Retrieval of aerosol properties from Airborne Hyper-Angular Rainbow Polarimeter (AirHARP) observations during ACEPOL 2017

dc.contributor.authorPuthukkudy, Anin
dc.contributor.authorMartins, J. Vanderlei
dc.contributor.authorRemer, Lorraine A.
dc.contributor.authorXu, Xiaoguang
dc.contributor.authorDubovik, Oleg
dc.contributor.authorLitvinov, Pavel
dc.contributor.authorMcBride, Brent
dc.contributor.authorBurton, Sharon
dc.contributor.authorBarbosa, H. M. J.
dc.date.accessioned2024-06-28T18:09:52Z
dc.date.available2024-06-28T18:09:52Z
dc.date.issued2020-10-05
dc.description.abstractMulti-angle polarimetric (MAP) imaging of Earth scenes can be used for the retrieval of microphysical and optical parameters of aerosols and clouds. The Airborne Hyper-Angular Rainbow Polarimeter (AirHARP) is an aircraft MAP instrument with a hyper-angular imaging capability of 60 along-track viewing angles at 670 nm and 20 along-track viewing angles at other wavelengths – 440, 550, and 870 nm – across the full 114° (94°) along-track (cross-track) field of view. Here we report the retrieval of aerosol properties using the Generalized Retrieval of Aerosols and Surface Properties (GRASP) algorithm applied to AirHARP observations collected during the NASA Aerosol Characterization from Polarimeter and Lidar (ACEPOL) campaign in October–November 2017. The retrieved aerosol properties include spherical fraction (SF), aerosol column concentration in multiple size distribution modes, and, with sufficient aerosol loading, complex aerosol refractive index. From these primary retrievals, we derive aerosol optical depth (AOD), Angstrom exponent (AE), and single scattering albedo (SSA). AODs retrieved from AirHARP measurements are compared with the High Spectral Resolution LiDAR-2 (HSRL2) AOD measurements at 532 nm and validated with measurements from collocated Aerosol Robotic NETwork (AERONET) stations. A good agreement with HSRL2 (ρ=0.940, |BIAS|=0.062, mean absolute error (MAE) = 0.122) and AERONET AOD (0.010 <= MAE <= 0.015, 0.002 <= |BIAS| <= 0.009) measurements is observed for the collocated points. There was a mismatch between the HSRL2- and AirHARP-retrieved AOD for the pixels close to the forest fire smoke source and to the edges of the plume due to spatial mismatch in the sampling. This resulted in a higher BIAS and MAE for the HSRL2 AOD comparison. For the case of AERONET AOD comparison, two different approaches are used in the GRASP retrievals, and the simplified aerosol component-based GRASP/Models kernel which retrieves fewer number of aerosol parameter performed well compared to a more generous GRASP/Five mode approach in the low aerosol loading cases. Forest fire smoke intercepted during ACEPOL provided a situation with homogenous plume and sufficient aerosol loading to retrieve the real part of the refractive index (RRI) of 1.55 and the imaginary part of the refractive index (IRI) of 0.024. The derived SSAs for this case are 0.87, 0.86, 0.84, and 0.81 at wavelengths of 440, 550, 670, and 870 nm, respectively. Finer particles with an average AE of 1.53, a volume median radius of 0.157µm, and a standard deviation (SD) of 0.55 for fine mode is observed for the same smoke plume. These results serve as a proxy for the scale and detail of aerosol retrievals that are anticipated from future space mission data, as HARP CubeSat (mission begins 2020) and HARP2 (aboard the NASA PACE mission with launch in 2023) are near duplicates of AirHARP and are expected to provide the same level of aerosol characterization.
dc.description.sponsorshipThis research is primarily supported through NASA projects HARP CubeSat (grant no. NNX13AN11G), AirHARP (grant no. NNX16AK36G), and JCET cooperative agreement (grant no. NNX15AT34A). This research is also supported by the National Key R&D Program of China (grant no. 2016YFE0201400). Oleg Dubovik appreciates the support from the Chemical and Physical Properties of the Atmosphere Project funded by the French National Research Agency through the Programme d’Investissement d’Avenir (contract no. ANR-11-LABX0 0 05-01), the Regional Council “Hauts-de-France”, and the “European Funds for Regional Economic Development”. Henrique M. J. Barbosa is grateful for the support of Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) (processo no. 2016/18866-2) and Conselho Nacional de Desenvolvimento Cien tífico e Tecnológico (CNPq) (project no. 308682/2017-3). The Dutch contribution to the ACEPOL flight campaign hours was funded by the SRON Netherlands Institute for SPACE Research and by NSO/NWO (project no. ALW-GO/16-09).
dc.description.urihttps://amt.copernicus.org/articles/13/5207/2020/
dc.format.extent30 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2wmth-8o9u
dc.identifier.citationPuthukkudy, Anin, J. Vanderlei Martins, Lorraine A. Remer, Xiaoguang Xu, Oleg Dubovik, Pavel Litvinov, Brent McBride, Sharon Burton, and Henrique M. J. Barbosa. “Retrieval of Aerosol Properties from Airborne Hyper-Angular Rainbow Polarimeter (AirHARP) Observations during ACEPOL 2017.” Atmospheric Measurement Techniques 13, no. 10 (October 5, 2020): 5207–36. https://doi.org/10.5194/amt-13-5207-2020.
dc.identifier.urihttps://doi.org/10.5194/amt-13-5207-2020
dc.identifier.urihttp://hdl.handle.net/11603/34758
dc.language.isoen_US
dc.publisherEGU
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Faculty Collection
dc.relation.ispartofUMBC Physics Department
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology (JCET)
dc.relation.ispartofUMBC Geography and Environmental Systems Department
dc.relation.ispartofUMBC GESTAR II
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.titleRetrieval of aerosol properties from Airborne Hyper-Angular Rainbow Polarimeter (AirHARP) observations during ACEPOL 2017
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0002-7371-2338
dcterms.creatorhttps://orcid.org/0000-0003-4333-533X
dcterms.creatorhttps://orcid.org/0000-0001-9583-980X
dcterms.creatorhttps://orcid.org/0000-0002-3138-9341
dcterms.creatorhttps://orcid.org/0000-0002-4027-1855

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