Red Admiral
17th June 2006, 06:28
Temperature vs. Altitude
Temperature decreases with altitude according to the formula;
Temperature = Initial Temperature + Altitude*Temperature Lapse Rate
This relationship is derived from empirical evidence, not theoretical results. The Temperature Lapse Rate for air is -0.0065K/m
At sea level, the mean temperature is 288K (15°C).
The graph below shows the variation of temperature with altitude;
http://img.photobucket.com/albums/v12/red_admiral/temperatevsaltitude.jpg
As can be seen, the temperature decreases with altitude until about 17km at which point it stabilises to a value of c.180K (actually it increases slightly). This point is the boundary of the troposphere and stratosphere which varies in height between 6000 and 17000m at the poles and equator respectively. It is not a distinct boundary and varies with weather and other atmospheric affects.
next, Pressure and Density.
Temperature decreases with altitude according to the formula;
Temperature = Initial Temperature + Altitude*Temperature Lapse Rate
This relationship is derived from empirical evidence, not theoretical results. The Temperature Lapse Rate for air is -0.0065K/m
At sea level, the mean temperature is 288K (15°C).
The graph below shows the variation of temperature with altitude;
http://img.photobucket.com/albums/v12/red_admiral/temperatevsaltitude.jpg
As can be seen, the temperature decreases with altitude until about 17km at which point it stabilises to a value of c.180K (actually it increases slightly). This point is the boundary of the troposphere and stratosphere which varies in height between 6000 and 17000m at the poles and equator respectively. It is not a distinct boundary and varies with weather and other atmospheric affects.
next, Pressure and Density.