The Relationship Between the Saharan Air Layer, Convective Environmental Conditions, and Precipitation in Puerto Rico

dc.contributor.authorMiller, Paul W.en
dc.contributor.authorRamseyer, Craig A.en
dc.date.accessioned2024-02-19T18:09:21Zen
dc.date.available2024-02-19T18:09:21Zen
dc.date.issued2024-01-04en
dc.description.abstractThe Saharan Air Layer (SAL) is a hot, dry, and dust-laden feature that advects large concentrations of dust across the Atlantic annually to destination regions in the Americas and Caribbean. However, recent work has suggested the SAL may be a contributing factor to high-impact drought in the Caribbean basin. While the SAL's characteristic dust loadings have been the focus of much previous research, fewer efforts have holistically engaged the co-evolution of the dust plume, its associated convective environment, and resultant rainfall in Caribbean islands. This study employs a self-organizing map (SOM) classification to identify the common trans-Atlantic dust transport typologies associated with the SAL during June and July 1981–2020. Using the column-integrated dust flux, termed integrated dust transport (IDT), from MERRA-2 reanalysis as a SAL proxy, the SOM resolved two common patterns which resembled trans-Atlantic SAL outbreaks. During these events, the convective environment associated with the SAL, as inferred by the Gálvez-Davison Index, becomes less conducive to precipitation as the SAL migrates further away from the west African coast. Simultaneously, days with IDT patterns grouped to the SAL outbreak typologies demonstrate island-wide negative precipitation anomalies in Puerto Rico. The SOM's most distinctive SAL outbreak pattern has experienced a statistically significant increase during the 40-year study period, becoming roughly 10% more frequent over that time. These results are relevant for both climate scientists and water managers wishing to better anticipate Caribbean droughts on both the long and short terms.en
dc.description.versionAccepted versionen
dc.format.extent14 page(s)en
dc.format.mimetypeapplication/pdfen
dc.identifierARTN e2023JD039681 (Article number)en
dc.identifier.doihttps://doi.org/10.1029/2023JD039681en
dc.identifier.eissn2169-8996en
dc.identifier.issn2169-897Xen
dc.identifier.issue1en
dc.identifier.orcidRamseyer, Craig [0000-0003-0290-4639]en
dc.identifier.urihttps://hdl.handle.net/10919/118034en
dc.identifier.volume129en
dc.language.isoenen
dc.publisherAmerican Geophysical Unionen
dc.rightsIn Copyrighten
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en
dc.subjectSaharan air layeren
dc.subjectconvective precipitationen
dc.subjecteastern Caribbeanen
dc.subjectdroughten
dc.titleThe Relationship Between the Saharan Air Layer, Convective Environmental Conditions, and Precipitation in Puerto Ricoen
dc.title.serialJournal of Geophysical Research-Atmospheresen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten
dc.type.otherArticleen
dc.type.otherJournalen
pubs.organisational-group/Virginia Techen
pubs.organisational-group/Virginia Tech/Natural Resources & Environmenten
pubs.organisational-group/Virginia Tech/Natural Resources & Environment/Geographyen
pubs.organisational-group/Virginia Tech/Natural Resources & Environment/Geography/Geography T&R facultyen
pubs.organisational-group/Virginia Tech/All T&R Facultyen
pubs.organisational-group/Virginia Tech/Natural Resources & Environment/CNRE T&R Facultyen

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