Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data
Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Panchenko, M. V. [verfasserIn] Zhuravleva, T. B. [verfasserIn] Kozlov, V. S. [verfasserIn] Nasrtdinov, I. M. [verfasserIn] Pol’kin, V. V. [verfasserIn] Terpugova, S. A. [verfasserIn] Chernov, D. G. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Russian meteorology and hydrology - New York, NY : Allerton Press, 2007, 41(2016), 2 vom: Feb., Seite 104-111 |
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| Übergeordnetes Werk: |
volume:41 ; year:2016 ; number:2 ; month:02 ; pages:104-111 |
| Links: |
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| DOI / URN: |
10.3103/S1068373916020047 |
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| Katalog-ID: |
SPR023462892 |
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| 100 | 1 | |a Panchenko, M. V. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data |
| 264 | 1 | |c 2016 | |
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| 520 | |a Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. | ||
| 650 | 4 | |a Empirical model |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a aerosol optical depth |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a single scattering albedo |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a downward fluxes of solar radiation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a deficiency in diurnal values of solar radiation |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Zhuravleva, T. B. |e verfasserin |4 aut | |
| 700 | 1 | |a Kozlov, V. S. |e verfasserin |4 aut | |
| 700 | 1 | |a Nasrtdinov, I. M. |e verfasserin |4 aut | |
| 700 | 1 | |a Pol’kin, V. V. |e verfasserin |4 aut | |
| 700 | 1 | |a Terpugova, S. A. |e verfasserin |4 aut | |
| 700 | 1 | |a Chernov, D. G. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Russian meteorology and hydrology |d New York, NY : Allerton Press, 2007 |g 41(2016), 2 vom: Feb., Seite 104-111 |w (DE-627)531203581 |w (DE-600)2324879-8 |x 1934-8096 |7 nnns |
| 773 | 1 | 8 | |g volume:41 |g year:2016 |g number:2 |g month:02 |g pages:104-111 |
| 856 | 4 | 0 | |u https://dx.doi.org/10.3103/S1068373916020047 |z lizenzpflichtig |3 Volltext |
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10.3103/S1068373916020047 doi (DE-627)SPR023462892 (SPR)S1068373916020047-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Panchenko, M. V. verfasserin aut Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. Empirical model (dpeaa)DE-He213 aerosol optical depth (dpeaa)DE-He213 single scattering albedo (dpeaa)DE-He213 downward fluxes of solar radiation (dpeaa)DE-He213 deficiency in diurnal values of solar radiation (dpeaa)DE-He213 Zhuravleva, T. B. verfasserin aut Kozlov, V. S. verfasserin aut Nasrtdinov, I. M. verfasserin aut Pol’kin, V. V. verfasserin aut Terpugova, S. A. verfasserin aut Chernov, D. G. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 41(2016), 2 vom: Feb., Seite 104-111 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:41 year:2016 number:2 month:02 pages:104-111 https://dx.doi.org/10.3103/S1068373916020047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 41 2016 2 02 104-111 |
| spelling |
10.3103/S1068373916020047 doi (DE-627)SPR023462892 (SPR)S1068373916020047-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Panchenko, M. V. verfasserin aut Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. Empirical model (dpeaa)DE-He213 aerosol optical depth (dpeaa)DE-He213 single scattering albedo (dpeaa)DE-He213 downward fluxes of solar radiation (dpeaa)DE-He213 deficiency in diurnal values of solar radiation (dpeaa)DE-He213 Zhuravleva, T. B. verfasserin aut Kozlov, V. S. verfasserin aut Nasrtdinov, I. M. verfasserin aut Pol’kin, V. V. verfasserin aut Terpugova, S. A. verfasserin aut Chernov, D. G. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 41(2016), 2 vom: Feb., Seite 104-111 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:41 year:2016 number:2 month:02 pages:104-111 https://dx.doi.org/10.3103/S1068373916020047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 41 2016 2 02 104-111 |
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10.3103/S1068373916020047 doi (DE-627)SPR023462892 (SPR)S1068373916020047-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Panchenko, M. V. verfasserin aut Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. Empirical model (dpeaa)DE-He213 aerosol optical depth (dpeaa)DE-He213 single scattering albedo (dpeaa)DE-He213 downward fluxes of solar radiation (dpeaa)DE-He213 deficiency in diurnal values of solar radiation (dpeaa)DE-He213 Zhuravleva, T. B. verfasserin aut Kozlov, V. S. verfasserin aut Nasrtdinov, I. M. verfasserin aut Pol’kin, V. V. verfasserin aut Terpugova, S. A. verfasserin aut Chernov, D. G. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 41(2016), 2 vom: Feb., Seite 104-111 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:41 year:2016 number:2 month:02 pages:104-111 https://dx.doi.org/10.3103/S1068373916020047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 41 2016 2 02 104-111 |
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10.3103/S1068373916020047 doi (DE-627)SPR023462892 (SPR)S1068373916020047-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Panchenko, M. V. verfasserin aut Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. Empirical model (dpeaa)DE-He213 aerosol optical depth (dpeaa)DE-He213 single scattering albedo (dpeaa)DE-He213 downward fluxes of solar radiation (dpeaa)DE-He213 deficiency in diurnal values of solar radiation (dpeaa)DE-He213 Zhuravleva, T. B. verfasserin aut Kozlov, V. S. verfasserin aut Nasrtdinov, I. M. verfasserin aut Pol’kin, V. V. verfasserin aut Terpugova, S. A. verfasserin aut Chernov, D. G. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 41(2016), 2 vom: Feb., Seite 104-111 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:41 year:2016 number:2 month:02 pages:104-111 https://dx.doi.org/10.3103/S1068373916020047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 41 2016 2 02 104-111 |
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10.3103/S1068373916020047 doi (DE-627)SPR023462892 (SPR)S1068373916020047-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl 38.85 bkl Panchenko, M. V. verfasserin aut Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. Empirical model (dpeaa)DE-He213 aerosol optical depth (dpeaa)DE-He213 single scattering albedo (dpeaa)DE-He213 downward fluxes of solar radiation (dpeaa)DE-He213 deficiency in diurnal values of solar radiation (dpeaa)DE-He213 Zhuravleva, T. B. verfasserin aut Kozlov, V. S. verfasserin aut Nasrtdinov, I. M. verfasserin aut Pol’kin, V. V. verfasserin aut Terpugova, S. A. verfasserin aut Chernov, D. G. verfasserin aut Enthalten in Russian meteorology and hydrology New York, NY : Allerton Press, 2007 41(2016), 2 vom: Feb., Seite 104-111 (DE-627)531203581 (DE-600)2324879-8 1934-8096 nnns volume:41 year:2016 number:2 month:02 pages:104-111 https://dx.doi.org/10.3103/S1068373916020047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE 38.85 ASE AR 41 2016 2 02 104-111 |
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Enthalten in Russian meteorology and hydrology 41(2016), 2 vom: Feb., Seite 104-111 volume:41 year:2016 number:2 month:02 pages:104-111 |
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Enthalten in Russian meteorology and hydrology 41(2016), 2 vom: Feb., Seite 104-111 volume:41 year:2016 number:2 month:02 pages:104-111 |
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Empirical model aerosol optical depth single scattering albedo downward fluxes of solar radiation deficiency in diurnal values of solar radiation |
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Russian meteorology and hydrology |
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Panchenko, M. V. @@aut@@ Zhuravleva, T. B. @@aut@@ Kozlov, V. S. @@aut@@ Nasrtdinov, I. M. @@aut@@ Pol’kin, V. V. @@aut@@ Terpugova, S. A. @@aut@@ Chernov, D. G. @@aut@@ |
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Panchenko, M. V. |
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Panchenko, M. V. ddc 550 bkl 38.80 bkl 38.85 misc Empirical model misc aerosol optical depth misc single scattering albedo misc downward fluxes of solar radiation misc deficiency in diurnal values of solar radiation Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data |
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550 ASE 38.80 bkl 38.85 bkl Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data Empirical model (dpeaa)DE-He213 aerosol optical depth (dpeaa)DE-He213 single scattering albedo (dpeaa)DE-He213 downward fluxes of solar radiation (dpeaa)DE-He213 deficiency in diurnal values of solar radiation (dpeaa)DE-He213 |
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ddc 550 bkl 38.80 bkl 38.85 misc Empirical model misc aerosol optical depth misc single scattering albedo misc downward fluxes of solar radiation misc deficiency in diurnal values of solar radiation |
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ddc 550 bkl 38.80 bkl 38.85 misc Empirical model misc aerosol optical depth misc single scattering albedo misc downward fluxes of solar radiation misc deficiency in diurnal values of solar radiation |
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Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data |
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Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data |
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Panchenko, M. V. |
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Russian meteorology and hydrology |
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Panchenko, M. V. Zhuravleva, T. B. Kozlov, V. S. Nasrtdinov, I. M. Pol’kin, V. V. Terpugova, S. A. Chernov, D. G. |
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Panchenko, M. V. |
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verfasserin |
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estimation of aerosol radiation effects under background and smoke-haze atmospheric conditions over siberia from empirical data |
| title_auth |
Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data |
| abstract |
Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. |
| abstractGer |
Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. |
| abstract_unstemmed |
Abstract The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/$ m^{2} $. |
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2 |
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Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data |
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https://dx.doi.org/10.3103/S1068373916020047 |
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Zhuravleva, T. B. Kozlov, V. S. Nasrtdinov, I. M. Pol’kin, V. V. Terpugova, S. A. Chernov, D. G. |
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Zhuravleva, T. B. Kozlov, V. S. Nasrtdinov, I. M. Pol’kin, V. V. Terpugova, S. A. Chernov, D. G. |
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10.3103/S1068373916020047 |
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2024-07-03T19:05:22.258Z |
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| score |
7.3985205 |