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dc.contributor.authorCuevas, E.
dc.contributor.authorGómez-Peláez, A.J.
dc.contributor.authorRodríguez, S.
dc.contributor.authorTerradellas, E.
dc.contributor.authorBasart, S.
dc.contributor.authorGarcía, R.D.
dc.contributor.authorGarcía, O.E.
dc.contributor.authorAlonso-Pérez, S.
dc.contributor.otherBarcelona Supercomputing Center
dc.date.accessioned2017-10-11T10:01:04Z
dc.date.available2017-10-11T10:01:04Z
dc.date.issued2017-10
dc.identifier.citationCuevas, E. [et al.]. The pulsating nature of large-scale Saharan dust transport as a result of interplays between mid-latitude Rossby waves and the North African Dipole Intensity. "Atmospheric Environment", Octubre 2017, vol. 167, p. 586-602.
dc.identifier.issn1352-2310
dc.identifier.urihttp://hdl.handle.net/2117/108640
dc.description.abstractIt was previously shown that during August the export of Saharan dust to the Atlantic was strongly affected by the difference of the 700-hPa geopotential height anomaly between the subtropics and the tropics over North Africa, which was termed the North African Dipole Intensity (NAFDI). In this work a more comprehensive analysis of the NAFDI is performed, focusing on the entire summer dust season (June–September), and examining the interactions between the mid-latitude Rossby waves (MLRWs) and NAFDI. Widespread and notable aerosol optical depth (AOD) monthly anomalies are found for each NAFDI-phase over the dust corridors off the Sahara, indicating that NAFDI presents intra-seasonal variability and drives dust transport over both the Mediterranean basin and the North Atlantic. Those summer months with the same NAFDI-phase show similar AOD-anomaly patterns. Variations in NAFDI-phase also control the displacement of the Saharan Heat Low (SHL) westwards or eastwards through horizontal advection of temperature over Morocco-Western Sahara or eastern Algeria-Western Libya, respectively. The connection between the SHL and the NAFDI is quantified statistically by introducing two new daily indexes that account for their respective phases (NAFDI daily index -NAFDIDI-, and SHL longitudinal shift index -SHLLSI-) and explained physically using the energy equation of the atmospheric dynamics. The Pearson's correlation coefficient between the one–day-lag SHLLSI and the NAFDIDI for an extended summer season (1980–2013) is 0.78. A positive NAFDI is associated with the West-phase of the SHL, dust sources intensification on central Algeria, and positive AOD anomalies over this region and the Subtropical North Atlantic. A negative NAFDI is associated with the East-phase of the SHL, and positive AOD anomalies over central-eastern Sahara and the central-western Mediterranean Sea. The results point out that the phase changes of NAFDI at intra-seasonal time scale are conducted by those MLRWs that penetrate deeply into the low troposphere.
dc.description.sponsorshipThis work is part of the research activities developed by the WMO SDS-WAS Regional Centre for Northern Africa, Middle East and Europe, held by AEMET and BSC-CNS. This study also contributes to Copernicus Atmosphere Monitoring Service (CAMS). Our acknowledgment to ECMWF for providing MACC-dust reanalysis. The authors wish to thank NCEP/NCAR Reanalysis Project. We acknowledge NASA LADS for providing MODIS data. The University of Granada (Spain) and its “Physics and Space Sciences” PhD Programme are acknowledged by A. J. Gómez-Peláez and E. Cuevas. AEROATLAN project (CGL2015-17 66229-P), co-funded by the Ministry of Economy and Competitiveness of Spain and the European Regional Development Fund contributed to this study. Sara Basart acknowledges the CICYT project (CGL2013-46736).
dc.format.extent17 p.
dc.language.isoeng
dc.publisherElsevier
dc.rightsAttribution-NonCommercial-NoDerivs 4.0 Spain
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/es/
dc.subjectÀrees temàtiques de la UPC::Energies
dc.subject.lcshDust--adverse effects
dc.subject.lcshSahara--Climate
dc.subject.otherSaharan dust
dc.subject.otherNorth African Dipole Intensity (NAFDI)
dc.subject.otherSaharan Heat Low (SHL)
dc.titleThe pulsating nature of large-scale Saharan dust transport as a result of interplays between mid-latitude Rossby waves and the North African Dipole Intensity
dc.typeArticle
dc.subject.lemacDeserts--Àfrica del Nord
dc.subject.lemacSàhara
dc.identifier.doi10.1016/j.atmosenv.2017.08.059
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttp://www.sciencedirect.com/science/article/pii/S1352231017305757
dc.rights.accessOpen Access
dc.description.versionPostprint (author's final draft)
dc.relation.projectidinfo:eu-repo/grantAgreement/MINECO/1PE/CGL2015-17-66229-P
dc.relation.projectidinfo:eu-repo/grantAgreement/MINECO/1PE/CGL2013-46736
upcommons.citation.publishedtrue
upcommons.citation.publicationNameAtmospheric Environment
upcommons.citation.volume167
upcommons.citation.startingPage586
upcommons.citation.endingPage602


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