466 RADIATIVE HEAT TRANSFER
20.8 The new planet in an adjacent solar system recently found by Penn State (and other) researchers has been
determined to have an atmosphere consisting of nitrogen with 1% by volume NO. The planet’s surface has
an emittance of (ǫ=0.5), and a temperature of Ts=900 K. The atmosphere’s total pressure is known to be
p(z)=pse−z/L(surface pressure ps=5 bar, characteristic length L=10 km). Assuming radiative equilibrium
prevails, what is the heat loss from the planet? You may assume that for NO line broadening is unaffected by
temperature.
(a) To make a coarse approximation, replace the atmosphere by a constant pressure (ps) layer of a thick-
ness that would contain the correct total pressure path length. Evaluate radiative properties as if the
atmosphere’s temperature were constant at Ts.
(b) The problem is to be solved by the P1approximation combined with the box model. Find the appropriate
absorption coefficient(s) and other necessary parameters. You may assume that the spectral width of
bands for NO is unaffected by altitude (evaluate at surface conditions). Set up equation(s) and boundary
condition(s).
(c) Determine the heat loss from the planet.
(d) What would change if an infinitely thick atmosphere with exponentially decaying pressure were con-
sidered?
RnTs
8.3144kJ/kmol K900K =20.0g
m3
The box model parameters are found from equations (20.33) and (20.34) as
κ∆ηe=αρNO =9.0×20.0=180.0cm−1m−1
A(Lm)= ∆ηe(1 −e−κLm)≃∆ηe,
where Lmis the mean beam length from Table 20.1, Lm=1.76L=17.6 km. From Table 9.2: