Cargando…

Atmospheric radiation : theoretical basis /

Detalles Bibliográficos
Clasificación:QC912.3 G6.62 1989
Autor principal: Goody, Richard M. (autor)
Otros Autores: Yung, Y. L. (autor)
Formato: Libro
Idioma:Inglés
Publicado: New York : Oxford University Press, [1989].
Edición:Second edition.
Temas:
Tabla de Contenidos:
  • 1. Introduction.
  • Nature of the problem.
  • Thermal structure of the atmosphere.
  • Chemical composition of the atmosphere.
  • 2. Theory of Radiative Transfer. Thermal emission.
  • Integral equations.
  • Approximate methods for thermal radiation.
  • 3. Vibration-Rotation Spectra of Gaseous Molecules. Vibration-rotation spectra.
  • Shape of a spectral line.
  • Collision-induced and polymer spectra .
  • 4. Band Models. Isolated lines.
  • Distributed line intensities.
  • Effect of overlap.
  • Regular models.
  • Random models.
  • Generalized transmission functions.
  • k distributions.
  • Models of complete bands.
  • 5. Absorption by Atmospheric Gases. Nitrogen.
  • Oxigen.
  • Water vapor.
  • Carbon dioxide.
  • Ozone.
  • Nitrous oxide, carbon monoxide, and methane.
  • 6. Radiations calculations in a clear Atmosphere. Transmission through a nonhomogeneous atmosphere.
  • Topics concerning heating rates.
  • Approximate methods.
  • Inverse problem for thermal radiation.
  • 7. Extinction by Molecules and Droplets. Problem in terms of the electromagnetic theory.
  • Scattering functions.
  • Rayleigh's solution for small particles.
  • Large particles as m-1.
  • Geometric optics
  • The Mie theory.
  • Nonspherical particles.
  • 8. Radiative Transfer in a Scattering Atmosphere. Integrodifferential equation.
  • Interaction principle.
  • Miscellaneous methods.
  • Numerical results.
  • Applications.
  • 9. Atmospheres in a Radiative Equilibrium. Elementary solution.
  • Nongrey atmospheres.
  • Troposphere and the stratosphere.
  • Runaway greenhouse.
  • 10. Evolution of a Thermal Disturbance. Radiation eigenvalue problem.
  • Numerical results.
  • Planetary-scale relaxation.
  • Newtonian cooling approximation.
  • Solar radiation in the middle atmosphere.