Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere
Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A cri...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Korshunov, V. A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. |
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| Übergeordnetes Werk: |
Enthalten in: Atmospheric and oceanic optics - Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009, 35(2022), 2 vom: Apr., Seite 151-157 |
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| Übergeordnetes Werk: |
volume:35 ; year:2022 ; number:2 ; month:04 ; pages:151-157 |
| Links: |
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| DOI / URN: |
10.1134/S1024856022020051 |
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| Katalog-ID: |
SPR050668781 |
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| 520 | |a Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. | ||
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10.1134/S1024856022020051 doi (DE-627)SPR050668781 (SPR)S1024856022020051-e DE-627 ger DE-627 rakwb eng Korshunov, V. A. verfasserin aut Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 35(2022), 2 vom: Apr., Seite 151-157 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:35 year:2022 number:2 month:04 pages:151-157 https://dx.doi.org/10.1134/S1024856022020051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 35 2022 2 04 151-157 |
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10.1134/S1024856022020051 doi (DE-627)SPR050668781 (SPR)S1024856022020051-e DE-627 ger DE-627 rakwb eng Korshunov, V. A. verfasserin aut Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 35(2022), 2 vom: Apr., Seite 151-157 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:35 year:2022 number:2 month:04 pages:151-157 https://dx.doi.org/10.1134/S1024856022020051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 35 2022 2 04 151-157 |
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10.1134/S1024856022020051 doi (DE-627)SPR050668781 (SPR)S1024856022020051-e DE-627 ger DE-627 rakwb eng Korshunov, V. A. verfasserin aut Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 35(2022), 2 vom: Apr., Seite 151-157 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:35 year:2022 number:2 month:04 pages:151-157 https://dx.doi.org/10.1134/S1024856022020051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 35 2022 2 04 151-157 |
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10.1134/S1024856022020051 doi (DE-627)SPR050668781 (SPR)S1024856022020051-e DE-627 ger DE-627 rakwb eng Korshunov, V. A. verfasserin aut Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 35(2022), 2 vom: Apr., Seite 151-157 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:35 year:2022 number:2 month:04 pages:151-157 https://dx.doi.org/10.1134/S1024856022020051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 35 2022 2 04 151-157 |
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10.1134/S1024856022020051 doi (DE-627)SPR050668781 (SPR)S1024856022020051-e DE-627 ger DE-627 rakwb eng Korshunov, V. A. verfasserin aut Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 35(2022), 2 vom: Apr., Seite 151-157 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:35 year:2022 number:2 month:04 pages:151-157 https://dx.doi.org/10.1134/S1024856022020051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 35 2022 2 04 151-157 |
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Korshunov, V. A. Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere |
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Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere |
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multiple scattering in cirrus clouds and taking it into account when interpreting lidar measurements in the stratosphere |
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Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere |
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Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. |
| abstractGer |
Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. |
| abstract_unstemmed |
Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data. © Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana. |
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Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">SPR050668781</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230507164951.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230507s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S1024856022020051</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR050668781</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)S1024856022020051-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Korshunov, V. A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Multiple Scattering in Cirrus Clouds and Taking It into Account When Interpreting Lidar Measurements in the Stratosphere</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Ltd. 2022. ISSN 1024-8560, Atmospheric and Oceanic Optics, 2022, Vol. 35, No. 2, pp. 151–157. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Optika Atmosfery i Okeana.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Multiple scattering arising in cirrus clouds in the process of lidar sensing of the atmosphere is studied using the Monte Carlo method. The calculations are performed for model scattering phase functions corresponding to crystalline cirrus cloud particles with sizes from 20 to 100 µm. A critical analysis of some common methods for multiple scattering correction in cirrus clouds is carried out. Numerical experiments on sensing cirrus clouds and stratospheric aerosol from the Earth’s surface with signal calibration at an altitude of 30 km are conducted. It is shown that ignoring the multiple scattering in this measurement scheme leads to a considerable distortion of the altitude profile of the backscattering coefficient in cirrus clouds and above them; at the same time, errors in the determination of the optical thickness of the clouds remain insignificant. An iteration scheme for taking into account multiple scattering is proposed and tested in numerical experiments. The simulation results are compared with experimental data.</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Atmospheric and oceanic optics</subfield><subfield code="d">Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009</subfield><subfield code="g">35(2022), 2 vom: Apr., Seite 151-157</subfield><subfield code="w">(DE-627)599674695</subfield><subfield code="w">(DE-600)2493873-7</subfield><subfield code="x">2070-0393</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:35</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:2</subfield><subfield code="g">month:04</subfield><subfield code="g">pages:151-157</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1134/S1024856022020051</subfield><subfield code="z">lizenzpflichtig</subfield><subfield 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