TY - JOUR
T1 - Development of a Line-by-Line and a Correlated k-Distribution Radiation Models for Planetary Atmospheres
AU - Takahashi, Yoshiyuki O.
AU - Hayashi, Yoshi Yuki
AU - Hashimoto, George L.
AU - Kuramoto, Kiyoshi
AU - Ishiwatari, Masaki
N1 - Funding Information:
The authors would like to thank Michael A. Mischna for providing us data of radiative fluxes and temperature tendencies shown in his paper. We are also grateful to two anonymous reviewers for their constructive comments on this article. Visualization software developed by GFD Dennou Club, Dennou Club Library (DCL) and GPhys, are used to make plots shown in this study. A supercomputer of the Education Center on Computational Science and Engineering, Kobe University is used to perform several calculations shown in this study. This study was funded by Grant-in-Aid for Scientific Research on Innovative Areas (JSPS KAKENHI Grant Numbers 17H06457 and 19H05605) from Japan Society for the Promotion of Science.
Publisher Copyright:
© The Author(s) 2023.
PY - 2023
Y1 - 2023
N2 - A set of line-by-line and correlated k-distribution radiation models are developed aiming for applications in simulations and examinations of Venus and Mars-like planetary atmospheres. Our line-by-line model is validated by comparing the results with observations and those of previous studies under conditions of Venus, and present and possible early Mars. The radiation fields calculated by our line-by-line model agree well with observed profiles and are within the acceptable range from those presented in previous studies. The results obtained by our line-by-line model are then processed to generate a series of parameters for our correlated k-distribution model. It is confirmed that the radiation fields calculated with those sets of parameters by our correlated k-distribution model sufficiently agree with those by our line-by-line model for the atmospheres with a wide range of surface pressure. By the use of our correlated k-distribution model implemented with those sets of parameters, we evalu-ate the radiation field for Venus and calculate radiative-convective equilibrium profiles for Venus and Mars. The obtained vertical thermal structures for Venus are qualitatively consistent with observations, and the behaviors of surface pressure and surface temperature for Mars are similar to those reported by previous studies. Those results demonstrate that our models including the procedure for generating tables of radiation parameters are applicable to examine climates of CO2 dominant atmospheres in our solar and exoplanetary systems.
AB - A set of line-by-line and correlated k-distribution radiation models are developed aiming for applications in simulations and examinations of Venus and Mars-like planetary atmospheres. Our line-by-line model is validated by comparing the results with observations and those of previous studies under conditions of Venus, and present and possible early Mars. The radiation fields calculated by our line-by-line model agree well with observed profiles and are within the acceptable range from those presented in previous studies. The results obtained by our line-by-line model are then processed to generate a series of parameters for our correlated k-distribution model. It is confirmed that the radiation fields calculated with those sets of parameters by our correlated k-distribution model sufficiently agree with those by our line-by-line model for the atmospheres with a wide range of surface pressure. By the use of our correlated k-distribution model implemented with those sets of parameters, we evalu-ate the radiation field for Venus and calculate radiative-convective equilibrium profiles for Venus and Mars. The obtained vertical thermal structures for Venus are qualitatively consistent with observations, and the behaviors of surface pressure and surface temperature for Mars are similar to those reported by previous studies. Those results demonstrate that our models including the procedure for generating tables of radiation parameters are applicable to examine climates of CO2 dominant atmospheres in our solar and exoplanetary systems.
KW - Mars
KW - planetary atmosphere
KW - radiation
KW - Venus
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U2 - 10.2151/jmsj.2023-003
DO - 10.2151/jmsj.2023-003
M3 - Article
AN - SCOPUS:85147710244
SN - 0026-1165
VL - 101
SP - 39
EP - 66
JO - Journal of the Meteorological Society of Japan
JF - Journal of the Meteorological Society of Japan
IS - 1
ER -