Measurements and empirical modeling of pure CO 2 absorption in the 2.3- m region at room temperature: far wings, allowed and collision-induced bands

Size: px
Start display at page:

Download "Measurements and empirical modeling of pure CO 2 absorption in the 2.3- m region at room temperature: far wings, allowed and collision-induced bands"

Transcription

1 Measurements and empirical modeling of pure CO 2 absorption in the 2.3- m region at room temperature: far wings, allowed and collision-induced bands M. V. Tonkov, N. N. Filippov, V. V. Bertsev, J. P. Bouanich, Nguyen Van-Thanh, C. Brodbeck, J. M. Hartmann, C. Boulet, F. Thibault, and R. Le Doucen Measurements of pure CO 2 absorption in the 2.3- m region are presented. The cm 1 range has been investigated at room temperature for pressures in the atm range by using long optical paths. Phenomena that contribute to absorption are listed and analyzed, including the contribution of far line wings as well as those of the central region of both allowed and collision-induced absorption bands. The presence of simultaneous transitions is also discussed. Simple and practical approaches are proposed for the modeling of absorption, which include a line-shape correction factor that extends to approximately 600 cm 1 from line centers. Key words: CO 2 infrared spectra, induced band, far wings Optical Society of America 1. Introduction The anomalous brightness of the nightside of Venus in the atmospheric window near 2.3 m is well known. 1,2 Radiation in this spectral region originates from low altitude layers and is due mostly to CO 2, which is the major constituent of the atmosphere. Its intensity is strongly underestimated by computations made with Lorentzian line shapes. Unfortunately, the mechanisms involved in radiation absorption emission in this spectral range are not clear and result from several phenomena. These in- M. V. Tonkov, N. N. Filippov, and V. V. Bertsev are with the Institute of Physics, St. Petersburg University, Peterhof, St. Petersburg, Russian Federation. J. P. Bouanich, N. Van- Thanh, C. Brodbeck, J. M. Hartmann, and C. Boulet are with the Laboratoire de Physique Moléculaire et Applications, Laboratoire associé aux Universités de Paris-Sud et Pierre et Marie Curie, Centre National de la Recherche Scientifique, Unité Propre de Recherche 136, Université Paris-Sud, Campus d Orsay, Bâtiment 350, Orsay cedex, France. F. Thibault and R. Le Doucen are with the Département de Physique Atomique et Moléculaire, Centre National de la Recherche Scientifique, Unité de Recherche Associée 1203, Université de Rennes I, Campus de Beaulieu, Rennes cedex, France. Received 22 May 1995; revised manuscript received 2 February $ Optical Society of America clude the breakdown of the Lorentz shape in the line wings, absorption by weak overtone and hot allowed dipolar transitions of CO 2, as well as significant contributions of collision-induced absorption. Because of the large amount of computational time required by remote-sensing spectra inversion, simple approaches must be used for the modeling of absorption. We present a study of the different processes that contribute to absorption by pure CO 2 in the 2.3- m region when large absorber amounts are considered. The CO 2 spectrum in this region has a great absorption coefficient variation approximately 4 orders of magnitude and results from various types of spectral feature allowed and induced bands, band wings that have to be studied with various resolutions. It was therefore necessary to combine the efforts of different research groups having a variety of experimental setups. The absorption by relatively small path lengths was measured in Orsay, the allowed bands in the cm 1 region were studied in Rennes, and the weak bands in the cm 1 region were investigated using the multipass cell in St. Petersburg. We present the synthesis of all the experiments conducted by these groups and we provide data on absorption by pure CO 2 in the cm 1 range. The measurements were done at room temperature by using long optical paths and high pressures, raising the effective gas abundance to 10 km 20 August 1996 Vol. 35, No. 24 APPLIED OPTICS 4863

2 Table 1. Experimental Apparatus Group Apparatus St. Petersburg Rennes Orsay Spectrometer Grating at first order Fourier transform Fourier transform Grating at first order Bruker HR120 Bruker IFS 66V Ge low-pass filter cm 1 filter No filter Ge low-pass filter 3.0-cm 1 resolution 0.1-cm 1 resolution 0.5-cm 1 resolution 4.0-cm 1 resolution Source Halogen tungsten lamp Halogen tungsten lamp Glow bar Glow bar Detector Room temperature PbS Liquid nitrogen InSb Liquid nitrogen InSb Liquid nitrogen InSb Cell 4-m-long multipass 2-m-long multipass 3-m-long single pass 7-cm-long single pass m paths 120-m paths 3-m paths 7-cm paths Stainless steel Stainless steel Stainless steel Titanium CaF 2 windows CaF 2 windows Sapphire windows Sapphire windows Temperatures Stabilized 1 K Stabilized 0.5 K Stabilized 1 K Stabilized 1 K K range 297-K range K range 292-K Pressures Bourdon manometer Bourdon and transducer Piezoresistive transducer Sedeme transducer 0.1-atm precision 0.1-atm precision 0.3-atm precision 0.1-atm precision atm range 1 22-atm range atm range atm range Studied region cm cm cm cm 1 atm. The contributions of far wings of the 1 3 band as well as those of bands centered within the studied wave-number range are analyzed. It is shown that absorption results from the usual allowed bands as well as collision-induced vibrational transitions including a simultaneous transition. Simple empirical approaches are proposed to model the different contributions to the spectra. It is shown that the central region of allowed bands can be computed by using spectroscopic data from databases 3,4 or using molecular constants from Ref. 5. Integrated band intensities are measured from the present data and a simple band-shape model was used for collision-induced contributions. Finally, we propose an empirical correction to the Lorentz line shape that enables computation of line wings to approximately 600 cm 1 from line center. The remainder of the paper is divided into two parts. In Section 2 we describe the experimental details and data reduction procedures. In Section 3 we have organized the presentation of data into three parts devoted, respectively, to contributions of farwing line shape, allowed transitions located in the spectral region, and collision-induced bands. 2. Experiments A. Setups and Data Analysis Measurements of pure CO 2 absorption in the 2.3- m region have been made by three different groups using a variety of experimental setups. The main characteristics of the apparatus are described in Table 1. The data of different sources were used in the spectral shape analysis of various regions. The studies of the 1 3 band wing shape in the cm 1 region were based mainly on the Orsay data. The allowed bands centered between 3950 and 4050 cm 1 were studied using the Rennes data obtained at higher resolution. The weak bands within the cm 1 range were registered by the St. Petersburg group since the other measurements in this region were invalid because of the too weak absorption for the path lengths used. Purity of the CO 2 gas used is important because the effective gas content reached 10 km atm. The gas used in Orsay was supplied by Alphagaz with a stated purity of %. In the Rennes experiments the gas was supplied by Prodair Airproducts with a stated purity of %. In both cases, the main impurities a few ppm 10 6 were water and hydrocarbons C n H m. The most difficult experiment was done with a density of 20.1 amagats in the St. Petersburg multipass cell with an optical path length of 482 m. Since traces of CO, CH 4,H 2 O, and N 2 O were detected in the original gas sample, an additional gas purification was performed by using chemical KOH, P 2 O 5 and physical from a gas-mask capsule absorbants. Unfortunately, we are not sure that the traces of N 2 O were removed completely since the 2 3 band of N 2 O and the band of CO 2 are located in the same frequency range and have a similar shape. The other impurities were absent from the spectrum after three days of purification. In all cases the absorption coefficient, n CO2 at wave number and CO 2 density n CO2 was obtained from two experiments, i.e.,, n CO2 1 d ln I, n CO 2 I, 0, (1) where d is the path length and I, n CO2 and I, 0 are the intensities that were measured with the gas sample and an empty cell, respectively. The density of CO 2 in amagats 1 amagat mol cm 3 was deduced from the measured temperature and pressure of the gas sample by using the data of Ref. 6. B. Data Intercomparisons and Checks Since data on CO 2 absorption was provided by various groups, intercomparisons between the different 4864 APPLIED OPTICS Vol. 35, No August 1996

3 Fig. 1. Experimental room temperature pure CO 2 absorption coefficients for a density of 20 amagats: curve, Rennes spectrum; E, St. Petersburg spectrum. results enabled a test of experimental procedures. This was done in two ways. When measurements had been made under the same conditions, n CO2 by different groups, direct comparison of absorption coefficients was possible. An example is plotted in Fig. 1 where spectra recorded in St. Petersburg and Rennes are compared. The agreement is satisfactory in the range in which absorption coefficients were measured with precision. In spectral regions that are sufficiently far away from allowed bands of significant contribution, the absorption results from far wings and collision-induced transitions. It is thus proportional to the square of the CO 2 density. In these regions, one can extract the normalized absorption coefficient B 0 cm 1 amagat 2 : B 0 1 n CO2 2, n CO 2. (2) This quantity enables comparison of experimental results obtained for different densities. The plot of Fig. 2 demonstrates the consistency of the experiments. Fig. 3. Experimental room temperature pure CO 2 absorption coefficient for a density of 20 amagats showing some of the contributions: a, far wing; b, allowed bands; c, collision-induced absorption bands. 3. Analysis of Absorption Figure 3 presents a typical spectrum in the cm 1 range. The different contributions to absorption that can be seen clearly are the following: a The smooth baseline is due mainly to the far wings of the intense C 16 O 2 band that is centered on the low-frequency side of the considered spectral range. This contribution increases with the square of the CO 2 density. Features that stick out from this baseline are due to local absorption transitions that are of different types, distinguishable through their dependences on density. b Dipole allowed absorption bands whose integrated intensities increase linearly with density; the structure centered near 4020 cm 1, for example, corresponds to the R branch of the band of 12 C 16 O 2. c Collision-induced absorption bands whose magnitudes increase as the square of density; the band centered near 4063 cm 1 was observed previously 7,8 and corresponds to the 12 C 16 O II vibrational transition. These different contributions to the overall absorption coefficient are analyzed and modeled hereafter. A. Far-Wing Contributions It is well known that absorption by far wings of CO 2 absorption lines is strongly sub-lorentzian. 7 This behavior results from the combined influences of line mixing and finite duration of collision. 9,10 Theoretical approaches for direct computations 9 12 require significant computer time, and their accuracies are still insufficient for practical applications. Since the latter require precise, low computer cost, and easy to implement modeling of line-wing absorption, empirical corrections to the Lorentz shape are generally used; the absorption coefficient for pure CO 2 can then be written as Fig. 2. Experimental room temperature pure CO 2 normalized absorption coefficients: }, Orsay-2 values; curve, Orsay-1 values; F, St. Petersburg values;, values from Burch et al. 7 S wing 2, T, n CO2 n CO2 s l l lines l l l T, l. 2 (3) 20 August 1996 Vol. 35, No. 24 APPLIED OPTICS 4865

4 Fig. 4. Room temperature pure CO 2 absorption coefficients for a density of 20 amagats: E, experimental values; computed values accounting for allowed HITRAN-92 and induced transitions with the factor from dashed curve, Ref m region ; solid curve, Ref m region. Fig. 5. Room temperature pure CO 2 absorption coefficients for a density of 20 amagats: E, experimental values; solid curve, computed values accounting for allowed and induced transitions with the factor of Table 2; dashed curve, computed contribution of the far wings of the 1 3 band. The spectroscopic data l, S l, s l, which are the position, intensity, and self-broadening coefficient of line l, were taken from the HITRAN-92 database. 3 The line-shape correction factor is considered independent of the transition but depends on both temperature and collision partner CO 2 in the present case. A large set of factors has been proposed for pure CO 2 line wings. 7,13 18 Except for the research of Burch et al. 7 who have investigated various spectral regions, all the other studies refer to the 3 band. On the other hand, the only factor for pure CO 2 and temperatures in the K range is, to our knowledge, that of Ref. 13, which was deduced from measurements beyond the 3 bandhead. In Fig. 4 we plotted a comparison between the present experimental results and predictions using the factors of Refs. 7 and 13. The methods that were used to account for allowed and induced bands are discussed below. Figure 4 shows that line-wing contributions are underestimated when we use a factor adapted to the 4- m region 13 ; this is consistent with the results of Figs. 13 and 14 of Ref. 7, which indicate that line wings in the 3 band are more sub- Lorentzian than those of the 1 3 band. The agreement obtained with Burch s factor 7 is much better although absorption in the far wing seems slightly overestimated. To correct some of the discrepancies we have derived a new factor, which is described in Table 2, for the 2.3- m spectral region. The accuracy of the fit is shown in Fig. 5. These computations show that Table 2. Parameters of the Factor Fitted from the Current Experiments T 296 K cm exp exp exp most of the far-wing contributions in the cm 1 region result from lines of the 1 3 I,II bands that are centered 3,5 near 3700 and 3600 cm 1. The factor deduced from the present experiments thus extends to approximately 600 cm 1 from line centers. We emphasize that this factor is empirical and it probably corrects for a number of small local contributions weak allowed bands, collision-induced absorption, simultaneous transitions, dimers,... that have not been accounted for in the computations. B. Allowed Bands Located in the Spectral Region Molecular spectroscopic databases 3,4 provide spectroscopic information on the lines centered in this wavenumber range whereas Ref. 5 describes the main bands. Because of the moderate densities involved by the present experiments, use of the modified Lorentzian shape of Ref. 19 generally enables accurate prediction of absorption coefficients in the central region of absorption bands. The prediction is more questionable for Q-branches in which line-mixing effects are significant due to the small spacing between lines; nevertheless such regions are quite narrow and errors in the computations have little consequences, considering the aim of this study. We have thus computed the absorption coefficients by using the following expression: 1 n Lor CO2 S l T n cor, n CO2 lines s CO2 l T l l 2 n s CO2 l T 2 cor l, n CO2. (4) The spectroscopic data l, S l, s l, which are the position, intensity, and self-broadening coefficient of line l, were again taken from the HITRAN-92 database. 3 The correction function cor was computed following Ref. 19 by using the corrective factor of Table 2. Note that cor is equal to the sub-lorentzian factor in the far wing but the intensity removed from the wing is transferred to the central part of each line 4866 APPLIED OPTICS Vol. 35, No August 1996

5 Fig. 6. Room temperature pure CO 2 absorption coefficients for a density of amagats: solid curve, experimental absorption Rennes data corrected for far wings difference between the experimental data and that calculated according to Eq. 3. Computed contributions of local allowed transitions: dot dash curve, HITRAN-92 database; dashed curve, HITRAN-95 database. Fig. 7. Room temperature pure CO 2 absorption coefficients for a density of 20 amagats: F, experimental values; solid curve, computed values accounting for allowed and induced transitions with the optimized factor of Table 2 and the HITEMP database; dashed curve, computed contribution of the far wings of allowed bands centered outside the considered spectral region. The lower plot gives the relative difference between observed and computed spectra. such that the line intensity is conserved. Nevertheless, at the considered density, the Lorentzian shape is quite accurate and corrections remain small see, for example, Ref. 20. When compared with experimental values corrected from far-wing and collision-induced contributions the computed absorption by local allowed transitions is in reasonable agreement with experiment with few exceptions. For example, HITRAN-92 does not enable correct modeling of absorption in the band near 4005 cm 1 probably owing to an error in the Herman Wallis factor. Therefore, thanks to L. Rothman, this part of the database has been replaced by the 1995 HITRAN version that will soon be available, leading to a reasonable agreement with experiment as it appears from Fig. 6. Similarly, the 2 3 band of 16 O 13 C 18 O centered 5 near 4508 cm 1, which is not given in the HITRAN-92 database because of its intensity cutoff, is responsible for some of the observed discrepancy: In order to test the completeness of the HITRAN-92 base for local allowed transitions for the large absorber amounts considered here, we have compared the allowed contributions in the cm 1 region computed with HITRAN-92 and with the HITEMP database. This calculation has been made by Bezard and Drossard within the framework of Ref. 2. Comparison of Figs. 5 and 7 shows that the differences can be significant, as has already been shown in Ref. 2 the arrow in Fig. 7 corresponds to the center of the 2 3 band of 16 O 13 C 18 O. The remaining discrepancies, restricted to the cm 1 spectral region, are due mainly to incorrect modeling of the collision-induced absorption missing bands, wrong shape in the wings of these bands and the far-wing contributions of the I,II,III bands centered beyond 4800 cm 1 as well as neglecting other contributions such as simultaneous transitions. C. Collision-Induced Bands Collision-induced absorption bands of CO 2 in the near IR have been observed previously. 7,8,21 23 In this study the main bands have been identified by their increasing intensity with squared density, elimination of allowed bands, and knowledge of the energies of CO 2 vibrational levels. 5 Their integrated intensities have been estimated by integration of the absorption coefficient after corrections for the baseline that is due to line wings and subtraction of allowed bands. The results obtained, which are given in Table 3, have large uncertainties and should be considered with great caution. Unfortunately, there is, to our knowledge, a lack of data for the intensities of these bands. Table 3 also lists the band centers that are compared with the theoretical predictions deduced from Ref. 5. The calculated transition frequencies for CO 2 are in good accordance with measured ones with one exception: The feature near 4280 cm 1 shows a quadratic dependence on density and thus should be treated as an induced band. It was detected at Table 3. Observed Collision-Induced Bands: Estimated Band Centers and Intensities Upper Level of Vibrational Transitions Calculated Frequency cm 1 Measured Frequency cm 1 Measured Intensity 10 6 cm 2 amagat III II I a II a II I I I I I a The assignment of weak observed structures is doubtful. 20 August 1996 Vol. 35, No. 24 APPLIED OPTICS 4867

6 higher densities both by the St. Petersburg team and in Orsay, but its wave-number center 4278 cm 1 does not coincide with any possible collision-induced transition from the ground state. However, its central wave number is close to that associated with the double transition 1 a I and 2 3 b in molecules a and b at cm 1. The appearance of the Fermi dyad 1 a I,II 2 3 b can be used to explain the great difference in intensities of the components at 4250 and 4383 cm 1 : the observed band at 4383 cm 1 corresponds to the superposition of single and double transitions. This interpretation can be confirmed by the absence of the two bands at 4278 and 4383 cm 1 in the spectra of high density CO 2 Ar mixtures measured in Orsay. For practical applications, modeling of the shape of near-infrared collision absorption bands is required. Introducing the spectral density function the collision-induced absorption CIA coefficient is given by Fig. 8. Optimized normalized spectral density n for the collisioninduced bands as a function of the detuning wave number from the band center. 1 exp hc k CIA, n CO2 n 2 b T CO2 S band T band, T, (5) band 1 exp hc k b T band, T d where S band T is the band intensity, band is the band center see Table 3, and the integral expands over the whole region of significant absorption. In the absence of a simple theoretical model for the computation of the spectral density function, band, T has been obtained using the following procedure: It was first assumed that the normalized line shape is independent of the type of induced vibrational band. This hypothesis seems acceptable for g g bands but is probably less appropriate for g g bands with significantly different structures. Then the central part of 40 cm 1 was deduced from the current observed values of the collision-induced band located around 4063 cm 1. The wings 40 cm 1 were obtained by a shape derived from previous experiments made in the far-infrared region for the pure collision-induced rotational band, 24,25 which is free of any contamination by contributions of allowed transitions. The resulting density function is plotted in Fig. 8. A test of the current approach i.e., Eq. 5, Table 3, and Fig. 8 is presented in Fig. 9. Although the computation accounts for the main features, significant discrepancies remain. They may result from a number of approximations that include large uncertainties on the intensities and shapes that were used for modeling collision-induced absorption. Furthermore it is clear that a number of weak absorption contributions have not been taken into account. For example, the feature indicated by an arrow in Fig. 9 at 4430 cm 1 has to be attributed to an allowed transition because of its density dependence. Its origin is not clear. The rather strong CO 2 band 3 is in this region. However, this explanation remains doubtful since the strong 2 3 band of N 2 O, which may be present as impurity in our samples, is also in this region. Computations with the HITRAN-92 database 3 enabled estimation of the N 2 O amount 0.05% and removal of this absorption. Finally Fig. 10 gives a global idea of the quality of the optimized fit obtained in the spectral region Fig. 9. Room temperature pure CO 2 absorption coefficients for a density of 20 amagats: E, experimental values corrected for local allowed transitions with the HITRAN-92 database; dashed curve, computed contribution of local collision-induced transitions; solid curve, experimental absorption corrected for local allowed and collision-induced transitions difference between the previous two APPLIED OPTICS Vol. 35, No August 1996

7 available part of the 1995 version of HITRAN for CO 2 prior to publication. Fig. 10. Room temperature pure CO 2 absorption coefficients for a density of 20 amagats. Ratio of the experimental to computed absorption with the HITRAN-92 database including all the mechanisms and the optimized factor of Table 2. where the use of the HITRAN-92 database is valid. This fit can be considered reasonable. 4. Conclusion Measurements and analysis of the processes that contribute to radiation absorption in the cm 1 spectral range have been presented. Empirical modelings of the contributions of collision-induced bands and far line wings have been proposed that enable satisfactory agreement with experiments in the cm 1 range at room temperature. Remaining discrepancies result from weak absorption processes allowed, collision-induced bands, simultaneous transitions that have not been accounted for. Nevertheless, the empirical line-shape correction function proposed enables correct modeling of spectra, accounting for line-wing contributions to approximately 600 cm 1 from line centers. This study has been limited to room temperature, whereas modeling of spectra resulting from the deep atmosphere of Venus requires knowledge of the farwing line-shape dependence with temperature in the K range. As high temperature and long path-length measurements are hardly feasible in the laboratories, the following method may be considered: Taking into account recent progress in the theory of far-wing absorption, 9,12,26 29 the calculation of the far-wing line shape for the CO 2 CO 2 system can be developed and compared with an experimental factor at room temperature. Since the formalism can reasonably be used to predict the temperature dependence of the far-wing absorption for various other systems, 12,27 29 it can also be used in a second step to derive the temperature dependence of the factor for CO 2 CO 2. The authors are grateful to P. Drossart and B. Bézard from Observatoire de Meudon for communicating the results they obtained with the HITEMP database. They also thank L. Rothman who made References 1. B. Bézard, C. de Berg, D. Crisp, and J. P. Maillard, The deep atmosphere of Venus revealed by high-resolution nightside spectra, Nature London 345, J. B. Pollack, J. B. Dalton, D. Grinspoon, R. B. Wattson, R. Freedman, D. Crisp, D. A. Allen, B. Bézard, C. de Berg, L. P. Giver, Q. Ma, and R. H. Tipping, Near-infrared light from Venus nightside: a spectroscopic analysis, Icarus 103, L. S. Rothman, R. R. Gamache, R. H. Tipping, C. P. Rinsland, M. A. H. Smith, D. C. Benner, V. Malathy Devi, J. M. Flaud, C. Camy-Peyret, A. Perrin, A. Goldman, S. T. Massie, L. R. Brown, and R. A. Toth, The HITRAN molecular database: editions of 1991 and 1992, J. Quant. Spectrosc. Radiat. Transfer 48, N. Husson, B. Bonnet, A. Chédin, N. A. Scott, A. A. Chursin, V. F. Golovko, and Vl. G. Tyuterev, The GEISA data bank in 1993: A PC AT compatible computers new version, J. Quant. Spectrosc. Radiat. Transfer 52, L. S. Rothman, R. L. Hawkins, R. B. Wattson, and R. R. Gamache, Energy level, intensities, and linewidths of atmospheric carbon dioxide bands, J. Quant. Spectrosc. Radiat. Transfer 48, ; L. S. Rothman, Infrared energy levels and intensities of carbon dioxide. Part 3, Appl. Opt. 25, S. Angus, B. Armstrong, and K. M. de Reuck, International Thermodynamic Tables of the Fluid State: Carbon Dioxide Pergamon, Oxford, D. E. Burch, D. A. Gryvnak, R. R. Patty, and C. E. Bartky, Shapes of collision-broadened CO 2 lines, J. Opt. Soc. Am. 59, T. G. Adiks, Absorption spectrum of CO 2 in the m region under conditions of high pressure and CO 2 content, Opt. Spectrosc. 40, C. Boulet, J. Boissoles, and D. Robert, Collisionally-induced population transfer effect in infrared absorption spectra. I. A line-by-line coupling theory from resonances to the far wings, J. Chem. Phys. 89, J. M. Hartmann and C. Boulet, Line mixing and finite duration of collision effects in pure CO 2 infrared spectra: fitting and scaling analysis, J. Chem. Phys. 94, J. Boissoles, V. Menoux, R. Le Doucen, C. Boulet, and D. Robert, Collisionally-induced population transfer effect in infrared absorption spectra. II. The wing of the Ar-broadened 2 band of CO 2, J. Chem. Phys. 91, J. Boissoles, C. Boulet, J. M. Hartmann, M. Y. Perrin, and D. Robert, Collision-induced population transfer in infrared absorption spectra. III. Temperature dependence of absorption in the Ar-broadened wing of CO 2 3 band, J. Chem. Phys. 93, M. Y. Perrin and J. M. Hartmann, Temperature-dependent measurements and modeling of absorption by CO 2 N 2 mixtures in the far line-wing of the 4.3 m CO 2 band, J. Quant. Spectrosc. Radiat. Transfer 42, B. H. Winters, S. Silverman, and W. S. Benedict, Line shape in the wing beyond the band-head of the 4.3 m band of CO 2, J. Quant. Spectrosc. Radiat. Transfer 4, M. W. P. Cann, R. W. Nicholls, P. L. Roney, A. Blanchard, and F. D. Findlay, Spectral line shapes for carbon dioxide in the 4.3- m band, Appl. Opt. 24, R. Le Doucen, C. Cousin, C. Boulet, and A. Henry, Temperature dependence of the absorption in the region beyond the 20 August 1996 Vol. 35, No. 24 APPLIED OPTICS 4869

8 4.3- m band head of CO 2. 1: Pure CO 2 case, Appl. Opt. 24, V. Menoux, R. Le Doucen, and C. Boulet, Line shape in the low-frequency wing of self-broadened CO 2 lines, Appl. Opt. 26, J. M. Hartmann and M. Y. Perrin, Measurements of pure CO 2 absorption beyond the 3 bandhead at high temperature, Appl. Opt. 28, J. M. Hartmann, J. P. Bouanich, C. Boulet, and M. Sergent, Absorption of radiation by gases from low to high pressures. I. Empirical line-by-line and narrow-band statistical models, J. Phys. II Paris 1, M. Fukabori, T. Nakazawa, and M. Tanaka, Absorption properties of infrared active gases at high pressures-i. CO 2, J. Quant. Spectrosc. Radiat. Transfer 36, T. G. Adiks, Influence of the state of aggregation of CO 2 on the intensities of allowed and induced absorption bands in the 1 4 m region, Opt. Spectrosc. 44, N. I. Moskalenko, Yu. A. Il in, S. N. Parzhin, and L. V. Rodionov, Pressure-induced IR radiation absorption in atmospheres, Atmos. Ocean Phys. 15, M. E. Thomas and M. J. Linevsky, Integrated intensities of N 2,CO 2, and SF 6 vibrational bands from 1800 to 5000 cm 1 as a function of density and temperature, J. Quant. Spectrosc. Radiat. Transfer 42, W. Ho, G. Birnbaum, and A. Rosenberg, Far-infrared collision induced absorption in CO 2. I. Temperature dependence, J. Chem. Phys. 55, G. Birnbaum, W. Ho, and A. Rosenberg, Far-infrared collision induced absorption in CO 2. II. Pressure dependence in the gas phase and absorption in the liquid, J. Chem. Phys. 55, P. W. Rosenkranz, Pressure broadening of rotational bands II. Water vapor from 300 to 1100 cm 1, J. Chem. Phys. 87, Q. Ma and R. H. Tipping, The atmospheric water continuum in the infrared: extension of the statistical theory of Rosenkranz, J. Chem. Phys. 93, Q. Ma and R. H. Tipping, A far wing lineshape theory and its application to the water continuum in the infrared region I, J. Chem. Phys. 95, Q. Ma and R. H. Tipping, A far wing lineshape theory and its application to the foreign broadened water continuum absorption III, J. Chem. Phys. 97, APPLIED OPTICS Vol. 35, No August 1996

Comment on Radiative transfer in CO 2 -rich atmospheres: 1. Collisional line mixing implies a colder early Mars

Comment on Radiative transfer in CO 2 -rich atmospheres: 1. Collisional line mixing implies a colder early Mars Comment on Radiative transfer in CO 2 -rich atmospheres: 1. Collisional line mixing implies a colder early Mars M. Turbet and H. Tran Laboratoire de Météorologie Dynamique, IPSL, UPMC Univ Paris 06, Ecole

More information

Moderate Spectral Resolution Radiative Transfer Modeling Based on Modified Correlated-k Method

Moderate Spectral Resolution Radiative Transfer Modeling Based on Modified Correlated-k Method Moderate Spectral Resolution Radiative Transfer Modeling Based on Modified Correlated-k Method S. Yang, P. J. Ricchiazzi, and C. Gautier University of California, Santa Barbara Santa Barbara, California

More information

DIODE- AND DIFFERENCE-FREQUENCY LASER STUDIES OF ATMOSPHERIC MOLECULES IN THE NEAR- AND MID-INFRARED: H2O, NH3, and NO2

DIODE- AND DIFFERENCE-FREQUENCY LASER STUDIES OF ATMOSPHERIC MOLECULES IN THE NEAR- AND MID-INFRARED: H2O, NH3, and NO2 DIODE- AND DIFFERENCE-FREQUENCY LASER STUDIES OF ATMOSPHERIC MOLECULES IN THE NEAR- AND MID-INFRARED: H2O, NH3, and NO2 Johannes ORPHAL, Pascale CHELIN, Nofal IBRAHIM, and Pierre-Marie FLAUD Laboratoire

More information

N. Jacquinet-Husson, R. Armante, T. Langlois, N.A. Scott, A. Chédin

N. Jacquinet-Husson, R. Armante, T. Langlois, N.A. Scott, A. Chédin N. Jacquinet-Husson, R. Armante, T. Langlois, N.A. Scott, A. Chédin Laboratoire de Météorologie Dynamique Atmospheric Radiation Analysis Group Ecole Polytechnique 91128, Palaiseau, France http://ara.lmd.polytechnique.fr

More information

The Smithsonian Astrophysical Observatory Database SAO92

The Smithsonian Astrophysical Observatory Database SAO92 The Smithsonian Astrophysical Observatory Database SAO92 K. Chance, K. W. Jucks, D. G. Johnson, and W. A. Traub Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, USA ABSTRACT The Smithsonian

More information

Line Intensities in the ν 6 Fundamental Band of CH 3 Br at 10 µm

Line Intensities in the ν 6 Fundamental Band of CH 3 Br at 10 µm Journal of Molecular Spectroscopy 216, 30 47 (2002) doi:10.1006/jmsp.2002.8640 Line Intensities in the ν 6 Fundamental Band of CH 3 Br at 10 µm E. Brunetaud, I. Kleiner, and N. Lacome Laboratoire de Dynamique,

More information

Medium resolution transmission measurements of water vapor at high temperature

Medium resolution transmission measurements of water vapor at high temperature Medium resolution transmission measurements of water vapor at high temperature Sudarshan P. Bharadwaj, Michael F. Modest and Robert J. Riazzi Department of Mechanical and Nuclear Engineering The Pennsylvania

More information

Linda R. Brown. Jet Propulsion Laboratory California Institute of Technology Pasadena, CA

Linda R. Brown. Jet Propulsion Laboratory California Institute of Technology Pasadena, CA Infrared Laboratory Spectroscopy. of CH4 and CH3D for Atmospheric Studies Linda R. Brown Jet Propulsion Laboratory California Institute of Technology Pasadena, CA 91109 linda.brown@jpl.nasa.gov The part

More information

Icarus. The and 1.18-lm nightside windows of Venus observed by SPICAV-IR aboard Venus Express

Icarus. The and 1.18-lm nightside windows of Venus observed by SPICAV-IR aboard Venus Express Icarus 216 (211) 173 183 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus The 1.1- and 1.18-lm nightside windows of Venus observed by SPICAV-IR

More information

Hefei

Hefei 2017 3rd International Conference on Computer Science and Mechanical Automation (CSMA 2017) ISBN: 978-1-60595-506-3 Experimental Study of Broadening Coefficients for the v3 Band of CO by Tunable Diode

More information

Recent spectroscopy updates to the line-by-line radiative transfer model LBLRTM evaluated using IASI case studies

Recent spectroscopy updates to the line-by-line radiative transfer model LBLRTM evaluated using IASI case studies Recent spectroscopy updates to the line-by-line radiative transfer model LBLRTM evaluated using IASI case studies M.J. Alvarado 1, V.H. Payne 2, E.J. Mlawer 1, J.-L. Moncet 1, M.W. Shephard 3, K.E. Cady-Pereira

More information

MULTISPECTRUM ANALYSIS OF THE OXYGEN A-BAND

MULTISPECTRUM ANALYSIS OF THE OXYGEN A-BAND MULTISPECTRUM ANALYSIS OF THE OXYGEN A-BAND BRIAN J. DROUIN, LINDA R. BROWN, MATTHEW J. CICH, TIMOTHY J. CRAWFORD, ALEXANDER GUILLAUME, FABIANO OYAFUSO, VIVIENNE PAYNE, KEEYOON SUNG, SHANSHAN YU, JET PROPULSION

More information

Impact of different spectroscopic datasets on CH 4 retrievals from Jungfraujoch FTIR spectra

Impact of different spectroscopic datasets on CH 4 retrievals from Jungfraujoch FTIR spectra Impact of different spectroscopic datasets on CH 4 retrievals from Jungfraujoch FTIR spectra P. Duchatelet (1), E. Mahieu (1), P. Demoulin (1), C. Frankenberg (2), F. Hase (3), J. Notholt (4), K. Petersen

More information

FIRST HIGH-RESOLUTION ANALYSIS OF PHOSGENE 35 Cl 2. CO AND 35 Cl 37 ClCO FUNDAMENTALS IN THE CM -1 SPECTRAL REGION

FIRST HIGH-RESOLUTION ANALYSIS OF PHOSGENE 35 Cl 2. CO AND 35 Cl 37 ClCO FUNDAMENTALS IN THE CM -1 SPECTRAL REGION FIRST HIGH-RESOLUTION ANALYSIS OF PHOSGENE 35 Cl 2 CO AND 35 Cl 37 ClCO FUNDAMENTALS IN THE 250-480 CM -1 SPECTRAL REGION F. Kwabia Tchana 1, M. Ndao 1, L. Manceron 2, A. Perrin 1, J. M. Flaud 1, W.J.

More information

DEVELOPMENT OF A NEW RADIATION SCHEME FOR THE GLOBAL ATMOSPHERIC NWP MODEL

DEVELOPMENT OF A NEW RADIATION SCHEME FOR THE GLOBAL ATMOSPHERIC NWP MODEL P1.66 DEVELOPMENT O A NEW RADIATION SCHEME OR THE GLOBAL ATMOSPHERIC NWP MODEL Shigeki MURAI, Syoukichi YABU and Hiroto ITAGAWA Japan Meteorological Agency, Tokyo, JAPAN 1 INTRODUCTION A radiation scheme

More information

A tool for IASI hyperspectral remote sensing applications: The GEISA/IASI database in its latest edition

A tool for IASI hyperspectral remote sensing applications: The GEISA/IASI database in its latest edition A tool for IASI hyperspectral remote sensing applications: The GEISA/IASI database in its latest edition N. Jacquinet-Husson, C. Boutammine, R. Armante, L.Crépeau, A. Chédin, N.A. Scott, C. Crevoisier,

More information

Line shape modeling and application to remote sensing

Line shape modeling and application to remote sensing Line shape modeling and application to remote sensing Dr. Ha Tran Senior Researcher at CNRS, Paris, France Laboratoire de Météorologie Dynamique Sorbonne Université, Ecole Polytechnique, Ecole Normale

More information

In situ combustion measurements of CO 2 by use of a distributed-feedback diode-laser sensor near 2.0 m

In situ combustion measurements of CO 2 by use of a distributed-feedback diode-laser sensor near 2.0 m In situ combustion measurements of CO 2 by use of a distributed-feedback diode-laser sensor near 2.0 m Michael E. Webber, Suhong Kim, Scott T. Sanders, Douglas S. Baer, Ronald K. Hanson, and Yuji Ikeda

More information

Infrared quantitative spectroscopy and atmospheric satellite measurements

Infrared quantitative spectroscopy and atmospheric satellite measurements Infrared quantitative spectroscopy and atmospheric satellite measurements Jean-Marie Flaud Laboratoire Interuniversitaire des Systèmes Atmosphériques CNRS, Universités Paris Est Créteil et Paris Diderot

More information

Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A.

Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Laboratoire de Météorologie Dynamique Atmospheric Radiation Analysis Group Ecole Polytechnique 91128, Palaiseau, France http://ara.lmd.polytechnique.fr

More information

ASSESSMENT OF THE GEISA AND GEISA/IASI SPECTROSCOPIC DATA QUALITY: trough comparisons with other public database archives

ASSESSMENT OF THE GEISA AND GEISA/IASI SPECTROSCOPIC DATA QUALITY: trough comparisons with other public database archives ASSESSMENT OF THE GEISA AND GEISA/IASI SPECTROSCOPIC DATA QUALITY: trough comparisons with other public database archives N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante Laboratoire de Météorologie

More information

MEASUREMENT AND MODELING OF OH, NO, AND CO 2 INFRARED RADIATION IN A LOW TEMPERATURE AIR PLASMA

MEASUREMENT AND MODELING OF OH, NO, AND CO 2 INFRARED RADIATION IN A LOW TEMPERATURE AIR PLASMA MEASUREMENT AND MODELING OF OH, NO, AND CO 2 INFRARED RADIATION IN A LOW TEMPERATURE AIR PLASMA Denis M. Packan, * Richard J. Gessman, * Laurent Pierrot, Christophe O. Laux, and Charles H. Kruger Department

More information

Impact of Spectroscopic Parameter Archive on Second Generation Vertical Sounders Radiance Simulation: the GEISA/IASI Database as an example

Impact of Spectroscopic Parameter Archive on Second Generation Vertical Sounders Radiance Simulation: the GEISA/IASI Database as an example Impact of Spectroscopic Parameter Archive on Second Generation Vertical Sounders Radiance Simulation: the GEISA/IASI Database as an example N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante et co-authors

More information

Detection of ozone for use as an extrasolar biosignature

Detection of ozone for use as an extrasolar biosignature Detection of ozone for use as an extrasolar biosignature Kristina Pistone ABSTRACT While it has previously been proposed that ozone could be a sign of life if detected in an extrasolar planetary atmosphere,

More information

Molecular spectroscopy, besides its own interest. Infrared Spectroscopy and the Atmosphere

Molecular spectroscopy, besides its own interest. Infrared Spectroscopy and the Atmosphere Gentner-Kastler-Preis Infrared Spectroscopy and the Atmosphere Measurements from space enable accurate monitoring of molecular abundances Jean-Marie Flaud In recent years, numerous studies concerning the

More information

Weak water absorption lines around and 1.66 lm by CW-CRDS

Weak water absorption lines around and 1.66 lm by CW-CRDS Journal of Molecular Spectroscopy 244 (2007) 170 178 www.elsevier.com/locate/jms Weak water absorption lines around 1.455 and 1.66 lm by CW-CRDS Semen N. Mikhailenko a, *, Wang Le b,c, Samir Kassi b, Alain

More information

Temperature-Dependent Line Shift and Broadening of CO Infrared Transitions

Temperature-Dependent Line Shift and Broadening of CO Infrared Transitions JOURNAL OF MOLECULAR SPECTROSCOPY 192, 268 276 (1998) ARTICLE NO. MS987694 Temperature-Dependent Line Shift and Broadening of CO Infrared Transitions T. Drascher,* T. F. Giesen,*,1 T. Y. Wang,* N. Schmücker,*

More information

Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A.

Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Laboratoire de Météorologie Dynamique Atmospheric Radiation Analysis Group Ecole Polytechnique 91128, Palaiseau, France http://ara.lmd.polytechnique.fr

More information

An assessment of the accuracy of the RTTOV fast radiative transfer model using IASI data

An assessment of the accuracy of the RTTOV fast radiative transfer model using IASI data An assessment of the accuracy of the RTTOV fast radiative transfer model using IASI data Marco Matricardi, Tony McNally ECMWF Reading, Berkshire, UK Abstract IASI measurements of spectral radiances made

More information

New analysis of the 3 & 4 bands of HNO 3 by high resolution Fourier transform spectroscopy in the 7.6 µm region

New analysis of the 3 & 4 bands of HNO 3 by high resolution Fourier transform spectroscopy in the 7.6 µm region New analysis of the 3 & 4 bands of HNO 3 by high resolution Fourier transform spectroscopy in the 7.6 µm region Agnés Perrin,, J.M.Flaud Laboratoire Interuniversitaire des Systémes Atmosphériques (LISA),

More information

HDO and D 2 O long path spectroscopy: Ongoing work of the Brussels-Reims Team.

HDO and D 2 O long path spectroscopy: Ongoing work of the Brussels-Reims Team. HDO and D 2 O long path spectroscopy: Ongoing work of the Brussels-Reims Team. Ludovic Daumont Groupe de Spectroscopie Moléculaire et Atmosphérique UMR CNRS 6089 Université de Reims Champagne Ardenne Reims,

More information

The Laboratory Measurement of Pressure Broadening Parameter for Atmospheric Remote Sensing

The Laboratory Measurement of Pressure Broadening Parameter for Atmospheric Remote Sensing The Laboratory Measurement of Pressure Broadening Parameter for Atmospheric Remote Sensing YAMADA Masumi, KASAI Yasuko, and AMANO Takayoshi The upcoming JEM/SMILES (Superconducting Submillimeter-wave Limb

More information

An Improved Version of the CO2 Line-mixing Database and Software: Update and Extension

An Improved Version of the CO2 Line-mixing Database and Software: Update and Extension An Improved Version of the CO2 Line-mixing Database and Software: Update and Extension ANNE L. LARAIA, JULIEN LAMOUROUX, ROBERT R. GAMACHE University of Massachusetts School of Marine Sciences, Department

More information

Updates to Spectroscopy for OCO-2

Updates to Spectroscopy for OCO-2 Updates to Spectroscopy for OCO-2 Vivienne Payne 1, Brian Drouin 1, Malathy Devi 2, Chris Benner 2, Fabiano Oyafuso 1, Linda Brown 1*, Thinh Bui 3, Matt Cich 1, David Crisp 1, Brendan Fisher 1, Iouli Gordon

More information

Pure water vapor continuum measurements between 3100 and 4400 cm 1 : Evidence for water dimer absorption in near atmospheric conditions

Pure water vapor continuum measurements between 3100 and 4400 cm 1 : Evidence for water dimer absorption in near atmospheric conditions Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L12808, doi:10.1029/2007gl029259, 2007 Pure water vapor continuum measurements between 3100 and 4400 cm 1 : Evidence for water dimer absorption

More information

Laboratory measurements of the water vapor continuum in the cm 1 region between 293 K and 351 K

Laboratory measurements of the water vapor continuum in the cm 1 region between 293 K and 351 K JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114,, doi:10.1029/2008jd011355, 2009 Laboratory measurements of the water vapor continuum in the 1200 8000 cm 1 region between 293 K and 351 K D. J. Paynter, 1,2 I.

More information

Absorption Line Physics

Absorption Line Physics Topics: 1. Absorption line shapes 2. Absorption line strength 3. Line-by-line models Absorption Line Physics Week 4: September 17-21 Reading: Liou 1.3, 4.2.3; Thomas 3.3,4.4,4.5 Absorption Line Shapes

More information

6 Terahertz-Wave Propagation Model

6 Terahertz-Wave Propagation Model 6 Terahertz-Wave Propagation Model 6-1 Atmospheric Propagation Model of Terahertz-Wave Knowledge of atmospheric propagation property of terahertz-wave is very important for terahertz technology and its

More information

Venus surface data extraction from VIRTIS/Venus Express measurements: Estimation of a quantitative approach

Venus surface data extraction from VIRTIS/Venus Express measurements: Estimation of a quantitative approach JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113,, doi:10.1029/2008je003087, 2008 Venus surface data extraction from VIRTIS/Venus Express measurements: Estimation of a quantitative approach Gabriele Arnold, 1,2

More information

Spectroscopic database GEISA-08 : content description and assessment through IASI/MetOp flight data

Spectroscopic database GEISA-08 : content description and assessment through IASI/MetOp flight data Spectroscopic database GEISA-08 : content description and assessment through IASI/MetOp flight data Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Laboratoire de Météorologie

More information

Infrared radiance modelling and assimilation

Infrared radiance modelling and assimilation Infrared radiance modelling and assimilation Marco Matricardi ECMWF Workshop on the Radiation in the Next Generation of Weather Forecast Models 21-24 May 2018 ECMWF - Reading - UK Radiative transfer models

More information

High-Resolution Survey of the Visible Spectrum of NiF by Fourier Transform Spectroscopy

High-Resolution Survey of the Visible Spectrum of NiF by Fourier Transform Spectroscopy Journal of Molecular Spectroscopy 214, 152 174 (2002) doi:10.1006/jmsp.2002.8567 High-Resolution Survey of the Visible Spectrum of NiF by Fourier Transform Spectroscopy Y. Krouti, T. Hirao,,1 C. Dufour,

More information

Water Pressure Broadening: A Never-ending Story

Water Pressure Broadening: A Never-ending Story Water Pressure Broadening: A Never-ending Story Georg Wagner, Manfred Birk DLR Remote Sensing Technology Institute, Oberpfaffenhofen, Germany Remote Sensing Technology Institute 1 Requirements Database

More information

N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante, K. Garceran, Th. Langlois.

N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante, K. Garceran, Th. Langlois. Assessing Spectroscopic Parameter Archives for the Second Generation Vertical Sounders Radiance Simulation: Illustration through the GEISA/IASI database N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante,

More information

Molecular spectroscopy for planetary and exoplanetary radiative transfer : The rock of Sisyphus or the barrel of the Danaids?

Molecular spectroscopy for planetary and exoplanetary radiative transfer : The rock of Sisyphus or the barrel of the Danaids? Molecular spectroscopy for planetary and exoplanetary radiative transfer : The rock of Sisyphus or the barrel of the Danaids? Pierre Drossart LESIA, Observatoire de Meudon Situation of molecular spectroscopy

More information

Stark profiles of infrared helium lines

Stark profiles of infrared helium lines ASTRONOMY & ASTROPHYSICS DECEMBER I 1998, PAGE 229 SUPPLEMENT SERIES Astron. Astrophys. Suppl. Ser. 133, 229 244 (1998) Stark profiles of infrared helium lines N. Terzi 1, S. Sahal-Bréchot 2, and Z. Ben

More information

Description of radiation field

Description of radiation field Description of radiation field Qualitatively, we know that characterization should involve energy/time frequency all functions of x,t. direction We also now that radiation is not altered by passing through

More information

Lecture 3. Composition and structure of the atmosphere. Absorption and emission by atmospheric gases.

Lecture 3. Composition and structure of the atmosphere. Absorption and emission by atmospheric gases. Lecture 3. Composition and structure of the atmosphere. Absorption and emission by atmospheric gases. 1. Structure and composition of the Earth s atmosphere. 2. Properties of atmospheric gases. 3. Basic

More information

THz Time-Domain Spectroscopy on Ammonia

THz Time-Domain Spectroscopy on Ammonia 6038 J. Phys. Chem. A 2001, 105, 6038-6047 THz Time-Domain Spectroscopy on Ammonia H. Harde and J. Zhao UniVersität der Bundeswehr Hamburg, Holstenhofweg 85, 22043 Hamburg, Germany M. Wolff, R. A. Cheville,

More information

Spectroscopy of complex organic molecules on Titan A. JOLLY

Spectroscopy of complex organic molecules on Titan A. JOLLY Spectroscopy of complex organic molecules on Titan A. JOLLY Outline of the talk New molecules on Titan? Expected molecules from laboratory experiment Results from the Huygens lander Infrared observation

More information

GEISA 2013 Ozone and related atmospheric species contents description and assessment

GEISA 2013 Ozone and related atmospheric species contents description and assessment GEISA 2013 Ozone and related atmospheric species contents description and assessment N. Jacquinet-Husson C. Boutammine, R. Armante, L.Crépeau, A. Chédin, N.A. Scott, C. Crevoisier, V.Capelle, A. Bouhdaoui

More information

A Study on Infrared Signature of Aircraft Exhaust Plume

A Study on Infrared Signature of Aircraft Exhaust Plume A Study on Infrared Signature of Aircraft Exhaust Plume Pyung Ki Cho a*, Seung Wook Baek a and Bonchan Gu a a Korea Advanced Institute of Science and Technology 291 Daehak-ro, Yuseong-gu, Daejeon 34141,

More information

ROOM TEMPERATURE LINE LISTS FOR CO 2 ISOTOPOLOGUES WITH AB INITIO COMPUTED INTENSITIES

ROOM TEMPERATURE LINE LISTS FOR CO 2 ISOTOPOLOGUES WITH AB INITIO COMPUTED INTENSITIES DEPARTMENT OF PHYSICS AND ASTRONOMY ROOM TEMPERATURE LINE LISTS FOR CO 2 ISOTOPOLOGUES WITH AB INITIO COMPUTED INTENSITIES Emil Żak a, Jonathan Tennyson a, Oleg L. Polyansky a, Lorenzo Lodi a Nikolay F.

More information

A Spectroscopic Database for MIPAS

A Spectroscopic Database for MIPAS A Spectroscopic Database for MIPAS J.-M. Flaud a, C. Piccolo b and B. Carli b a Laboratoire de Photophysique Moleculaire,CNRS, Bat. 350, Université de Paris Sud, 91405 Orsay cedex, France b IFAC-CNR, via

More information

The Stefan-Boltzmann Law

The Stefan-Boltzmann Law The Stefan-Boltzmann Law Department of Physics Ryerson University 1 Introduction Thermal radiation is typically considered the starting point in many texts for discussions of old quantum theory and the

More information

PRESSURE-DEPENDENT LINE PARAMETERS OF CO 2 BY MULTISPECTRUM LEAST-SQUARES FITTING

PRESSURE-DEPENDENT LINE PARAMETERS OF CO 2 BY MULTISPECTRUM LEAST-SQUARES FITTING PRESSURE-DEPENDENT LINE PARAMETERS OF CO 2 BY MULTISPECTRUM LEAST-SQUARES FITTING A project submitted in partial fulfillment of the requirements for the degree of Bachelor of Science with a concentration

More information

An Overview of Molecular Opacities

An Overview of Molecular Opacities Experimental Molecular Spectroscopy & Data Compilations An Overview of Molecular Opacities Peter Peter Bernath Old Dominion University Norfolk, VA JWST Spectroscopy: mainly IR and low resolution Spectra

More information

Observations 3: Data Assimilation of Water Vapour Observations at NWP Centres

Observations 3: Data Assimilation of Water Vapour Observations at NWP Centres Observations 3: Data Assimilation of Water Vapour Observations at NWP Centres OUTLINE: Data Assimilation A simple analogy: data fitting 4D-Var The observation operator : RT modelling Review of Radiative

More information

An ef cient and accurate correlated-k parameterization of infrared radiative transfer for troposphere±stratosphere±mesosphere GCMs

An ef cient and accurate correlated-k parameterization of infrared radiative transfer for troposphere±stratosphere±mesosphere GCMs Atmospheric Science Letters (200) Volume doi:0.006/asle.2000.0022 An ef cient and accurate correlated-k parameterization of infrared radiative transfer for troposphere±stratosphere±mesosphere GCMs Wenyi

More information

Absorption cross-sections of NO 2 : simulation of temperature and pressure eects

Absorption cross-sections of NO 2 : simulation of temperature and pressure eects Journal of Quantitative Spectroscopy & Radiative Transfer 76 (2003) 373 391 www.elsevier.com/locate/jqsrt Absorption cross-sections of NO 2 : simulation of temperature and pressure eects A.C. Vandaele

More information

Relief is on the Way: Status of the Line Positions and Intensities for Nitric Acid

Relief is on the Way: Status of the Line Positions and Intensities for Nitric Acid Relief is on the Way: Status of the Line Positions and Intensities for Nitric Acid Agnés Perrin, J.M.Flaud, J.Orphal Laboratoire Interuniversitaire des Systémes Atmosphériques (LISA), CNRS, Université

More information

Scholars Research Library

Scholars Research Library Available online at www.scholarsresearchlibrary.com Archives of Physics Research, 2011, 2 (3):23-28 (http://scholarsresearchlibrary.com/archive.html) ISSN : 0976-0970 CODEN (USA): APRRC7 Application of

More information

An Overview of the AIRS Radiative Transfer Model

An Overview of the AIRS Radiative Transfer Model IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 41, NO. 2, FEBRUARY 2003 303 An Overview of the AIRS Radiative Transfer Model L. Larrabee Strow, Scott E. Hannon, Sergio De Souza-Machado, Howard

More information

E. V. Karlovets ab, A. Campargue a*, D. Mondelain a, S. Kassi a, S. A. Tashkun b, V. I. Perevalov b

E. V. Karlovets ab, A. Campargue a*, D. Mondelain a, S. Kassi a, S. A. Tashkun b, V. I. Perevalov b High sensitivity Cavity Ring Down spectroscopy of 18 O enriched carbon dioxide between 5850 and 7000 cm -1 : III. Analysis and theoretical modelling of the 12 C 17 O 2, 16 O 12 C 17 O, 17 O 12 C 18 O,

More information

A TOOL FOR THE SECOND GENERATION VERTICAL SOUNDERS RADIANCE SIMULATION: THE GEISA/IASI SPECTROSCOPIC DATABASE SYSTEM

A TOOL FOR THE SECOND GENERATION VERTICAL SOUNDERS RADIANCE SIMULATION: THE GEISA/IASI SPECTROSCOPIC DATABASE SYSTEM A TOOL FOR THE SECOND GENERATION VERTICAL SOUNDERS RADIANCE SIMULATION: THE GEISA/IASI SPECTROSCOPIC DATABASE SYSTEM N. Jacquinet-Husson*, N.A. Scott*, A. Chédin*, and A.A. Chursin** *Laboratoire de Météorologie

More information

Remote Measurement of Emissions by Scanning Imaging Infrared Spectrometry

Remote Measurement of Emissions by Scanning Imaging Infrared Spectrometry Remote Measurement of Emissions by Scanning Imaging Infrared Spectrometry R. Harig *, M. Grutter 2, G. Matz, P. Rusch, J. Gerhard Hamburg University of Technology, Harburger Schlossstr. 2, 279 Hamburg,

More information

Composition and structure of the atmosphere. Absorption and emission by atmospheric gases.

Composition and structure of the atmosphere. Absorption and emission by atmospheric gases. Lecture 3. Composition and structure of the atmosphere. Absorption and emission by atmospheric gases. 1. Structure and composition of the Earth s atmosphere. 2. Properties of atmospheric gases. 3. Basic

More information

Fourier Transform Spectroscopy of the O 2 Herzberg Bands

Fourier Transform Spectroscopy of the O 2 Herzberg Bands Journal of Molecular Spectroscopy 202, 171 193 (2000) doi:10.1006/jmsp.2000.8126, available online at http://www.idealibrary.com on Fourier Transform Spectroscopy of the O 2 Herzberg Bands II. Band Oscillator

More information

Radiation in the Earth's Atmosphere. Part 1: Absorption and Emission by Atmospheric Gases

Radiation in the Earth's Atmosphere. Part 1: Absorption and Emission by Atmospheric Gases Radiation in the Earth's Atmosphere Part 1: Absorption and Emission by Atmospheric Gases Electromagnetic Waves Electromagnetic waves are transversal. Electric and magnetic fields are perpendicular. In

More information

ABSTRACT 1 INTRODUCTION

ABSTRACT 1 INTRODUCTION Terahertz atmospheric attenuation and continuum effects David M. Slocum,* a Thomas M. Goyette, a Elizabeth J. Slingerland, a Robert H. Giles, a and William E. Nixon b a Submillimeter-Wave Technology Laboratory,

More information

Lecture 6 - spectroscopy

Lecture 6 - spectroscopy Lecture 6 - spectroscopy 1 Light Electromagnetic radiation can be thought of as either a wave or as a particle (particle/wave duality). For scattering of light by particles, air, and surfaces, wave theory

More information

ENVISAT VALIDATION RESULTS OBTAINED WITH LPMA AND IASI-BALLOON FTIR

ENVISAT VALIDATION RESULTS OBTAINED WITH LPMA AND IASI-BALLOON FTIR ENVISAT VALIDATION RESULTS OBTAINED WITH LPMA AND IASI-BALLOON FTIR G. Dufour (1), S. Payan (1), Y. Té (1), P. Jeseck (1), V. Ferreira (1), C. Camy-Peyret (1), M. Eremenko (1, *), A. Butz (2), K. Pfeilsticker

More information

Spatial variability of carbon monoxide in Venus mesosphere from Venus Express/Visible and Infrared Thermal Imaging Spectrometer measurements

Spatial variability of carbon monoxide in Venus mesosphere from Venus Express/Visible and Infrared Thermal Imaging Spectrometer measurements Click Here for Full Article JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113,, doi:10.1029/2008je003093, 2008 Spatial variability of carbon monoxide in Venus mesosphere from Venus Express/Visible and Infrared

More information

Spectroscopic Parameter Requirements for Remote Sensing of Terrestrial Planets

Spectroscopic Parameter Requirements for Remote Sensing of Terrestrial Planets Spectroscopic Parameter Requirements for Remote Sensing of Terrestrial Planets The four terrestrial (meaning 'Earth-like') planets of our inner Solar System: Mercury, Venus, Earth and Mars. These images

More information

IRFS-2 instrument onboard Meteor-M N2 satellite: measurements analysis

IRFS-2 instrument onboard Meteor-M N2 satellite: measurements analysis IRFS-2 instrument onboard Meteor-M N2 satellite: measurements analysis Polyakov A.V., Virolainen Ya.A., Timofeyev Yu.M. SPbSU, Saint-Petersburg, Russia Uspensky A.B., A.N. Rublev, SRC Planeta, Moscow,

More information

Ground-based near-infrared observations of water vapour in the Venus troposphere.

Ground-based near-infrared observations of water vapour in the Venus troposphere. Ground-based near-infrared observations of water vapour in the Venus troposphere. S.Chamberlain 1, J.A.Bailey, 2 D.Crisp, 3 and V.S.Meadows 4 1 Centre of Astronomy and Astrophysics, University of Lisbon,

More information

Quantum defect and fine-structure measurements of P, D, F and G Rydberg states of atomic caesium

Quantum defect and fine-structure measurements of P, D, F and G Rydberg states of atomic caesium J. Phys. B: Atom. Molec. Phys., Vol. 12, No. 20, 1979. Printed in Great Britain LETTER TO THE EDTOR Quantum defect and fine-structure measurements of P, D, F and G Rydberg states of atomic caesium L R

More information

The HITRAN 2004 molecular spectroscopic database

The HITRAN 2004 molecular spectroscopic database Journal of Quantitative Spectroscopy & Radiative Transfer 96 (2005) 139 204 www.elsevier.com/locate/jqsrt The HITRAN 2004 molecular spectroscopic database L.S. Rothman a,, D. Jacquemart a,1, A. Barbe b,

More information

Spectroscopic Investigation of Polycyclic Aromatic Hydrocarbons Trapped in Liquid Helium Clusters

Spectroscopic Investigation of Polycyclic Aromatic Hydrocarbons Trapped in Liquid Helium Clusters Spectroscopic Investigation of Polycyclic Aromatic Hydrocarbons Trapped in Liquid Helium Clusters Friedrich Huisken and Serge Krasnokutski Max-Planck-Institut für Strömungsforschung, Bunsenstr. 10, D-37073

More information

Empirical low energy values for methane transitions in the cm-1 region by absorption spectroscopy at 81 K.

Empirical low energy values for methane transitions in the cm-1 region by absorption spectroscopy at 81 K. Empirical low energy values for methane transitions in the 5852-6181 cm-1 region by absorption spectroscopy at 81 K. Bo Gao, Samir Kassi, Alain Campargue To cite this version: Bo Gao, Samir Kassi, Alain

More information

A critical review of the absorption cross-sections of O 3 and NO 2 in the ultraviolet and visible

A critical review of the absorption cross-sections of O 3 and NO 2 in the ultraviolet and visible Journal of Photochemistry and Photobiology A: Chemistry 157 (2003) 185 209 A critical review of the absorption cross-sections of O 3 and NO 2 in the ultraviolet and visible J. Orphal Laboratoire de Photophysique

More information

The spectrum of acetylene in the 5-m region from new line-parameter measurements

The spectrum of acetylene in the 5-m region from new line-parameter measurements Journal of Quantitative Spectroscopy & Radiative Transfer 76 (2003) 237 267 www.elsevier.com/locate/jqsrt The spectrum of acetylene in the 5-m region from new line-parameter measurements D.Jacquemart a,

More information

Journal of Quantitative Spectroscopy & Radiative Transfer

Journal of Quantitative Spectroscopy & Radiative Transfer JQSRT : 4 Journal of Quantitative Spectroscopy & Radiative Transfer ] (]]]]) ]]] ]]] Contents lists available at ScienceDirect Journal of Quantitative Spectroscopy & Radiative Transfer journal homepage:

More information

Infrared and Microwave Spectra and Force Field of DBO: The Coriolis Interaction between the 1 and 2 3 States

Infrared and Microwave Spectra and Force Field of DBO: The Coriolis Interaction between the 1 and 2 3 States JOURNAL OF MOLECULAR SPECTROSCOPY 192, 152 161 (1998) ARTICLE NO. MS987633 Infrared and Microwave Spectra and Force Field of DBO: The Coriolis Interaction between the 1 and 2 3 States Yoshiyuki Kawashima,*

More information

High Sensitivity Gas Sensor Based on IR Spectroscopy Technology and Application

High Sensitivity Gas Sensor Based on IR Spectroscopy Technology and Application PHOTONIC SENSORS / Vol. 6, No. 2, 2016: 127 131 High Sensitivity Gas Sensor Based on IR Spectroscopy Technology and Application Hengyi LI Department of Electronic Information Engineering, Jincheng College

More information

Reinvestigation of the NCN Radical Using Infrared Laser Magnetic Resonance Spectroscopy

Reinvestigation of the NCN Radical Using Infrared Laser Magnetic Resonance Spectroscopy Reinvestigation of the NCN Radical Using Infrared Laser Magnetic Resonance Spectroscopy Brooke Chuzles, Chris DiRocco and Dan Sutton Faculty Sponsor: M. Jackson, Department of Physics ABSTRACT The laser

More information

Training Coarse ECOPROBE 5 CHEMISTRY RS DYNAMICS

Training Coarse ECOPROBE 5 CHEMISTRY RS DYNAMICS Training Coarse ECOPROBE 5 CHEMISTRY Contents Ecoprobe analytical principles Photoionization Infrared spectroscopy Oxygen measurement Pollutants Types and responses Head space New application of Ecoprobe

More information

ARTICLE IN PRESS. JID:THESCI AID:2527 /FLA [m5+; v 1.65; Prn:8/09/2006; 16:19] P.1 (1-12) Sudarshan P. Bharadwaj, Michael F.

ARTICLE IN PRESS. JID:THESCI AID:2527 /FLA [m5+; v 1.65; Prn:8/09/2006; 16:19] P.1 (1-12) Sudarshan P. Bharadwaj, Michael F. JID:THESCI AID:2527 /FLA [m5+; v 1.65; Prn:8/9/26; 16:19] P.1 1-12) 3 International Journal of Thermal Sciences ) 6 4 www.elsevier.com/locate/ijts 61 A multiscale Malkmus model for treatment of inhomogeneous

More information

ANALYZING ASTRONOMICAL OBSERVATIONS WITH THE NASA AMES PAH DATABASE

ANALYZING ASTRONOMICAL OBSERVATIONS WITH THE NASA AMES PAH DATABASE PAHs and the Universe C. Joblin and A.G.G.M. Tielens (eds) EAS Publications Series, 46 (2011) 117-122 www.eas.org ANALYZING ASTRONOMICAL OBSERVATIONS WITH THE NASA AMES PAH DATABASE J. Cami 1, 2 Abstract.

More information

Abstract. Introduction

Abstract. Introduction DESIGNING A MULTIPASS ABSORPTION CELL FOR A HIGH RESOLUTION FTIR SPECTROMETER P. Karhu, T. Ahonen, V.-M. Horneman, and R. Anttila Department of Physical Sciences in the University of Oulu B.O.X 3000 Fin-90014

More information

GEISA Release of updated database and way forward

GEISA Release of updated database and way forward GEISA Release of updated database and way forward N. Jacquinet, R. Armante N.A. Scott, A. Chédin, L. Crépeau, C. Boutammine, A. Bouhdaoui, C. Crevoisier, V. Capelle GEISA: Gestion et Etude des Informations

More information

Methods and Models Used to Parameterize the Infrared Absorption of Methane and Nitrous Oxide for Calculations Within the LLNL/UCLA Climate Model

Methods and Models Used to Parameterize the Infrared Absorption of Methane and Nitrous Oxide for Calculations Within the LLNL/UCLA Climate Model UCRL-ID-129290 Methods and Models Used to Parameterize the Infrared Absorption of Methane and Nitrous Oxide for Calculations Within the LLNL/UCLA Climate Model K.E. Grant A.S. Grossman R.L. Tarp November

More information

The Quest for Consistency and Accuracy of Spectroscopic Parameters in HITRAN:

The Quest for Consistency and Accuracy of Spectroscopic Parameters in HITRAN: The Quest for Consistency and Accuracy of Spectroscopic Parameters in HITRAN: Bridge between Archive and Application Laurence S. Rothman Harvard-Smithsonian Center for Astrophysics Cambridge MA HITRAN

More information

Measurements and modeling of absorption by CO 2 +H 2 O mixtures in the spectral region beyond the CO 2 3 -band head

Measurements and modeling of absorption by CO 2 +H 2 O mixtures in the spectral region beyond the CO 2 3 -band head Measurements and modeling of absorption by CO 2 +H 2 O mixtures in the spectral region beyond the CO 2 3 -band head H. Tran 1,*, M. Turbet 1, P. Chelin 2, X. Landsheere 2 1 Laboratoire de Météorologie

More information

Isotopic effect of Cl + 2 rovibronic spectra in the A X system

Isotopic effect of Cl + 2 rovibronic spectra in the A X system Vol 18 No 7, July 009 c 009 Chin. Phys. Soc. 1674-1056/009/1807)/74-05 Chinese Physics B and IOP Publishing Ltd Isotopic effect of Cl + rovibronic spectra in the A X system Wu Ling ) a)c), Yang Xiao-Hua

More information

MODELING OF NO AND OH INFRARED RADIATION ON A CONVERGENT-DIVERGENT NOZZLE

MODELING OF NO AND OH INFRARED RADIATION ON A CONVERGENT-DIVERGENT NOZZLE 28 TH INTERNATIONAL CONGRESS OF THE AERONAUTICAL SCIENCES MODELING OF NO AND OH INFRARED RADIATION ON A CONVERGENT-DIVERGENT NOZZLE Hyun Jae Nam, Jae Won Kim and Oh Joon Kwon* Korea Advanced Institute

More information

REMOTE SENSING OF ATMOSPHERIC TRACE GASES BY OPTICAL CORRELATION SPECTROSCOPY AND LIDAR

REMOTE SENSING OF ATMOSPHERIC TRACE GASES BY OPTICAL CORRELATION SPECTROSCOPY AND LIDAR REMOTE SENSING OF ATMOSPHERIC TRACE GASES BY OPTICAL CORRELATION SPECTROSCOPY AND LIDAR by Benjamin Thomas Grégory David, Christophe Anselmo, Alain Miffre, Jean-Pierre Cariou and Patrick Rairoux Institute

More information

Refractive indices of water and ice in the to 2.5-gm spectral range

Refractive indices of water and ice in the to 2.5-gm spectral range Refractive indices of water and ice in the 0.65- to 2.5-gm spectral range Linhong Kou, Daniel Labrie, and Petr Chylek New accurate values of the imaginary part, k, of the refractive index of water at T

More information

Observing Habitable Environments Light & Radiation

Observing Habitable Environments Light & Radiation Homework 1 Due Thurs 1/14 Observing Habitable Environments Light & Radiation Given what we know about the origin of life on Earth, how would you recognize life on another world? Would this require a physical

More information

High sensitivity CW-cavity ring down spectroscopy of N 2 O near 1.5lm (I)

High sensitivity CW-cavity ring down spectroscopy of N 2 O near 1.5lm (I) Journal of Molecular Spectroscopy 244 (2007) 33 47 www.elsevier.com/locate/jms High sensitivity CW-cavity ring down spectroscopy of N 2 O near 1.5lm (I) A.W. Liu a,b, S. Kassi a, P. Malara a,c, D. Romanini

More information