ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 26583
    Type of Medium: Monograph available for loan
    Pages: 171 S.
    Uniform Title: The physics of the stratosphere
    Language: Russian
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Monograph available for loan
    Monograph available for loan
    Moskva
    Call number: MOP 43464 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 436 S.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Oxford Univ. Press
    Call number: AWI A10-92-0279 ; MOP 47991
    Type of Medium: Monograph available for loan
    Pages: XIII, 519 S : graph. Darst. , 24 cm
    Edition: 2nd ed.
    ISBN: 0195051343
    Note: CONTENTS: 1. INTRODUCTION. - 1.1 The nature of the problem. - 1.2 The thermal structure of the atmosphere. - 1.3 The chemical composition of the atmosphere. - Bibliography. - 2. THEORY OF RADIATIVE TRANSFER. - 2.1 Definitions. - 2.1.1 Intensity, flux, energy density. - 2.1.2 Extinction and emission. - 2.1.3 Simple scattering. - 2.2 Thermal emission. - 2.2.1 Thermodynamic equilibrium. - 2.2.2 Breakdown of thermodynamic equilibrium. - 2.2.3 The interaction between matter and radiation. - 2.2.4 Discussion of the source function. - 2.2.5 Transitions between more than two levels. - 2.3 The integral equations. - 2.3.1 Introduction. - 2.3.2 The general solution. - 2.3.3 Thermal radiation in a stratified atmosphere. - 2.3.4 Solar radiation in a stratified atmosphere. - 2.4 Approximate methods for thermal radiation. - 2.4.1 The atmospheric problem. - 2.4.2 Transparent and opaque approximations. - 2.4.3 Approximate forms for the absorption coefficient. - 2.4.4 The method of moments in three dimensions. - 2.4.5 Approximations for a stratified atmosphere. - Bibliography. - 3. VIBRATION-ROTATION SPECTRA OF GASEOUS MOLECULES. - 3.1 Introduction. - 3.2 Vibration-rotation spectra. - 3.2.1 The Hamiltonian for a semirigid molecule. - 3.2.2 The states of the harmonic-oscillator, rigid-rotator model. - 3.2.3 Selection rules and line intensities. - 3.2.4 Interactions. - 3.3 The shape of a spectral line. - 3.3.1 Introduction. - 3.3.2 The Michelson-Lorentz theory. - 3.3.3 An adiabatic model. - 3.3.4 The Anderson-Tsao-Curnutte theory. - 3.3.5 The far wings of pressure-broadened lines. - 3.3.6 Doppler effects. - 3.4 Collision-induced and polymer spectra. - 3.5 Overview. - Bibliography. - 4. BAND MODELS. - 4.1 Introduction. - 4.2 Isolated lines. - 4.2.1 Single line of Lorentz shape. - 4.2.2 Single line with a Voigt profile. - 4.3 Distributed line intensities. - 4.3.1 Distribution functions. - 4.3.2 Application to the Lorentz profile. - 4.3.3 Application to the Doppler and Voigt profiles. - 4.4 The effect of overlap. - 4.4.1 Schnaidt's model. - 4.4.2 The method of Matossi, Meyer, and Rauscher. - 4.5 Regular models. - 4.5.1 The Elsasser model for Lorentz lines. - 4.5.2 The Curtis model. - 4.5.3 The Elsasser model for the Voigt profile. - 4.6 Random models. - 4.6.1 Introduction. - 4.6.2 Constant line intensity. - 4.6.3 The general random model. - 4.6.4 Verification of the theory. - 4.7 Generalized transmission functions. - 4.7.1 Superimposed regular and random bands. - 4.7.2 Deviations from the Voigt profile. - 4.7.3 Background continuum. - 4.8 k distributions. - 4.8.1 Band models and spectral representations. - 4.8.2 Calculations of k distributions. - 4.8.3 Overlapping bands. - 4.9 Models of complete bands. - 4.9.1 Band absorption areas. - 4.9.2 Empirical models. - 4.9.3 Exponential band contour. - 4.9.4 Semiempirical treatment. - Bibliography. - 5. ABSORPTION BY ATMOSPHERIC GASES. - 5.1 Introduction. - 5.2 Nitrogen. - 5.3 Oxygen. - 5.3.1 Ultraviolet, molecular absorptions. - 5.3.2 Forbidden bands in the vibration-rotation spectrum. - 5.3.3 The "atmospheric" bands. - 5.3.4 The collision-induced spectrum. - 5.3.5 Atomic oxygen. - 5.4 Water vapor. - 5.4.1 The vibration-rotation spectrum. - 5.4.2 Listed data. - 5.4.3 Continuum absorption. - 5.5 Carbon dioxide. - 5.5.1 The vibration-rotation spectrum. - 5.5.2 Listed data. - 5.5.3 The collision-induced rotation spectrum. - 5.6 Ozone. - 5.6.1 Electronic bands. - 5.6.2 The vibration-rotation spectrum. - 5.7 Nitrous oxide, carbon monoxide, and methane. - 5.7.1 Nitrous oxide. - 5.7.2 Carbon monoxide. - 5.7.3 Methane. - Bibliography. - 6. RADIATION CALCULATIONS IN A CLEAR ATMOSPHERE. - 6.1 Introduction. - 6.1.1 Line-by-line calculations. - 6.1.2 The angular integration. - 6.1.3 The frequency integration. - 6.2 Transmission through a nonhomogeneous atmosphere. - 6.2.1 Exact solutions for constant mixing ratio. - 6.2.2 Scaling approximations. - 6.2.3 The H-C-G approximation. - 6.2.4 Correlated k. - 6.3 Topics concerning heating rates. - 6.3.1 The Chapman layer. - 6.3.2 The Curtis matrix. - 6.3.3 Calculations for the middle atmosphere. - 6.4 Approximate methods. - 6.4.1 Exchange of radiation with the boundaries. - 6.4.2 Use of emissivities. - 6.4.3 Radiation charts. - 6.5 The inverse problem for thermal radiation. - 6.5.1 The Kernel functions. - 6.5.2 A "physical" approach to retrieval. - 6.5.3 Linear analysis. - Bibliography. - 7. EXTINCTION BY MOLECULES AND DROPLETS. - 7.1 The problem in terms of the electromagnetic theory. - 7.2 Scattering functions. - 7.3 Rayleigh's solution for small particles. - 7.4 Large particles as |m̃| → 1,300. - 7.5 Geometric optics. - 7.6 The Mie theory. - 7.7 Nonspherical particles. - Bibliography. - 8. RADIATIVE TRANSFER IN A SCATTERING ATMOSPHERE. - 8.1 Introduction. - 8.2 Integrodifferential equation. - 8.2.1 Fourier series expansion. - 8.2.2 Discrete ordinates. - 8.2.3 Feautrier method. - 8.3 Interaction principle. - 8.3.1 Adding two layers. - 8.3.2 The star semigroup. - 8.3.3 Doubling and adding. - 8.3.4 Invariant imbedding. - 8.3.5 X, Y, and H functions. - 8.4 Miscellaneous methods. - 8.4.1 Successive orders of scattering. - 8.4.2 The integral equation. - 8.4.3 Monte Carlo. - 8.4.4 Distribution of path lengths. - 8.4.5 Low-order approximations for anisotropic scattering. - 8.5 Numerical results. - 8.5.1 The diffusion exponent. - 8.5.2 X, Y, and H functions. - 8.5.3 Internal radiation field. - 8.5.4 Scattering by haze. - 8.5.5 Convergence of successive scatterings. - 8.5.6 The accuracy of low-order approximations. - 8.6 Applications. - 8.6.1 Solar and thermal fluxes in stratocumulus clouds. - 8.6.2 Polarization of light reflected from Venus. - 8.6.3 Scattered light in the stratosphere. - 8.6.4 Scattered light in clear water. - 8.6.5 CO2 lines in the reflection spectrum of Venus. - 8.6.6 The color and polarization of skylight. - Bibliography. - 9. ATMOSPHERES IN RADIATIVE EQUILIBRIUM. - 9.1 Introduction. - 9.2 An elementary solution. - 9.2.1 Without solar absorption. - 9.2.2 Absorption of solar radiation. - 9.3 Nongrey atmospheres. - 9.3.1 Models without pressure broadening. - 9.3.2 Pressure broadening. - 9.3.3 Numerical methods. - 9.4 The troposphere and the stratosphere. - 9.4.1 Introductio. - 9.4.2 The troposphere and the stratosphere. - 9.4.3 Convective models. - 9.4.4 Nonlocal dissipation. - 9.4.5 Semiconvection. - 9.5 The runaway greenhouse. - 9.5.1 History of ideas. - 9.5.2 Simpson's paradox. - 9.5.3 An evolving atmosphere. - 9.5.4 Influence of the tropospheric lapse rate. - Bibliography. - 10. EVOLUTION OF A THERMAL DISTURBANCE. - 10.1 Introduction. - 10.2 The radiation eigenvalue problem. - 10.2.1 The integral equation. - 10.2.2 Spiegel's solution. - 10.2.3 Two-stream solution for a scattering atmosphere. - 10.2.4 Effect of boundaries. - 10.3 Numerical results. - 10.3.1 Ni(∞) for atmospheric bands. - 10.3.2 Special absorption laws. - 10.3.3 Radiative relaxation for earth and Mars. - 10.3.4 Nonequilibrium source functions. - 10.4 Planetary-scale relaxation. - 10.4.1 The planetary relaxation rate. - 10.4.2 The temperature of a nonrotating atmosphere. - 10.5 The Newtonian cooling approximation. - 10.5.1 Transparent and boundary-exchange approximations. - 10.5.2 Internal gravity waves. - 10.6 Solar radiation in the middle atmosphere. - Bibliography. - Appendix 1. Physical constants. - Appendix 2. Spectroscopic units. - Appendix 3. A model atmosphere. - Appendix 4. Properties of water vapor. - Appendix 5. The Planck function. - Appendix 6. The exponential integrals. - Appendix 7. The Ladenburg and Reiche function. - Appendix 8. The Elsasser function. - Appendix 9. The physical state of the sun. - 9.1 The quiet sun. - 9.2 The solar spectrum. - 9.3 The intensity of solar radiation. -
    Location: AWI Reading room
    Location: MOP - must be ordered
    Branch Library: AWI Library
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 1976-02-01
    Print ISSN: 0032-0633
    Electronic ISSN: 1873-5088
    Topics: Geosciences , Physics
    Published by Elsevier
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 1967-10-01
    Print ISSN: 0032-0633
    Electronic ISSN: 1873-5088
    Topics: Geosciences , Physics
    Published by Elsevier
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 1966-11-01
    Print ISSN: 0004-637X
    Electronic ISSN: 1538-4357
    Topics: Physics
    Published by Institute of Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2005-03-15
    Description: Sampling retrievals of high-accuracy first-moment statistics constitute a central concern for climate research. Considered here is the important case of brightness temperature retrievals from a selection of possible orbits. Three-hourly global satellite brightness temperature data are used to predict the sampling error of monthly to annual mean brightness temperature retrieved by one or more satellites in low earth orbits. A true polar orbit is found to offer substantial advantages over a sun-synchronous orbit in the retrieval of annual mean brightness temperature, since the rotation of the local time of observation through two full diurnal cycles greatly reduces the error due to imperfect sampling of diurnal variations. Thus, a single polar orbiting satellite can produce annual mean, zonal mean brightness temperatures with typical sampling errors of less than 0.1 K, while even three sun-synchronous orbiters have high-latitude errors of up to 0.4 K. The error in retrievals of the annual mean diurnal cycle of brightness temperature is also discussed. In this case, high accuracy (
    Print ISSN: 0894-8755
    Electronic ISSN: 1520-0442
    Topics: Geography , Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 1989-04-01
    Print ISSN: 0022-4928
    Electronic ISSN: 1520-0469
    Topics: Geography , Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 1985-03-01
    Print ISSN: 0022-4928
    Electronic ISSN: 1520-0469
    Topics: Geography , Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 1990-08-01
    Print ISSN: 0022-4928
    Electronic ISSN: 1520-0469
    Topics: Geography , Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...