Articles | Volume 8, issue 9
https://doi.org/10.5194/amt-8-3767-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/amt-8-3767-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The impact of vibrational Raman scattering of air on DOAS measurements of atmospheric trace gases
J. Lampel
CORRESPONDING AUTHOR
now at: Max Planck Institute for Chemistry, Mainz, Germany
Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany
Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany
U. Platt
Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany
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- Vertical Profiles of Tropospheric Ozone From MAX‐DOAS Measurements During the CINDI‐2 Campaign: Part 1—Development of a New Retrieval Algorithm Y. Wang et al. 10.1029/2018JD028647
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- Raman scattering in the earth’s atmosphere, part I: Optical properties S. Sanghavi 10.1016/j.jqsrt.2022.108328
- Biogenic halocarbons from the Peruvian upwelling region as tropospheric halogen source H. Hepach et al. 10.5194/acp-16-12219-2016
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- New methods for the retrieval of chlorophyll red fluorescence from hyperspectral satellite instruments: simulations and application to GOME-2 and SCIAMACHY J. Joiner et al. 10.5194/amt-9-3939-2016
- Daytime HONO, NO<sub>2</sub> and aerosol distributions from MAX-DOAS observations in Melbourne R. Ryan et al. 10.5194/acp-18-13969-2018
- Intercomparison of NO<sub>2</sub>, O<sub>4</sub>, O<sub>3</sub> and HCHO slant column measurements by MAX-DOAS and zenith-sky UV–visible spectrometers during CINDI-2 K. Kreher et al. 10.5194/amt-13-2169-2020
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- Raman scattering in the Earth’s atmosphere, Part II: Radiative transfer modeling for remote sensing applications S. Sanghavi & C. Frankenberg 10.1016/j.jqsrt.2023.108791
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- Retrieval and Regional Distribution Analysis of Ammonia, Sulfur Dioxide and Nitrogen Dioxide in the Urban Environment Using Ultraviolet DOAS Algorithm H. Chen et al. 10.32604/cmes.2022.022279
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- Evaluating different methods for elevation calibration of MAX-DOAS (Multi AXis Differential Optical Absorption Spectroscopy) instruments during the CINDI-2 campaign S. Donner et al. 10.5194/amt-13-685-2020
- Modeling of inelastically scattered radiation: Rotational Raman scattering in the spherical Earth’s atmosphere A. Rozanov et al. 10.1016/j.jqsrt.2021.107611
- Detection of water vapour absorption around 363 nm in measured atmospheric absorption spectra and its effect on DOAS evaluations J. Lampel et al. 10.5194/acp-17-1271-2017
- Is a scaling factor required to obtain closure between measured and modelled atmospheric O<sub>4</sub> absorptions? An assessment of uncertainties of measurements and radiative transfer simulations for 2 selected days during the MAD-CAT campaign T. Wagner et al. 10.5194/amt-12-2745-2019
- Full latitudinal marine atmospheric measurements of iodine monoxide H. Takashima et al. 10.5194/acp-22-4005-2022
- Evaluation of transport processes over North China Plain and Yangtze River Delta using MAX-DOAS observations Y. Song et al. 10.5194/acp-23-1803-2023
- Ozone Monitoring Instrument (OMI) Total Column Water Vapor version 4 validation and applications H. Wang et al. 10.5194/amt-12-5183-2019
- Space-based observation of volcanic iodine monoxide A. Schönhardt et al. 10.5194/acp-17-4857-2017
- Ultraviolet differential optical absorption spectrometry: quantitative analysis of the CS2produced by SF6decomposition X. Zhang et al. 10.1088/1361-6501/aa821a
26 citations as recorded by crossref.
- 基于国产卫星紫外可见光谱仪的大气水汽总量观测 冉. 赵 et al. 10.1360/N072023-0317
- Inter-comparison of MAX-DOAS measurements of tropospheric HONO slant column densities and vertical profiles during the CINDI-2 campaign Y. Wang et al. 10.5194/amt-13-5087-2020
- Investigating differences in DOAS retrieval codes using MAD-CAT campaign data E. Peters et al. 10.5194/amt-10-955-2017
- Vertical Profiles of Tropospheric Ozone From MAX‐DOAS Measurements During the CINDI‐2 Campaign: Part 1—Development of a New Retrieval Algorithm Y. Wang et al. 10.1029/2018JD028647
- iFit: A simple method for measuring volcanic SO2 without a measured Fraunhofer reference spectrum B. Esse et al. 10.1016/j.jvolgeores.2020.107000
- Raman scattering in the earth’s atmosphere, part I: Optical properties S. Sanghavi 10.1016/j.jqsrt.2022.108328
- Biogenic halocarbons from the Peruvian upwelling region as tropospheric halogen source H. Hepach et al. 10.5194/acp-16-12219-2016
- MAX-DOAS measurements of HONO slant column densities during the MAD-CAT campaign: inter-comparison, sensitivity studies on spectral analysis settings, and error budget Y. Wang et al. 10.5194/amt-10-3719-2017
- The tilt effect in DOAS observations J. Lampel et al. 10.5194/amt-10-4819-2017
- New methods for the retrieval of chlorophyll red fluorescence from hyperspectral satellite instruments: simulations and application to GOME-2 and SCIAMACHY J. Joiner et al. 10.5194/amt-9-3939-2016
- Daytime HONO, NO<sub>2</sub> and aerosol distributions from MAX-DOAS observations in Melbourne R. Ryan et al. 10.5194/acp-18-13969-2018
- Intercomparison of NO<sub>2</sub>, O<sub>4</sub>, O<sub>3</sub> and HCHO slant column measurements by MAX-DOAS and zenith-sky UV–visible spectrometers during CINDI-2 K. Kreher et al. 10.5194/amt-13-2169-2020
- Parameterizing the instrumental spectral response function and its changes by a super-Gaussian and its derivatives S. Beirle et al. 10.5194/amt-10-581-2017
- Detection of O<sub>4</sub> absorption around 328 and 419 nm in measured atmospheric absorption spectra J. Lampel et al. 10.5194/acp-18-1671-2018
- Raman scattering in the Earth’s atmosphere, Part II: Radiative transfer modeling for remote sensing applications S. Sanghavi & C. Frankenberg 10.1016/j.jqsrt.2023.108791
- S5P TROPOMI NO<sub>2</sub> slant column retrieval: method, stability, uncertainties and comparisons with OMI J. van Geffen et al. 10.5194/amt-13-1315-2020
- Retrieval and Regional Distribution Analysis of Ammonia, Sulfur Dioxide and Nitrogen Dioxide in the Urban Environment Using Ultraviolet DOAS Algorithm H. Chen et al. 10.32604/cmes.2022.022279
- On the relative absorption strengths of water vapour in the blue wavelength range J. Lampel et al. 10.5194/amt-8-4329-2015
- Evaluating different methods for elevation calibration of MAX-DOAS (Multi AXis Differential Optical Absorption Spectroscopy) instruments during the CINDI-2 campaign S. Donner et al. 10.5194/amt-13-685-2020
- Modeling of inelastically scattered radiation: Rotational Raman scattering in the spherical Earth’s atmosphere A. Rozanov et al. 10.1016/j.jqsrt.2021.107611
- Detection of water vapour absorption around 363 nm in measured atmospheric absorption spectra and its effect on DOAS evaluations J. Lampel et al. 10.5194/acp-17-1271-2017
- Is a scaling factor required to obtain closure between measured and modelled atmospheric O<sub>4</sub> absorptions? An assessment of uncertainties of measurements and radiative transfer simulations for 2 selected days during the MAD-CAT campaign T. Wagner et al. 10.5194/amt-12-2745-2019
- Full latitudinal marine atmospheric measurements of iodine monoxide H. Takashima et al. 10.5194/acp-22-4005-2022
- Evaluation of transport processes over North China Plain and Yangtze River Delta using MAX-DOAS observations Y. Song et al. 10.5194/acp-23-1803-2023
- Ozone Monitoring Instrument (OMI) Total Column Water Vapor version 4 validation and applications H. Wang et al. 10.5194/amt-12-5183-2019
- Space-based observation of volcanic iodine monoxide A. Schönhardt et al. 10.5194/acp-17-4857-2017
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Latest update: 04 Oct 2024
Short summary
In remote sensing applications, such as differential optical absorption spectroscopy (DOAS), atmospheric scattering processes need to be considered. Inelastic scattering on air molecules can lead to filling-in of absorption lines. The contribution of rotational Raman scattering is typically corrected for. The magnitude of vibrational Raman scattering (VRS) is known from theory and agrees with our first DOAS observations of this effect. Its impact on trace-gas measurements of NO2 is discussed.
In remote sensing applications, such as differential optical absorption spectroscopy (DOAS),...