area (generally greater than 2 1/2 square kilometers) is burning<br />
at one time under meteorological conditions such that the entrainment of air to the fire is confined to a relatively shallow<br />
layer near the surface, and air enters the fire area with an appreciable tendency to rotate. This combination results in the<br />
development of strong surf,-ce winds which act to fan the fire and incre<strong>as</strong>e its burning rate. The incre<strong>as</strong>ed burning rate<br />
causes more rapid air entrainment with a consequent further incre<strong>as</strong>e in wind speed, which incre<strong>as</strong>es burning rate still<br />
further which incre<strong>as</strong>es etc., etc. until all available fuel h<strong>as</strong> been burned. Wind velocities exceeding 100 miles per hour<br />
are often attained during peak firestorm development. 10/<br />
Experts are not in full agreement on the conditions necessary for firestorm formation.<br />
In general, any factor<br />
contributing to a rapid vertical heat rele<strong>as</strong>e rate, or to marked surface wind vorticity will be favorable. Such factors<br />
include:<br />
I. Heavy fuel loadings of unusually dry material.<br />
2. Many simultaneous ignitions.<br />
3. Intense solar insolation.<br />
4. An unstable atmospheric lapse rate.<br />
5. Marked vertical and/or horizontal wind shear.<br />
Since the winds are blowing into a firestorm area from all sides, the firestorm h<strong>as</strong> no rate of spread in the conventional<br />
sense-the entire firestorm area burns up <strong>as</strong> a unit. However, a firestorm almost always occurs on only a portion of<br />
a large forest fire. Consequently, the fire may be spreading actively at one location while a firestorm is keeping the fire<br />
stationary at another. Flame heights usually reach 100-150 feet in firestorms, and fl<strong>as</strong>hes of flame <strong>as</strong> high <strong>as</strong> 500-600 feet<br />
are not uncommon.<br />
Because of the intense heat and high winds, firestorms are extremely destructive. All dead material, regardless of<br />
size, and all living stems and branches smaller than 1-2 inches in diameter are consumed. <strong>Fire</strong>storms can be expected to<br />
cause extensive c<strong>as</strong>ualties to troops in the field. The mortality rate can be high, even among experienced firefighters.<br />
* when even a part of a forest fire reaches firestorm conditions.<br />
LOJ Anderson, H. E. Sundance <strong>Fire</strong>: An analysis of fire phenomena. USDA - <strong>Forest</strong> Service Research Paper INT - 56,<br />
37 pp., ilius. 1968.<br />
SECRET 8