Search results
Results From The WOW.Com Content Network
The last two components are the rate of fire spread if fuel is available for combustion, and the frontal fire intensity. [2] The essential information needed to calculate this index is: the humidity of the air at the beginning of the afternoon (when it has its lowest value); the temperature in the middle of the afternoon (when it has its ...
The output section of the NFDRS structure chart is the components or simply the outputs that are based in fire behavior description but expressed in the broader context of fire danger rating. [ 6 ] Spread Component – Displays a value numerically equivalent to the predicted forward rate of spread of a head fire in feet per minute.
The McArthur Forest Fire Danger Index (FFDI) was developed in the 1960s by CSIRO scientist A. G. McArthur to measure the degree of danger of fire in Australian forests. The index combines a record of dryness, based on rainfall and evaporation, with meteorological variables for wind speed , temperature and humidity.
Haines Index (also known as the Lower Atmosphere Severity Index) is a weather index developed by meteorologist Donald Haines in 1988 that measures the potential for dry, unstable air to contribute to the development of large or erratic wildland fires. [1]
The representation is made on a temperature-relative humidity, instead of a standard psychrometric chart. The comfort zone in blue represents the 90% of acceptability, which means the conditions between -0.5 and +0.5 PMV, or PPD < 10%.
The 4 percent rule was popularized in a landmark 1998 research report known as the “Trinity study,” which analyzed past market performance to determine a safe withdrawal rate in retirement.
For premium support please call: ... Multiply non-health insurance expenses by 28 — roughly equal to a 3.5% withdrawal rate — multiply expected health insurance costs by 40 and put aside 12-24 ...
The Penman equation describes evaporation (E) from an open water surface, and was developed by Howard Penman in 1948. Penman's equation requires daily mean temperature, wind speed, air pressure, and solar radiation to predict E. Simpler Hydrometeorological equations continue to be used where obtaining such data is impractical, to give comparable results within specific contexts, e.g. humid vs ...