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ROTATIONAL RAMAN SPECTROSCOPY OF ETHYLENE USING A FEMTOSECOND TIME-RESOLVED  PUMP-PROBE TECHNIQUE
ROTATIONAL RAMAN SPECTROSCOPY OF ETHYLENE USING A FEMTOSECOND TIME-RESOLVED PUMP-PROBE TECHNIQUE

PDF) Corrigendum to “N2, O2, and air broadening of NH3 in ν2 band measured  by FTIR spectroscopy” [J. Mol. Spectrosc. 173 (1995) 591–602] | Koichi  Yamada - Academia.edu
PDF) Corrigendum to “N2, O2, and air broadening of NH3 in ν2 band measured by FTIR spectroscopy” [J. Mol. Spectrosc. 173 (1995) 591–602] | Koichi Yamada - Academia.edu

Lidar depolarization ratio of soot fractal aggregates: spectral dependence  over the visible-to-infrared spectrum
Lidar depolarization ratio of soot fractal aggregates: spectral dependence over the visible-to-infrared spectrum

Journal of Quantitative Spectroscopy & Radiative Transfer 2000: Vol 66  Table of Contents : Free Download, Borrow, and Streaming : Internet Archive
Journal of Quantitative Spectroscopy & Radiative Transfer 2000: Vol 66 Table of Contents : Free Download, Borrow, and Streaming : Internet Archive

Editorial Journal of Quantitative Spectroscopy & Radiative Transfer
Editorial Journal of Quantitative Spectroscopy & Radiative Transfer

Second Derivative Tunable Diode Laser Spectrometry for Line Profile  Determination. II. Experimental Results
Second Derivative Tunable Diode Laser Spectrometry for Line Profile Determination. II. Experimental Results

PDF) The Reference Forward Model (RFM)
PDF) The Reference Forward Model (RFM)

Calculating the characteristics of a photoionization tea CO <Subscript>2  </Subscript> laser
Calculating the characteristics of a photoionization tea CO <Subscript>2 </Subscript> laser

PDF) Numerical optimization of Mean Absorption Coefficient in Air using  Planck Modified Mean Function
PDF) Numerical optimization of Mean Absorption Coefficient in Air using Planck Modified Mean Function

An Investigation of Non-Equilibrium Effects in Thermal Argon Plasmas
An Investigation of Non-Equilibrium Effects in Thermal Argon Plasmas

PDF) Multi-spectral ozone spectroscopy (SMO3) project
PDF) Multi-spectral ozone spectroscopy (SMO3) project

Optimization of iterative solvers for DDA-SI
Optimization of iterative solvers for DDA-SI

Spectral polarization distribution models (PDMs) for NASA CLARREO  Pathfinder's inter-calibration applications Solar radiation
Spectral polarization distribution models (PDMs) for NASA CLARREO Pathfinder's inter-calibration applications Solar radiation

J. Quant. Spectrosc. Radiat. Transfer Vol. 53, No. 2, pp. 165-178, 1995  TRANSPORTABILITY OF A LASER-INDUCED FLUORESCENCE CALIBRA
J. Quant. Spectrosc. Radiat. Transfer Vol. 53, No. 2, pp. 165-178, 1995 TRANSPORTABILITY OF A LASER-INDUCED FLUORESCENCE CALIBRA

J. Quant. Spectrosc. Radiat. Transfer. Vol. 6, pp. 903-908. Pergamon Press  Ltd., 1966. Printed in Great Britain NOTE ELECTRONIC
J. Quant. Spectrosc. Radiat. Transfer. Vol. 6, pp. 903-908. Pergamon Press Ltd., 1966. Printed in Great Britain NOTE ELECTRONIC

The spectrum of N2 from 4,500 to 15,700 cm−1 revisited with PGOPHER | UNB  Scholar
The spectrum of N2 from 4,500 to 15,700 cm−1 revisited with PGOPHER | UNB Scholar

PDF) GARLIC - A General Purpose Atmospheric Radiative Transfer Line-by-Line  Infrared Code: Implementation and Evaluation
PDF) GARLIC - A General Purpose Atmospheric Radiative Transfer Line-by-Line Infrared Code: Implementation and Evaluation

Journal of Quantitative Spectroscopy and Radiative Transfer |  ScienceDirect.com by Elsevier
Journal of Quantitative Spectroscopy and Radiative Transfer | ScienceDirect.com by Elsevier

Microprocessor-controlled Data Acquisition System for Pulsed Laser  Spectroscopy
Microprocessor-controlled Data Acquisition System for Pulsed Laser Spectroscopy

Single scattering albedo of homogeneous, spherical particles in the  transition region
Single scattering albedo of homogeneous, spherical particles in the transition region

Near Infrared Absorption of Pure Carbon Dioxide up to 3100 bar and 500 K  II. Wavenumber Range 5600 cm- 1 to 7400 cm-1
Near Infrared Absorption of Pure Carbon Dioxide up to 3100 bar and 500 K II. Wavenumber Range 5600 cm- 1 to 7400 cm-1

On the Information Time Scale of Geophysical Records in Maximum Entropy  Spectral Analysis
On the Information Time Scale of Geophysical Records in Maximum Entropy Spectral Analysis

RADIATIVE TRANSFER IN AN INHOMOGENEOUS SPHERE
RADIATIVE TRANSFER IN AN INHOMOGENEOUS SPHERE

Journal of quantitative spectroscopy & radiative transfer - PUBDB
Journal of quantitative spectroscopy & radiative transfer - PUBDB

J. Quant. Spectrosc. Radiat. Transfer Vol. 47, No. 1, pp. 1-8, 1992  0022-4073]92 $5.00 + 0.00 Printed in Great Britain. All figh
J. Quant. Spectrosc. Radiat. Transfer Vol. 47, No. 1, pp. 1-8, 1992 0022-4073]92 $5.00 + 0.00 Printed in Great Britain. All figh

HITRANonline - Documentation: Units and definitions
HITRANonline - Documentation: Units and definitions