Shortwave direct radiative effects of above-cloud aerosols over global oceans derived from 8 years of CALIOP and MODIS observations

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dc.contributor.authorZhang, Zhibo
dc.contributor.authorMeyer, Kerry
dc.contributor.authorYu, Hongbin
dc.contributor.authorPlatnick, Steven
dc.contributor.authorColarco, Peter
dc.contributor.authorLiu, Zhaoyan
dc.contributor.authorOreopoulos, Lazaros
dc.date.accessioned2018-10-15T13:53:34Z
dc.date.available2018-10-15T13:53:34Z
dc.date.issued2016-03-04
dc.description.abstractIn this paper, we studied the frequency of occurrence and shortwave direct radiative effects (DREs) of above-cloud aerosols (ACAs) over global oceans using 8 years (2007–2014) of collocated CALIOP and MODIS observations. Similar to previous work, we found high ACA occurrence in four regions: southeastern (SE) Atlantic region, where ACAs are mostly light-absorbing aerosols, i.e., smoke and polluted dust according to CALIOP classification, originating from biomass burning over the African Savanna; tropical northeastern (TNE) Atlantic and the Arabian Sea, where ACAs are predominantly windblown dust from the Sahara and Arabian deserts, respectively; and the northwestern (NW) Pacific, where ACAs are mostly transported smoke and polluted dusts from Asian. From radiative transfer simulations based on CALIOP–MODIS observations and a set of the preselected aerosol optical models, we found the DREs of ACAs at the top of atmosphere (TOA) to be positive (i.e., warming) in the SE Atlantic and NW Pacific regions, but negative (i.e., cooling) in the TNE Atlantic Ocean and the Arabian Sea. The cancellation of positive and negative regional DREs results in a global ocean annual mean diurnally averaged cloudy-sky DRE of 0.015Wm⁻² (range of −0.03 to 0.06Wm⁻²) at TOA. The DREs at surface and within the atmosphere are −0.15Wm⁻² (range of −0.09 to −0.21Wm⁻²), and 0.17Wm⁻² (range of 0.11 to 0.24Wm⁻²), respectively. The regional and seasonal mean DREs are much stronger. For example, in the SE Atlantic region, the JJA (July–August) seasonal mean cloudy-sky DRE is about 0.7Wm⁻² (range of 0.2 to 1.2Wm⁻²) at TOA. All our DRE computations are publicly available¹. The uncertainty in our DRE computations is mainly caused by the uncertainties in the aerosol optical properties, in particular aerosol absorption, the uncertainties in the CALIOP operational aerosol optical thickness retrieval, and the ignorance of cloud and potential aerosol diurnal cycle. In situ and remotely sensed measurements of ACA from future field campaigns and satellite missions and improved lidar retrieval algorithm, in particular vertical feature masking, would help reduce the uncertainty.en_US
dc.description.urihttps://www.atmos-chem-phys.net/16/2877/2016/en_US
dc.format.extent24 pagesen_US
dc.genreJournal Articleen_US
dc.identifierdoi:10.13016/M24X54M0T
dc.identifier.citationZhang, Z., Meyer, K., Yu, H., Platnick, S., Colarco, P., Liu, Z., and Oreopoulos, L.: Shortwave direct radiative effects of above-cloud aerosols over global oceans derived from 8 years of CALIOP and MODIS observations, Atmos. Chem. Phys., 16, 2877-2900, https://doi.org/10.5194/acp-16-2877-2016, 2016.en_US
dc.identifier.urihttps://doi.org/10.5194/acp-16-2877-2016
dc.identifier.urihttp://hdl.handle.net/11603/11539
dc.language.isoen_USen_US
dc.publisherCopernicus Publications on behalf of the European Geosciences Unionen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology
dc.relation.ispartofUMBC Physics Department
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author.
dc.rightsAttribution 3.0 Unported (CC BY 3.0)*
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/*
dc.subjectUMBC High Performance Computing Facility (HPCF)en_US
dc.subjectshortwave direct radiative effects (DREs)
dc.subjectabovecloud aerosols (ACAs)
dc.subjectCALIOP and MODIS observations
dc.titleShortwave direct radiative effects of above-cloud aerosols over global oceans derived from 8 years of CALIOP and MODIS observationsen_US
dc.typeTexten_US

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