Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals

The sub-micron (SM) aerosol optical depth (AOD) is an optical separation based on the fraction of particles below a specified cutoff radius of the particle size distribution (PSD) at a given particle radius. It is fundamentally different from spectrally separated FM (fine-mode) AOD. We present a sim...

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Published in:Atmospheric Measurement Techniques
Main Authors: N. T. O'Neill, K. Ranjbar, L. Ivănescu, T. F. Eck, J. S. Reid, D. M. Giles, D. Pérez-Ramírez, J. P. Chaubey
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/amt-16-1103-2023
https://doaj.org/article/60f65ad75a144662b6feff39fc0646a8
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spelling ftdoajarticles:oai:doaj.org/article:60f65ad75a144662b6feff39fc0646a8 2023-05-15T15:14:40+02:00 Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals N. T. O'Neill K. Ranjbar L. Ivănescu T. F. Eck J. S. Reid D. M. Giles D. Pérez-Ramírez J. P. Chaubey 2023-03-01T00:00:00Z https://doi.org/10.5194/amt-16-1103-2023 https://doaj.org/article/60f65ad75a144662b6feff39fc0646a8 EN eng Copernicus Publications https://amt.copernicus.org/articles/16/1103/2023/amt-16-1103-2023.pdf https://doaj.org/toc/1867-1381 https://doaj.org/toc/1867-8548 doi:10.5194/amt-16-1103-2023 1867-1381 1867-8548 https://doaj.org/article/60f65ad75a144662b6feff39fc0646a8 Atmospheric Measurement Techniques, Vol 16, Pp 1103-1120 (2023) Environmental engineering TA170-171 Earthwork. Foundations TA715-787 article 2023 ftdoajarticles https://doi.org/10.5194/amt-16-1103-2023 2023-03-05T01:30:39Z The sub-micron (SM) aerosol optical depth (AOD) is an optical separation based on the fraction of particles below a specified cutoff radius of the particle size distribution (PSD) at a given particle radius. It is fundamentally different from spectrally separated FM (fine-mode) AOD. We present a simple (AOD-normalized) SM fraction versus FM fraction (SMF vs. FMF) linear equation that explains the well-recognized empirical result of SMF generally being greater than the FMF. The AERONET inversion (AERinv) products (combined inputs of spectral AOD and sky radiance) and the spectral deconvolution algorithm (SDA) products (input of AOD spectra) enable, respectively, an empirical SMF vs. FMF comparison at similar (columnar) remote sensing scales across a variety of aerosol types. SMF (AERinv-derived) vs. FMF (SDA-derived) behavior is primarily dependent on the relative truncated portion ( ε c ) of the coarse-mode (CM) AOD associated with the cutoff portion of the CM PSD and, to a second order, the cutoff FM PSD and FM AOD ( ε f ). The SMF vs. FMF equation largely explains the SMF vs. FMF behavior of the AERinv vs. SDA products as a function of PSD cutoff radius (“inflection point”) across an ensemble of AERONET sites and aerosol types (urban-industrial, biomass burning, dust, maritime and a mixed class of Arctic aerosols). The overarching dynamic was that the linear SMF vs. FMF relation pivots clockwise about the approximate (SMF, FMF) singularity of (1, 1) in a “linearly inverse” fashion (slope and intercept of approximately 1− ε c and ε c ) with increasing cutoff radius. SMF vs. FMF slopes and intercepts derived from AERinv and SDA retrievals confirmed the general domination of ε c over ε f in controlling that dynamic. A more general conclusion is the apparent confirmation that the optical impact of truncating modal (whole) PSD features can be detected by an SMF vs. FMF analysis. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Atmospheric Measurement Techniques 16 4 1103 1120
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
spellingShingle Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
N. T. O'Neill
K. Ranjbar
L. Ivănescu
T. F. Eck
J. S. Reid
D. M. Giles
D. Pérez-Ramírez
J. P. Chaubey
Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals
topic_facet Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
description The sub-micron (SM) aerosol optical depth (AOD) is an optical separation based on the fraction of particles below a specified cutoff radius of the particle size distribution (PSD) at a given particle radius. It is fundamentally different from spectrally separated FM (fine-mode) AOD. We present a simple (AOD-normalized) SM fraction versus FM fraction (SMF vs. FMF) linear equation that explains the well-recognized empirical result of SMF generally being greater than the FMF. The AERONET inversion (AERinv) products (combined inputs of spectral AOD and sky radiance) and the spectral deconvolution algorithm (SDA) products (input of AOD spectra) enable, respectively, an empirical SMF vs. FMF comparison at similar (columnar) remote sensing scales across a variety of aerosol types. SMF (AERinv-derived) vs. FMF (SDA-derived) behavior is primarily dependent on the relative truncated portion ( ε c ) of the coarse-mode (CM) AOD associated with the cutoff portion of the CM PSD and, to a second order, the cutoff FM PSD and FM AOD ( ε f ). The SMF vs. FMF equation largely explains the SMF vs. FMF behavior of the AERinv vs. SDA products as a function of PSD cutoff radius (“inflection point”) across an ensemble of AERONET sites and aerosol types (urban-industrial, biomass burning, dust, maritime and a mixed class of Arctic aerosols). The overarching dynamic was that the linear SMF vs. FMF relation pivots clockwise about the approximate (SMF, FMF) singularity of (1, 1) in a “linearly inverse” fashion (slope and intercept of approximately 1− ε c and ε c ) with increasing cutoff radius. SMF vs. FMF slopes and intercepts derived from AERinv and SDA retrievals confirmed the general domination of ε c over ε f in controlling that dynamic. A more general conclusion is the apparent confirmation that the optical impact of truncating modal (whole) PSD features can be detected by an SMF vs. FMF analysis.
format Article in Journal/Newspaper
author N. T. O'Neill
K. Ranjbar
L. Ivănescu
T. F. Eck
J. S. Reid
D. M. Giles
D. Pérez-Ramírez
J. P. Chaubey
author_facet N. T. O'Neill
K. Ranjbar
L. Ivănescu
T. F. Eck
J. S. Reid
D. M. Giles
D. Pérez-Ramírez
J. P. Chaubey
author_sort N. T. O'Neill
title Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals
title_short Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals
title_full Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals
title_fullStr Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals
title_full_unstemmed Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals
title_sort relationship between the sub-micron fraction (smf) and fine-mode fraction (fmf) in the context of aeronet retrievals
publisher Copernicus Publications
publishDate 2023
url https://doi.org/10.5194/amt-16-1103-2023
https://doaj.org/article/60f65ad75a144662b6feff39fc0646a8
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Atmospheric Measurement Techniques, Vol 16, Pp 1103-1120 (2023)
op_relation https://amt.copernicus.org/articles/16/1103/2023/amt-16-1103-2023.pdf
https://doaj.org/toc/1867-1381
https://doaj.org/toc/1867-8548
doi:10.5194/amt-16-1103-2023
1867-1381
1867-8548
https://doaj.org/article/60f65ad75a144662b6feff39fc0646a8
op_doi https://doi.org/10.5194/amt-16-1103-2023
container_title Atmospheric Measurement Techniques
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container_start_page 1103
op_container_end_page 1120
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