Inverse problem of thermal radiation transfer accounting for non-LTE effects has been considered for limb geometry in the spectral region covering 10.4 mu m, 15 mu m CO2 and 9.6 mu m O-3 bands. Limb radiance has been calculated line-by-line on the basis of the non-LTE model describing day-time non-equilibrium populations of the vibrational states of CO2 and O-3 molecules which correspond to the bands under consideration. The inverse problem for the satellite limb radiance high resolution measurements in the spectral interval 540-1150 cm(-1) has been posed with respect to the simultaneous retrieval of the vertical profiles of pressure, kinetic temperature, number density of main absorbers, and vibrational temperatures of the states mentioned...
International audienceSince January 2004, the planetary Fourier spectrometer (PFS) on board the Mars...
Inverted planetary limb radiance for determining earth atmosphere temperature from orbiting satellit
Since the beginning of the industrial revolution (1750 to 1800) the Earth’s atmospheric composition ...
Inverse problems of the remote sensing of the atmosphere are formulated for the general case of an o...
Peculiarities of formation of outgoing limb radiance under non-LTE conditions in spectral lines of C...
The report contains the results of investigations performed in frame of Cooperation Agreement for 19...
MIPAS is a limb viewing fourier transform spectrometer operating in the infra-red. It scans the tang...
International audienceThe MIPAS instrument on board Envisat, in Earth orbit, the PFS and OMEGA instr...
The project was aimed at the retrieval of densities of trace gases and temperatures in the mesospher...
Recently, several new generation instruments for far infrared and microwave remote sensing of the Ea...
[1] Nonlocal thermodynamic equilibrium (non-LTE) simulations of the (CO)-C-12-O-16(1 -> 0) fundament...
As the dominant anthropogenic greenhouse gas, carbon dioxide (CO2), represents an important componen...
A description of an improved non-LTE model together with earlier two-level and multi-level models is...
Spectroscopy and forward modelling consistency and accuracy in the ν2 and ν3 fundamental absorption ...
A series of sensitivity studies is carried out to explore the feasibility of space-based global carb...
International audienceSince January 2004, the planetary Fourier spectrometer (PFS) on board the Mars...
Inverted planetary limb radiance for determining earth atmosphere temperature from orbiting satellit
Since the beginning of the industrial revolution (1750 to 1800) the Earth’s atmospheric composition ...
Inverse problems of the remote sensing of the atmosphere are formulated for the general case of an o...
Peculiarities of formation of outgoing limb radiance under non-LTE conditions in spectral lines of C...
The report contains the results of investigations performed in frame of Cooperation Agreement for 19...
MIPAS is a limb viewing fourier transform spectrometer operating in the infra-red. It scans the tang...
International audienceThe MIPAS instrument on board Envisat, in Earth orbit, the PFS and OMEGA instr...
The project was aimed at the retrieval of densities of trace gases and temperatures in the mesospher...
Recently, several new generation instruments for far infrared and microwave remote sensing of the Ea...
[1] Nonlocal thermodynamic equilibrium (non-LTE) simulations of the (CO)-C-12-O-16(1 -> 0) fundament...
As the dominant anthropogenic greenhouse gas, carbon dioxide (CO2), represents an important componen...
A description of an improved non-LTE model together with earlier two-level and multi-level models is...
Spectroscopy and forward modelling consistency and accuracy in the ν2 and ν3 fundamental absorption ...
A series of sensitivity studies is carried out to explore the feasibility of space-based global carb...
International audienceSince January 2004, the planetary Fourier spectrometer (PFS) on board the Mars...
Inverted planetary limb radiance for determining earth atmosphere temperature from orbiting satellit
Since the beginning of the industrial revolution (1750 to 1800) the Earth’s atmospheric composition ...