Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area
Descrevemos os resultados do estudo da profundidade ótica do aerossol (POA) e do Forçamento Radiativo Direto (FRD) no topo da atmosfera (TOA), obtidos durante a campanha de medição e monitoramento, XXI Expedição Antártica do Peru, entre os meses de janeiro e fevereiro de 2013, e na área metropolitan...
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Universidade Federal do Rio de Janeiro
2020
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Portal de Periódicos da UFRJ (Universidade Federal do Rio de Janeiro) |
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English |
topic |
Aerosol Radiative Forcing Antarctic |
spellingShingle |
Aerosol Radiative Forcing Antarctic Angeles Suazo, Julio Miguel Suarez Salas, Luis Huaman De La Cruz, Alex Rubén Angeles Vasquez, Roberto Rosales Aylas, Georgynio Rocha Condor, Alicia Requena Rojas, Edilson Muñoz Ccuro, Felipa Flores Rojas, Jose Luis Abi Karam, Hugo Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area |
topic_facet |
Aerosol Radiative Forcing Antarctic |
description |
Descrevemos os resultados do estudo da profundidade ótica do aerossol (POA) e do Forçamento Radiativo Direto (FRD) no topo da atmosfera (TOA), obtidos durante a campanha de medição e monitoramento, XXI Expedição Antártica do Peru, entre os meses de janeiro e fevereiro de 2013, e na área metropolitana de Huancayo (AMH) entre os meses de junho e julho de 2019. Na Estação Antártica Peruana Machu Picchu utilizou-se um fotômetro solar SP02-L. Tal instrumento possui 4 canais: 412 nm, 500 nm, 675 nm e 862 nm, permitindo realizar medições diretas do espectro de radiação visível. Na AMH usamos o sensor BF5, que mede a radiação direta, difusa e global em comprimento de onda curta. Os cálculos de AOD em latitudes polares variaram entre 0,0646 e 0,1061. Na AMH apresenta valor máximo de 0,58 (11 de junho) e mínimo de 0,19 (12 de junho). Determinou-se o coeficiente de Angstrom variando de 0 a 0,07, esses valores indicam a presença de partículas grandes. Na AMH varia de 0 a 1,8, que indica a presença de aerossóis de fonte de queima de biomassa e industrial. As propriedades óticas observadas foram usadas para estimar a forçante radiativa direta por aerossóis (FRDA) no topo da atmosfera. Os resultados indicam que no King George Island, o FRDA, está entre -2 e 4 W/m2; já para a AMH a forçante radiativa direta de aerossol está entre 0 e 20 W/m2. |
format |
Article in Journal/Newspaper |
author |
Angeles Suazo, Julio Miguel Suarez Salas, Luis Huaman De La Cruz, Alex Rubén Angeles Vasquez, Roberto Rosales Aylas, Georgynio Rocha Condor, Alicia Requena Rojas, Edilson Muñoz Ccuro, Felipa Flores Rojas, Jose Luis Abi Karam, Hugo |
author_facet |
Angeles Suazo, Julio Miguel Suarez Salas, Luis Huaman De La Cruz, Alex Rubén Angeles Vasquez, Roberto Rosales Aylas, Georgynio Rocha Condor, Alicia Requena Rojas, Edilson Muñoz Ccuro, Felipa Flores Rojas, Jose Luis Abi Karam, Hugo |
author_sort |
Angeles Suazo, Julio Miguel |
title |
Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area |
title_short |
Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area |
title_full |
Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area |
title_fullStr |
Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area |
title_full_unstemmed |
Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area |
title_sort |
direct radiative forcing due to aerosol properties at the peruvian antarctic station and metropolitan huancayo area |
publisher |
Universidade Federal do Rio de Janeiro |
publishDate |
2020 |
url |
https://revistas.ufrj.br/index.php/aigeo/article/view/35045 https://doi.org/10.11137/2020_4_404_412 |
geographic |
Antarctic King George Island |
geographic_facet |
Antarctic King George Island |
genre |
Annals of Glaciology Antarc* Antarctic Antártica King George Island |
genre_facet |
Annals of Glaciology Antarc* Antarctic Antártica King George Island |
op_source |
Anuário do Instituto de Geociências; v. 43, n. 4 (2020); 404_412 1982-3908 0101-9759 |
op_relation |
https://revistas.ufrj.br/index.php/aigeo/article/view/35045/22011 Ångström, A. 1964. The parameters of atmospheric turbidity. Tellus, 16: 64-75. Braun, M.; Saurer, S.; Vogt, J.; Simoes, C. & Gobmann, H. 2001. The influence of large-scale atmospheric circulation on the surface energy balance of the King George Island ice cap. International Journal of Climatology, 21: 21–36. Cachorro, V.; Vergaz, R. & Frutos, A. 2001. A quantitative comparison of a-Angstrom turbidity parameter retrieved in different spectral ranges based on spectroradiometer solar radiation measurements. Atmospheric Environment, 35: 5117– 5124. Castro, T.; Madronich, S.; Rivale, S.; Muhlia, A. & Mar, B. 2001. Influence of aerosols on photochemical smog in Mexico City. Atmospheric Environment, 35: 1765-1772. Charlson, R.; Schwartz, S.; Hales, J.; Cess, R.; Coakley, J.; Hanses, J. & Hofmann, D. 1992. Climate forcing by anthropogenic aerosols. Science, 255: 423–430. Eck, T.; Holben, B.; Reid, J.; O’Neill, N.; Schafer, J.; Dubovik, O.; Simimov, A.; Yamasoe, M. & Artaxo, P. 2003. High aerosol optical depth biomass burning events: A comparison of optical properties for different source regions. Geophysical Research Letters, 30(20): 2035-2044. Eck, T.F.; Holben, B.N.; Reid, J.S.; Dubovik, O.; Smirnov, A.; O’Neill, N.; Slutsker, I. & Kinne, S. 1999. Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols. Journal of Geophysical Resesearch, 104(31): 333– 349. Estevan, R.; Martínez, D.; Suarez, L.; Moya, A. & Silva, Y. 2019. First two and a half years of aerosol measurements with an AERONET sunphotometer at the Huancayo Observatory, Peru. Atmospheric Environment, 3: 1-13. El-Shobokshy, M. & Al-Saedi, Y. 1993. Atmospheric turbidity and transmittance of solar radiation in Riyadh, Saudi Arabia. Atmospheric Environment, 27(4): 401–411. Ferron, F.; Simões, J.; Aquino, F. & Setzer, A. 2004. Air temperature time series for King George Island, Antarctica. Pesquisa Antártica Brasileira, 4: 155-169. Forster, P.; Ramaswamy, V.; Artaxo, P.; Berntsen, T.; Betts, R.; Fahey, D. W.; Haywood, J.; Lean, J.; Lowe, D. C.; Myhre, G.; Nganga, J.; Prinn, R.; Raga, G.; Schulz, M. & Van Dorland, R. 2007. Changes in Atmospheric Constituents and Radiative Forcing, In: Climate Change 2007: The Physical Science Basis, Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK and New York, NY, USA. Haywood, K. & Shine, K. 1995. The effect of anthropogenic sulfate and soot aerosol on the clear sky planetary radiation budget. Geophysical Research Letters, 22(5): 603-606. Haywood, J. & Boucher, O. 2000. Estimates of the direct and indirect radiative forcing due to tropospheric aerosols: a review. Reviews of Geophysics, 38(4): 513-543. Instituto Nacional de Estadística e Informática. 2007. Perfil sociodemográfico de la provincia de Huancayo. Disponible en: https://www.inei.gob.pe/media/MenuRecursivo/publicaciones_digitales/Est/Lib1136/libro.pdf. Acceso en 2 de febrero de 2020 y 1 de junio de 2020. Houghton, J.; Mereira, L.; Callander, B.; Harris, N.; Kattenberg, A. & Maskell, K. 1995. Climate Change 1995: The Science of Climate Change, The Contribution of Working Group I to the Second Assessment Report of the IPCC. New York, Cambridge University Press, 572p. Liou, K. 2007. An introduction to atmospheric radiation. New York 2nd Ed., Academic Press, 583p. Mazzola, M.; Stone, R.S.; Herber, A.; Tomasi, C.; Lupi, A.; Vitale, V.; Lanconelli, C.; Toledano, C.; Cachorro, V.; O’Neill, N.; Shiobara, M.; Aaltonen, V.; Stebel, K.; Zielinski, T.; Petelski, T.; Ortiz de Galisteo, J.; Torres, B.; Berjon, A.; Goloub, P.; Li, Z.; Blarel, L.; Abboud, I.; Cuevas, E.; Stock, M.; Schulz, K. & Virkkula, A. 2011. Evaluation of sun photometer capabilities for retrievals of aerosol optical depth at high latitudes: The POLAR-AOD intercomparison campaigns. Atmospheric Environment, 52: 4-17. Myhre, G. & Shindell, D. 2013. Anthropogenic and Natural radiative Forcing. Intergovernmental Panel of Change Climate, p. 659-740. Middleton Solar. 2004. SP02 y SP02-L Sunphotometer user’s guide, Victoria, pag. 9. Mitchell, R. & Forgan, B. 2003. Aerosol measurement in the Australian outback: intercomparison of sun photometers. Journal of Atmospheric and Oceanic Technology, 20: 54-66. Otero, L.; Ristori, P.; Holben, B. & Quel, E. 2006. Espesor óptico de aerosoles durante el año 2002 para diez estaciones pertenecientes a la red AERONET – NASA. Óptica Pura y Aplicada, 39(4): 355-364. Shaw, G. 1982. Atmospheric turbidity in the Polar regions. Journal of Applied Meteorology, 21: 1080– 1088. Shifrin, K. 1995. Simple Relationships for the Angstrom parameter of disperse systems. Applied Optical, 34: 4480 – 4485. Simoes, J.; Bremer, U.; Aquino, F. & Ferron, F. 1999. Morphology and variations of glacial drainage basins in the King George Island ice field, Antarctica. Annals of Glaciology, 29: 220–224. Stone, R.S. 2002. Monitoring aerosol optical depth at Barrow, Alaska and South Pole; Historical overview, recent results, and future goals. In: COLACINO, M. (ED.), Proceedings of the 9th Workshop Italian Research on Antarctic Atmosphere, Rome, Italy, 22-24 October 2001. Italian Physical Society, Bologna, Italy, pp. 123-144. Tomasi, C.; Caroli, E. & Vitale, V. 1983. Study of the relationship between Ångström’s wavelength exponent and Junge particle size distribution exponent. Journal of Climate and Applied Meteorology, 22: 1707-1716. Tomasi, C.; Vitale, V.; Lupi, A.; Di Carmine, C.; Campanelli, M.; Herber, A.; Treffeisen, R.; Stone, R.; Andrews, E.; Sharma, S.; Radionov, V.; von Hoyningen-Huene, W.; Stebel, K.; Hansen, G.H.; Myhre, C.; Wehrli, C.; Aaltonen, V.; Lihavainen, H.; Virkkula, A.; Hillamo, R.; Ström, J.; Toledano, C.; Cachorro, V.; Ortiz, P.; de Frutos, A.; Blindheim, S.; Frioud, M.; Gausa, M.; Zielinski, T.; Petelski, T. & Yamanouchi, T. 2007. Aerosols in polar regions: a historical overview based on optical depth and in situ observations. Journal of Geophysical Research, 112: 1-28. Volz, F. 1959. Photometer mit Selen-Photoelement zur spektralen messing der Soonenstrahlung and zur Bestimmung der wellenlangenabhangigkeit der Dunsttrubung. Archiv fur Meteolologie Geophysik und Bioklimatologie, 10: 100-131. World Meteorology Organization. 2005. WMO/GAW Experts Workshop on a Global Surface-based Network for Long Term Observations of Column Aerosol Optical Properties. Switzerland, 153 p. https://revistas.ufrj.br/index.php/aigeo/article/view/35045 doi:10.11137/2020_4_404_412 |
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ftufriodejaneiro:oai:www.revistas.ufrj.br:article/35045 2023-05-15T13:29:51+02:00 Direct Radiative Forcing Due to Aerosol Properties at the Peruvian Antarctic Station and Metropolitan Huancayo Area Angeles Suazo, Julio Miguel Suarez Salas, Luis Huaman De La Cruz, Alex Rubén Angeles Vasquez, Roberto Rosales Aylas, Georgynio Rocha Condor, Alicia Requena Rojas, Edilson Muñoz Ccuro, Felipa Flores Rojas, Jose Luis Abi Karam, Hugo 2020-12-18 application/pdf https://revistas.ufrj.br/index.php/aigeo/article/view/35045 https://doi.org/10.11137/2020_4_404_412 eng eng Universidade Federal do Rio de Janeiro https://revistas.ufrj.br/index.php/aigeo/article/view/35045/22011 Ångström, A. 1964. The parameters of atmospheric turbidity. Tellus, 16: 64-75. Braun, M.; Saurer, S.; Vogt, J.; Simoes, C. & Gobmann, H. 2001. The influence of large-scale atmospheric circulation on the surface energy balance of the King George Island ice cap. International Journal of Climatology, 21: 21–36. Cachorro, V.; Vergaz, R. & Frutos, A. 2001. A quantitative comparison of a-Angstrom turbidity parameter retrieved in different spectral ranges based on spectroradiometer solar radiation measurements. Atmospheric Environment, 35: 5117– 5124. Castro, T.; Madronich, S.; Rivale, S.; Muhlia, A. & Mar, B. 2001. Influence of aerosols on photochemical smog in Mexico City. Atmospheric Environment, 35: 1765-1772. Charlson, R.; Schwartz, S.; Hales, J.; Cess, R.; Coakley, J.; Hanses, J. & Hofmann, D. 1992. Climate forcing by anthropogenic aerosols. Science, 255: 423–430. Eck, T.; Holben, B.; Reid, J.; O’Neill, N.; Schafer, J.; Dubovik, O.; Simimov, A.; Yamasoe, M. & Artaxo, P. 2003. High aerosol optical depth biomass burning events: A comparison of optical properties for different source regions. Geophysical Research Letters, 30(20): 2035-2044. Eck, T.F.; Holben, B.N.; Reid, J.S.; Dubovik, O.; Smirnov, A.; O’Neill, N.; Slutsker, I. & Kinne, S. 1999. Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols. Journal of Geophysical Resesearch, 104(31): 333– 349. Estevan, R.; Martínez, D.; Suarez, L.; Moya, A. & Silva, Y. 2019. First two and a half years of aerosol measurements with an AERONET sunphotometer at the Huancayo Observatory, Peru. Atmospheric Environment, 3: 1-13. El-Shobokshy, M. & Al-Saedi, Y. 1993. Atmospheric turbidity and transmittance of solar radiation in Riyadh, Saudi Arabia. Atmospheric Environment, 27(4): 401–411. Ferron, F.; Simões, J.; Aquino, F. & Setzer, A. 2004. Air temperature time series for King George Island, Antarctica. Pesquisa Antártica Brasileira, 4: 155-169. Forster, P.; Ramaswamy, V.; Artaxo, P.; Berntsen, T.; Betts, R.; Fahey, D. W.; Haywood, J.; Lean, J.; Lowe, D. C.; Myhre, G.; Nganga, J.; Prinn, R.; Raga, G.; Schulz, M. & Van Dorland, R. 2007. Changes in Atmospheric Constituents and Radiative Forcing, In: Climate Change 2007: The Physical Science Basis, Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK and New York, NY, USA. Haywood, K. & Shine, K. 1995. The effect of anthropogenic sulfate and soot aerosol on the clear sky planetary radiation budget. Geophysical Research Letters, 22(5): 603-606. Haywood, J. & Boucher, O. 2000. Estimates of the direct and indirect radiative forcing due to tropospheric aerosols: a review. Reviews of Geophysics, 38(4): 513-543. Instituto Nacional de Estadística e Informática. 2007. Perfil sociodemográfico de la provincia de Huancayo. Disponible en: https://www.inei.gob.pe/media/MenuRecursivo/publicaciones_digitales/Est/Lib1136/libro.pdf. Acceso en 2 de febrero de 2020 y 1 de junio de 2020. Houghton, J.; Mereira, L.; Callander, B.; Harris, N.; Kattenberg, A. & Maskell, K. 1995. Climate Change 1995: The Science of Climate Change, The Contribution of Working Group I to the Second Assessment Report of the IPCC. New York, Cambridge University Press, 572p. Liou, K. 2007. An introduction to atmospheric radiation. New York 2nd Ed., Academic Press, 583p. Mazzola, M.; Stone, R.S.; Herber, A.; Tomasi, C.; Lupi, A.; Vitale, V.; Lanconelli, C.; Toledano, C.; Cachorro, V.; O’Neill, N.; Shiobara, M.; Aaltonen, V.; Stebel, K.; Zielinski, T.; Petelski, T.; Ortiz de Galisteo, J.; Torres, B.; Berjon, A.; Goloub, P.; Li, Z.; Blarel, L.; Abboud, I.; Cuevas, E.; Stock, M.; Schulz, K. & Virkkula, A. 2011. Evaluation of sun photometer capabilities for retrievals of aerosol optical depth at high latitudes: The POLAR-AOD intercomparison campaigns. Atmospheric Environment, 52: 4-17. Myhre, G. & Shindell, D. 2013. Anthropogenic and Natural radiative Forcing. Intergovernmental Panel of Change Climate, p. 659-740. Middleton Solar. 2004. SP02 y SP02-L Sunphotometer user’s guide, Victoria, pag. 9. Mitchell, R. & Forgan, B. 2003. Aerosol measurement in the Australian outback: intercomparison of sun photometers. Journal of Atmospheric and Oceanic Technology, 20: 54-66. Otero, L.; Ristori, P.; Holben, B. & Quel, E. 2006. Espesor óptico de aerosoles durante el año 2002 para diez estaciones pertenecientes a la red AERONET – NASA. Óptica Pura y Aplicada, 39(4): 355-364. Shaw, G. 1982. Atmospheric turbidity in the Polar regions. Journal of Applied Meteorology, 21: 1080– 1088. Shifrin, K. 1995. Simple Relationships for the Angstrom parameter of disperse systems. Applied Optical, 34: 4480 – 4485. Simoes, J.; Bremer, U.; Aquino, F. & Ferron, F. 1999. Morphology and variations of glacial drainage basins in the King George Island ice field, Antarctica. Annals of Glaciology, 29: 220–224. Stone, R.S. 2002. Monitoring aerosol optical depth at Barrow, Alaska and South Pole; Historical overview, recent results, and future goals. In: COLACINO, M. (ED.), Proceedings of the 9th Workshop Italian Research on Antarctic Atmosphere, Rome, Italy, 22-24 October 2001. Italian Physical Society, Bologna, Italy, pp. 123-144. Tomasi, C.; Caroli, E. & Vitale, V. 1983. Study of the relationship between Ångström’s wavelength exponent and Junge particle size distribution exponent. Journal of Climate and Applied Meteorology, 22: 1707-1716. Tomasi, C.; Vitale, V.; Lupi, A.; Di Carmine, C.; Campanelli, M.; Herber, A.; Treffeisen, R.; Stone, R.; Andrews, E.; Sharma, S.; Radionov, V.; von Hoyningen-Huene, W.; Stebel, K.; Hansen, G.H.; Myhre, C.; Wehrli, C.; Aaltonen, V.; Lihavainen, H.; Virkkula, A.; Hillamo, R.; Ström, J.; Toledano, C.; Cachorro, V.; Ortiz, P.; de Frutos, A.; Blindheim, S.; Frioud, M.; Gausa, M.; Zielinski, T.; Petelski, T. & Yamanouchi, T. 2007. Aerosols in polar regions: a historical overview based on optical depth and in situ observations. Journal of Geophysical Research, 112: 1-28. Volz, F. 1959. Photometer mit Selen-Photoelement zur spektralen messing der Soonenstrahlung and zur Bestimmung der wellenlangenabhangigkeit der Dunsttrubung. Archiv fur Meteolologie Geophysik und Bioklimatologie, 10: 100-131. World Meteorology Organization. 2005. WMO/GAW Experts Workshop on a Global Surface-based Network for Long Term Observations of Column Aerosol Optical Properties. Switzerland, 153 p. https://revistas.ufrj.br/index.php/aigeo/article/view/35045 doi:10.11137/2020_4_404_412 Direitos autorais 2020 Anuário do Instituto de Geociências http://creativecommons.org/licenses/by/4.0 CC-BY Anuário do Instituto de Geociências; v. 43, n. 4 (2020); 404_412 1982-3908 0101-9759 Aerosol Radiative Forcing Antarctic info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2020 ftufriodejaneiro https://doi.org/10.11137/2020_4_404_412 2022-01-02T02:21:00Z Descrevemos os resultados do estudo da profundidade ótica do aerossol (POA) e do Forçamento Radiativo Direto (FRD) no topo da atmosfera (TOA), obtidos durante a campanha de medição e monitoramento, XXI Expedição Antártica do Peru, entre os meses de janeiro e fevereiro de 2013, e na área metropolitana de Huancayo (AMH) entre os meses de junho e julho de 2019. Na Estação Antártica Peruana Machu Picchu utilizou-se um fotômetro solar SP02-L. Tal instrumento possui 4 canais: 412 nm, 500 nm, 675 nm e 862 nm, permitindo realizar medições diretas do espectro de radiação visível. Na AMH usamos o sensor BF5, que mede a radiação direta, difusa e global em comprimento de onda curta. Os cálculos de AOD em latitudes polares variaram entre 0,0646 e 0,1061. Na AMH apresenta valor máximo de 0,58 (11 de junho) e mínimo de 0,19 (12 de junho). Determinou-se o coeficiente de Angstrom variando de 0 a 0,07, esses valores indicam a presença de partículas grandes. Na AMH varia de 0 a 1,8, que indica a presença de aerossóis de fonte de queima de biomassa e industrial. As propriedades óticas observadas foram usadas para estimar a forçante radiativa direta por aerossóis (FRDA) no topo da atmosfera. Os resultados indicam que no King George Island, o FRDA, está entre -2 e 4 W/m2; já para a AMH a forçante radiativa direta de aerossol está entre 0 e 20 W/m2. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Antártica King George Island Portal de Periódicos da UFRJ (Universidade Federal do Rio de Janeiro) Antarctic King George Island Anuário do Instituto de Geociências 43 4 |