The thermal wave equation

The thermal wave equation - surface, a little way below...

Info iconThis preview shows pages 1–2. Sign up to view the full content.

View Full Document Right Arrow Icon
The thermal wave equation If the heat flow through a volume changes with time the rate of change of temperature is given by the thermal wave equation: where K is the coefficient of thermal conductivity. If we look at the penetration into a planetary surface of temperature variations due to an external heat source, the we can reduce this to one dimension: We shall assume the forcing function is periodic. It could be the diurnal variability of solar input, or the annual or seasonal variation of heating. We can also assume that the temperature varies with depth as f(z) (where z is depth). Then we can substitute for T(z,t): This has a general solution: The first term is physically meaningless as it represents a temperature exponentially growing with depth. Thus the equation for T(z,t) can be written: This is a sinusoidally travelling wave moving into the material from the surface, with an amplitude that drops exponentially with depth. Thus if we apply a sinusoidal variation at the
Background image of page 1

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Background image of page 2
This is the end of the preview. Sign up to access the rest of the document.

Unformatted text preview: surface, a little way below there will be a sinusoidal variation with a smaller amplitude and phase shifted from the input. The further in the larger the phase shift and the smaller the amplitude. The temperature at a great depth approaches the average value of the input variation. This equation can be used to explain things like the existence of permafrost. In the tundra regions, although the surface temperature may go well above zero in the summer months, a few meters below the surface it oscillates around the yearly average of the surface, and if that is below zero, the ice below the surface will never melt. Notice also that the peak temperature will be phase lagged compared to the surface - there will be a layer below the surface where the maximum temperature occurs at the point where the surface is at its coldest....
View Full Document

This note was uploaded on 12/15/2011 for the course AST AST1002 taught by Professor Emilyhoward during the Fall '10 term at Broward College.

Page1 / 2

The thermal wave equation - surface, a little way below...

This preview shows document pages 1 - 2. Sign up to view the full document.

View Full Document Right Arrow Icon
Ask a homework question - tutors are online