Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing

Mineral dust aerosols are composed of a complex mixture of silicates, carbonates, oxides, and sulfates. The minerals’ chemical composition and size distribution are vital parameters to evaluate dust environmental impacts. However, the quantification of minerals remains a challenge due to the sparse...

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Main Authors: Sanwlani, Nivedita, Das, Reshmi
Other Authors: Earth Observatory of Singapore
Format: Article
Language:English
Published: 2022
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Online Access:https://hdl.handle.net/10356/160599
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Institution: Nanyang Technological University
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spelling sg-ntu-dr.10356-1605992022-07-30T20:11:24Z Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing Sanwlani, Nivedita Das, Reshmi Earth Observatory of Singapore Satellite Remote Sensing Centre Science::Geology Mineral Dust Aerosol Aerosol Size Distribution Mineral dust aerosols are composed of a complex mixture of silicates, carbonates, oxides, and sulfates. The minerals’ chemical composition and size distribution are vital parameters to evaluate dust environmental impacts. However, the quantification of minerals remains a challenge due to the sparse in situ measurements of dust samples. Here we derive the size-resolved mineralogical composition of airborne dust aerosols from MODIS (Terra and Aqua) satellite-acquired optical measurements and compare it with chemically analyzed elemental (Al, Fe, Ca, Mg) concentrations of aerosols for PM2.5 and PM10 from Chonburi, Chiang Rai, and Bangkok in Thailand, and from Singapore. MODIS-derived mineral retrievals exhibited high correlations with elemental concentrations with R2 ≥ 0.84 for PM2.5 and ≥0.96 for PM10 . High mineral dust activity was detected in the vicinity of biomass-burning areas with gypsum and calcite exhibiting tracer characteristics of combustion. The spatiotemporal pattern of the MODIS-derived minerals matched with Ozone Monitoring Instrument (OMI)-derived dust, sulfates, and carbonaceous aerosols, indicating the model’s consistency. Variation in aerosol loading by ±90% led to deviation in the mineral concentration by <10%. An uncertainty of 6.4% between AERONET-measured and MODIS-derived AOD corresponds to a < ± 2% uncertainty in MODIS-derived mineral concentration, demonstrating the robustness of the model. Ministry of Education (MOE) Published version The in situ chemical analyses of aerosols were supported by a Singapore Ministry of Education (MOE) Tier 1 grant (MOE-NTU_RG125/16-(S)). 2022-07-27T06:18:05Z 2022-07-27T06:18:05Z 2022 Journal Article Sanwlani, N. & Das, R. (2022). Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing. Remote Sensing, 14(3), 761-. https://dx.doi.org/10.3390/rs14030761 2072-4292 https://hdl.handle.net/10356/160599 10.3390/rs14030761 2-s2.0-85124518363 3 14 761 en MOE-NTU_RG125/16-(S) Remote Sensing © 2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https:// creativecommons.org/licenses/by/ 4.0/). application/pdf
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Science::Geology
Mineral Dust Aerosol
Aerosol Size Distribution
spellingShingle Science::Geology
Mineral Dust Aerosol
Aerosol Size Distribution
Sanwlani, Nivedita
Das, Reshmi
Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing
description Mineral dust aerosols are composed of a complex mixture of silicates, carbonates, oxides, and sulfates. The minerals’ chemical composition and size distribution are vital parameters to evaluate dust environmental impacts. However, the quantification of minerals remains a challenge due to the sparse in situ measurements of dust samples. Here we derive the size-resolved mineralogical composition of airborne dust aerosols from MODIS (Terra and Aqua) satellite-acquired optical measurements and compare it with chemically analyzed elemental (Al, Fe, Ca, Mg) concentrations of aerosols for PM2.5 and PM10 from Chonburi, Chiang Rai, and Bangkok in Thailand, and from Singapore. MODIS-derived mineral retrievals exhibited high correlations with elemental concentrations with R2 ≥ 0.84 for PM2.5 and ≥0.96 for PM10 . High mineral dust activity was detected in the vicinity of biomass-burning areas with gypsum and calcite exhibiting tracer characteristics of combustion. The spatiotemporal pattern of the MODIS-derived minerals matched with Ozone Monitoring Instrument (OMI)-derived dust, sulfates, and carbonaceous aerosols, indicating the model’s consistency. Variation in aerosol loading by ±90% led to deviation in the mineral concentration by <10%. An uncertainty of 6.4% between AERONET-measured and MODIS-derived AOD corresponds to a < ± 2% uncertainty in MODIS-derived mineral concentration, demonstrating the robustness of the model.
author2 Earth Observatory of Singapore
author_facet Earth Observatory of Singapore
Sanwlani, Nivedita
Das, Reshmi
format Article
author Sanwlani, Nivedita
Das, Reshmi
author_sort Sanwlani, Nivedita
title Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing
title_short Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing
title_full Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing
title_fullStr Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing
title_full_unstemmed Understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing
title_sort understanding haze: modeling size-resolved mineral aerosol from satellite remote sensing
publishDate 2022
url https://hdl.handle.net/10356/160599
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