Correlation of aerosol optical properties with surface meteorological parameters over Manila
Aerosol optical properties such as aerosol optical depth (AOD) at 500 nm together with wavelength exponent (α) and Ångstrom turbidity coefficient (β) obtained from a sunphotometer over Manila were used to analyze their response to the changes in temperature, relative humidity (RH) and zonal wind. Da...
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oai:animorepository.dlsu.edu.ph:faculty_research-24472021-06-28T07:52:31Z Correlation of aerosol optical properties with surface meteorological parameters over Manila Vergara, Rhonalyn L. Macalalad, Ernest P. Bagtasa, Gerry Vallar, Edgar A. Galvez, Maria Cecilia D. Francisco, Raquel V. Aerosol optical properties such as aerosol optical depth (AOD) at 500 nm together with wavelength exponent (α) and Ångstrom turbidity coefficient (β) obtained from a sunphotometer over Manila were used to analyze their response to the changes in temperature, relative humidity (RH) and zonal wind. Data retrieved for a one year period of measurements (August 2009-July 2010) were used to describe the variations of the aerosol optical properties. Temperature showed weak correlations with the aerosol optical properties. Surface RH confirmed evidence for its influence on aerosols size distribution and dominant aerosol type. Zonal wind demonstrated influences on the prevailing aerosol present at a certain area and caused alteration the amount of its loading. © 2017 American Scientific Publishers. All rights reserved. 2017-03-01T08:00:00Z text text/html https://animorepository.dlsu.edu.ph/faculty_research/1448 https://animorepository.dlsu.edu.ph/context/faculty_research/article/2447/type/native/viewcontent Faculty Research Work Animo Repository Atmospheric aerosols Astronomical photometry Atmospheric turbidity Physics |
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Atmospheric aerosols Astronomical photometry Atmospheric turbidity Physics Vergara, Rhonalyn L. Macalalad, Ernest P. Bagtasa, Gerry Vallar, Edgar A. Galvez, Maria Cecilia D. Francisco, Raquel V. Correlation of aerosol optical properties with surface meteorological parameters over Manila |
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Aerosol optical properties such as aerosol optical depth (AOD) at 500 nm together with wavelength exponent (α) and Ångstrom turbidity coefficient (β) obtained from a sunphotometer over Manila were used to analyze their response to the changes in temperature, relative humidity (RH) and zonal wind. Data retrieved for a one year period of measurements (August 2009-July 2010) were used to describe the variations of the aerosol optical properties. Temperature showed weak correlations with the aerosol optical properties. Surface RH confirmed evidence for its influence on aerosols size distribution and dominant aerosol type. Zonal wind demonstrated influences on the prevailing aerosol present at a certain area and caused alteration the amount of its loading. © 2017 American Scientific Publishers. All rights reserved. |
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text |
author |
Vergara, Rhonalyn L. Macalalad, Ernest P. Bagtasa, Gerry Vallar, Edgar A. Galvez, Maria Cecilia D. Francisco, Raquel V. |
author_facet |
Vergara, Rhonalyn L. Macalalad, Ernest P. Bagtasa, Gerry Vallar, Edgar A. Galvez, Maria Cecilia D. Francisco, Raquel V. |
author_sort |
Vergara, Rhonalyn L. |
title |
Correlation of aerosol optical properties with surface meteorological parameters over Manila |
title_short |
Correlation of aerosol optical properties with surface meteorological parameters over Manila |
title_full |
Correlation of aerosol optical properties with surface meteorological parameters over Manila |
title_fullStr |
Correlation of aerosol optical properties with surface meteorological parameters over Manila |
title_full_unstemmed |
Correlation of aerosol optical properties with surface meteorological parameters over Manila |
title_sort |
correlation of aerosol optical properties with surface meteorological parameters over manila |
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Animo Repository |
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2017 |
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https://animorepository.dlsu.edu.ph/faculty_research/1448 https://animorepository.dlsu.edu.ph/context/faculty_research/article/2447/type/native/viewcontent |
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1703981056564133888 |