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dc.contributor.authorGrandey, Benjamin S
dc.contributor.authorWang, Chien
dc.date.accessioned2022-03-15T14:02:00Z
dc.date.available2022-03-15T14:02:00Z
dc.date.issued2019
dc.identifier.urihttps://hdl.handle.net/1721.1/141180
dc.description.abstract©2019. The Authors. Using the Community Earth System Model, with the Community Atmosphere Model version 5.3, we investigate the cloud radiative effects of anthropogenic aerosols emitted from different source regions and global shipping. We also analyze aerosol burdens, cloud condensation nuclei concentration, liquid water path, and ice water path. Due to transboundary transport and sublinearity in the response of clouds to aerosols, the cloud radiative effects of emissions from a given source region are influenced by emissions from other source regions. For example, the shortwave cloud radiative effect of shipping is −0.39 ± 0.03 W/m2 when other anthropogenic emissions sources are present (the “present-day background” assumption) compared with −0.60 ± 0.03 W/m2 when other anthropogenic emissions sources are absent (the “natural background” assumption). In general, the cloud radiative effects are weaker if present-day background conditions are assumed compared with if natural background conditions are assumed. Assumptions about background conditions should be carefully considered when investigating the climate impacts of aerosol emissions from a given source region.en_US
dc.language.isoen
dc.publisherAmerican Geophysical Union (AGU)en_US
dc.relation.isversionof10.1029/2018JD029644en_US
dc.rightsCreative Commons Attribution-NonCommercial-NoDerivs Licenseen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/en_US
dc.sourceWileyen_US
dc.titleBackground Conditions Influence the Estimated Cloud Radiative Effects of Anthropogenic Aerosol Emissions From Different Source Regionsen_US
dc.typeArticleen_US
dc.identifier.citationGrandey, Benjamin S and Wang, Chien. 2019. "Background Conditions Influence the Estimated Cloud Radiative Effects of Anthropogenic Aerosol Emissions From Different Source Regions." Journal of Geophysical Research: Atmospheres, 124 (4).
dc.relation.journalJournal of Geophysical Research: Atmospheresen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2022-03-15T13:42:15Z
dspace.orderedauthorsGrandey, BS; Wang, Cen_US
dspace.date.submission2022-03-15T13:42:17Z
mit.journal.volume124en_US
mit.journal.issue4en_US
mit.licensePUBLISHER_CC
mit.metadata.statusAuthority Work and Publication Information Neededen_US


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