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Aerosol Optical Depth measurements in the Azores.

Bibliographic Details
Main Author: Carvalho, Fernanda
Publication Date: 2008
Other Authors: Henriques, Diamantino, Fialho, Paulo
Language: eng
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: http://hdl.handle.net/10400.3/2224
Summary: A preliminary analysis of AOD results from sun-photometer measurements collected at Jose Agostinho Observatory at Angra do Heroísmo (Terceira Island, the Azores) was presented. The observational period ranges from August 2004 to December 2007, using a SP02 sun-photometer at wavelengths 412, 500, 675, and 862 nm, coupled to a 2AXP sun-tracker. The sampling interval is 5 s and data is filtered for cloud contamination in a time window of 10 minutes. Most AOD 500 nm values are below 0.3, showing a small variation during the day; frequency distribution shows a typical right skew distribution. Alpha and beta Angstrom coefficients were also computed and analyzed in the same way. Alpha values are generally positive and lower than 4, while beta values are below 1.5. AOD results from the AERONET station at Horta Observatory (Faial Island, the Azores) were also used and compared with Angra data. AOD and Angstrom coefficients were also analyzed with wind results from the automatic weather station located at both observatories. Results show different wind distributions due to different exposures; however, systematic higher AOD values are found at Horta. The proximity of the two sites indicates that these differences are more likely due to different instruments and processing methods used.
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spelling Aerosol Optical Depth measurements in the Azores.Aerosol Optical DepthTerceira Island (Azores)AzoresA preliminary analysis of AOD results from sun-photometer measurements collected at Jose Agostinho Observatory at Angra do Heroísmo (Terceira Island, the Azores) was presented. The observational period ranges from August 2004 to December 2007, using a SP02 sun-photometer at wavelengths 412, 500, 675, and 862 nm, coupled to a 2AXP sun-tracker. The sampling interval is 5 s and data is filtered for cloud contamination in a time window of 10 minutes. Most AOD 500 nm values are below 0.3, showing a small variation during the day; frequency distribution shows a typical right skew distribution. Alpha and beta Angstrom coefficients were also computed and analyzed in the same way. Alpha values are generally positive and lower than 4, while beta values are below 1.5. AOD results from the AERONET station at Horta Observatory (Faial Island, the Azores) were also used and compared with Angra data. AOD and Angstrom coefficients were also analyzed with wind results from the automatic weather station located at both observatories. Results show different wind distributions due to different exposures; however, systematic higher AOD values are found at Horta. The proximity of the two sites indicates that these differences are more likely due to different instruments and processing methods used.Repositório da Universidade dos AçoresCarvalho, FernandaHenriques, DiamantinoFialho, Paulo2013-09-09T12:20:43Z2008-072013-08-14T14:54:15Z2008-07-01T00:00:00Zconference objectinfo:eu-repo/semantics/publishedVersionapplication/pdfapplication/pdfhttp://hdl.handle.net/10400.3/2224enginfo:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2025-03-07T10:03:48Zoai:repositorio.uac.pt:10400.3/2224Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-29T00:34:12.072838Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Aerosol Optical Depth measurements in the Azores.
title Aerosol Optical Depth measurements in the Azores.
spellingShingle Aerosol Optical Depth measurements in the Azores.
Carvalho, Fernanda
Aerosol Optical Depth
Terceira Island (Azores)
Azores
title_short Aerosol Optical Depth measurements in the Azores.
title_full Aerosol Optical Depth measurements in the Azores.
title_fullStr Aerosol Optical Depth measurements in the Azores.
title_full_unstemmed Aerosol Optical Depth measurements in the Azores.
title_sort Aerosol Optical Depth measurements in the Azores.
author Carvalho, Fernanda
author_facet Carvalho, Fernanda
Henriques, Diamantino
Fialho, Paulo
author_role author
author2 Henriques, Diamantino
Fialho, Paulo
author2_role author
author
dc.contributor.none.fl_str_mv Repositório da Universidade dos Açores
dc.contributor.author.fl_str_mv Carvalho, Fernanda
Henriques, Diamantino
Fialho, Paulo
dc.subject.por.fl_str_mv Aerosol Optical Depth
Terceira Island (Azores)
Azores
topic Aerosol Optical Depth
Terceira Island (Azores)
Azores
description A preliminary analysis of AOD results from sun-photometer measurements collected at Jose Agostinho Observatory at Angra do Heroísmo (Terceira Island, the Azores) was presented. The observational period ranges from August 2004 to December 2007, using a SP02 sun-photometer at wavelengths 412, 500, 675, and 862 nm, coupled to a 2AXP sun-tracker. The sampling interval is 5 s and data is filtered for cloud contamination in a time window of 10 minutes. Most AOD 500 nm values are below 0.3, showing a small variation during the day; frequency distribution shows a typical right skew distribution. Alpha and beta Angstrom coefficients were also computed and analyzed in the same way. Alpha values are generally positive and lower than 4, while beta values are below 1.5. AOD results from the AERONET station at Horta Observatory (Faial Island, the Azores) were also used and compared with Angra data. AOD and Angstrom coefficients were also analyzed with wind results from the automatic weather station located at both observatories. Results show different wind distributions due to different exposures; however, systematic higher AOD values are found at Horta. The proximity of the two sites indicates that these differences are more likely due to different instruments and processing methods used.
publishDate 2008
dc.date.none.fl_str_mv 2008-07
2008-07-01T00:00:00Z
2013-09-09T12:20:43Z
2013-08-14T14:54:15Z
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url http://hdl.handle.net/10400.3/2224
dc.language.iso.fl_str_mv eng
language eng
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