Simulations of Carbon-Dioxide Equilibrium Infrared Radiation Measurements

2018 ◽  
Vol 32 (1) ◽  
pp. 184-195 ◽  
Author(s):  
A. Lemal ◽  
H. Takayanagi ◽  
S. Nomura ◽  
K. Fujita
2021 ◽  
pp. 96-121
Author(s):  
Raymond T. Pierrehumbert

‘Planetary climate and habitability’ studies planetary climate, particularly the way an atmosphere affects temperature and a planet's habitability. The entire temperature profile, from the planet's centre to the tenuous outer reaches of its atmosphere (if it has one), is of importance. Real atmospheres are never completely transparent to the infrared radiation which seeks to escape to space. Gases which are good absorbers of infrared radiation act as planetary insulation. This is the greenhouse effect, and gases that are good infrared absorbers are called greenhouse gases; carbon dioxide is an important greenhouse gas for Earth.


Author(s):  
Sayaka Nishimura ◽  
Adrien Lemal ◽  
Hiroki Takayanagi ◽  
Satoshi Nomura ◽  
Shingo Matsuyama ◽  
...  

1978 ◽  
Vol 100 (2) ◽  
pp. 235-239 ◽  
Author(s):  
G. L. Hubbard ◽  
C. L. Tien

A simple procedure has been developed for the calculation of the Planck mean emission and absorption coefficients and the Rosseland mean absorption coefficient for infrared radiation of the soot-gas mixtures commonly occurring in luminous flames and smoke. Specific results are presented for mixtures involving carbon dioxide, water vapor and carbon soot, the dominant species in most combustion systems. The close agreement between the various averages clearly demonstrates the usefulness of the mean absorption coefficient concept for applications.


2018 ◽  
Vol 32 (2) ◽  
pp. 483-494 ◽  
Author(s):  
H. Takayanagi ◽  
A. Lemal ◽  
S. Nomura ◽  
K. Fujita

Tellus ◽  
1965 ◽  
Vol 17 (2) ◽  
pp. 147-165 ◽  
Author(s):  
Wilford Zdunkowski ◽  
Donald Henderson ◽  
J. Vern Hales

1967 ◽  
Vol 89 (4) ◽  
pp. 321-327 ◽  
Author(s):  
M. M. Abu-Romia ◽  
C. L. Tien

In this paper, a study is made on the calculation of appropriate mean absorption coefficients for the infrared radiation of gases. The Planck and Rosseland mean absorption coefficients for the optically thin and optically thick gases are expressed as functions of the spectroscopic and thermodynamic properties of the gas. Values of the Planck and Rosseland mean absorption coefficients are presented for carbon monoxide, carbon dioxide, and water vapor in the temperature range from 1000 to 5000 deg Rankine. To illustrate the application of these results, the radiative heat flux is calculated for the simple case of a planar medium.


Sign in / Sign up

Export Citation Format

Share Document