Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation

Satellite measurements of backscattered UV radiation are sensitive to the presence of UV-absorbing aerosols in the atmosphere. These measurements are commonly used for determining the concentration of atmospheric trace gases such as O 3 , SO 2 , and H 2 CO. The theoretical results in this dataset de...

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Main Authors: Hiren Jethva, David Haffner, Pawan K. Bhartia, Omar Torres
Format: Other/Unknown Material
Language:English
Published: Zenodo 2022
Subjects:
OMI
Online Access:https://doi.org/10.5281/zenodo.7030280
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record_format openpolar
spelling ftzenodo:oai:zenodo.org:7030280 2024-09-09T18:55:31+00:00 Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation Hiren Jethva David Haffner Pawan K. Bhartia Omar Torres 2022-09-13 https://doi.org/10.5281/zenodo.7030280 eng eng Zenodo https://doi.org/10.5281/zenodo.7030279 https://doi.org/10.5281/zenodo.7030280 oai:zenodo.org:7030280 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Earth and Space Science, (2022-09-13) ULTRAVIOLET RADIANCE AEROSOL ABSORPTION ATMOSPHERIC OZONE Passive Remote Sensing AEROSOL OPTICAL DEPTH/THICKNESS AEROSOL PARTICLE PROPERTIES DUST/ASH/SMOKE OZONE PROFILES TOTAL OZONE Aura OMI info:eu-repo/semantics/other 2022 ftzenodo https://doi.org/10.5281/zenodo.703028010.5281/zenodo.7030279 2024-07-25T21:17:13Z Satellite measurements of backscattered UV radiation are sensitive to the presence of UV-absorbing aerosols in the atmosphere. These measurements are commonly used for determining the concentration of atmospheric trace gases such as O 3 , SO 2 , and H 2 CO. The theoretical results in this dataset describe the effects of UV-absorbing mineral dust and carbonaceous smoke aerosols on these backscatter satellite measurements between 300-400 nm. The information provided is independent of any specific trace gas retrieval algorithm and does not require detailed a priori knowledge of aerosol and surface properties. The results are derived from the analysis of the radiative transfer model simulations performed with the optical property data used in the Ozone Monitoring Instrument (OMI) UV aerosol retrieval algorithm, OMAERUV. Results from this algorithm have been validated with Aerosol Robotic Network (AERONET) observations (Jethva & Torres, 2011; Torres et al., 2018). This dataset is associated with the following publication: Jethva, H., Haffner, D.,Bhartia, P. K., & Torres, O. (2022). Estimating Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation, Earth Space Sci., Accepted. This dataset is a product of research funded by NASA's Science Mission Directorate, WBS 479717, Long Term Measurement of Ozone. Other/Unknown Material Aerosol Robotic Network Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic ULTRAVIOLET RADIANCE
AEROSOL ABSORPTION
ATMOSPHERIC OZONE
Passive Remote Sensing
AEROSOL OPTICAL DEPTH/THICKNESS
AEROSOL PARTICLE PROPERTIES
DUST/ASH/SMOKE
OZONE PROFILES
TOTAL OZONE
Aura
OMI
spellingShingle ULTRAVIOLET RADIANCE
AEROSOL ABSORPTION
ATMOSPHERIC OZONE
Passive Remote Sensing
AEROSOL OPTICAL DEPTH/THICKNESS
AEROSOL PARTICLE PROPERTIES
DUST/ASH/SMOKE
OZONE PROFILES
TOTAL OZONE
Aura
OMI
Hiren Jethva
David Haffner
Pawan K. Bhartia
Omar Torres
Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation
topic_facet ULTRAVIOLET RADIANCE
AEROSOL ABSORPTION
ATMOSPHERIC OZONE
Passive Remote Sensing
AEROSOL OPTICAL DEPTH/THICKNESS
AEROSOL PARTICLE PROPERTIES
DUST/ASH/SMOKE
OZONE PROFILES
TOTAL OZONE
Aura
OMI
description Satellite measurements of backscattered UV radiation are sensitive to the presence of UV-absorbing aerosols in the atmosphere. These measurements are commonly used for determining the concentration of atmospheric trace gases such as O 3 , SO 2 , and H 2 CO. The theoretical results in this dataset describe the effects of UV-absorbing mineral dust and carbonaceous smoke aerosols on these backscatter satellite measurements between 300-400 nm. The information provided is independent of any specific trace gas retrieval algorithm and does not require detailed a priori knowledge of aerosol and surface properties. The results are derived from the analysis of the radiative transfer model simulations performed with the optical property data used in the Ozone Monitoring Instrument (OMI) UV aerosol retrieval algorithm, OMAERUV. Results from this algorithm have been validated with Aerosol Robotic Network (AERONET) observations (Jethva & Torres, 2011; Torres et al., 2018). This dataset is associated with the following publication: Jethva, H., Haffner, D.,Bhartia, P. K., & Torres, O. (2022). Estimating Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation, Earth Space Sci., Accepted. This dataset is a product of research funded by NASA's Science Mission Directorate, WBS 479717, Long Term Measurement of Ozone.
format Other/Unknown Material
author Hiren Jethva
David Haffner
Pawan K. Bhartia
Omar Torres
author_facet Hiren Jethva
David Haffner
Pawan K. Bhartia
Omar Torres
author_sort Hiren Jethva
title Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation
title_short Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation
title_full Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation
title_fullStr Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation
title_full_unstemmed Spectral Effects of Absorbing Aerosols on Backscattered UV Radiation
title_sort spectral effects of absorbing aerosols on backscattered uv radiation
publisher Zenodo
publishDate 2022
url https://doi.org/10.5281/zenodo.7030280
genre Aerosol Robotic Network
genre_facet Aerosol Robotic Network
op_source Earth and Space Science, (2022-09-13)
op_relation https://doi.org/10.5281/zenodo.7030279
https://doi.org/10.5281/zenodo.7030280
oai:zenodo.org:7030280
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.703028010.5281/zenodo.7030279
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