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dc.contributor.authorZolina, Olga
dc.contributor.authorDufour, Ambroise
dc.contributor.authorGulev, Sergey K.
dc.contributor.authorStenchikov, Georgiy L.
dc.date.accessioned2017-01-24T08:30:07Z
dc.date.available2017-01-24T08:30:07Z
dc.date.issued2016-09-30
dc.identifier.citationZolina O, Dufour A, Gulev SK, Stenchikov G (2017) Regional Hydrological Cycle over the Red Sea in ERA-Interim. Journal of Hydrometeorology 18: 65–83. Available: http://dx.doi.org/10.1175/JHM-D-16-0048.1.
dc.identifier.issn1525-755X
dc.identifier.issn1525-7541
dc.identifier.doi10.1175/JHM-D-16-0048.1
dc.identifier.urihttp://hdl.handle.net/10754/622721
dc.description.abstractThe major sources of atmospheric moisture over the Red Sea are analyzed using ERA-Interim for the 1979-2013 period. The vertical structure of moisture transports across the coastlines has been computed separately for the western and eastern coasts of the Red Sea. The vertical structure of the moisture transport from the Red Sea to the continents is dominated by a breeze-like circulation in the near-surface layer and the Arabian high above 850 hPa. The lower-layer, breeze-like circulation is acting to export the moisture to the northwest of Africa and to the Arabian Peninsula and contributes about 80% of the moisture exports from the Red Sea, dominating over the transport in the upper layer, where the moisture is advected to the Arabian Peninsula in the northern part of the sea and to the African continent in the southern part. Integrated moisture divergence over the Red Sea decreased from the early 1980s to 1997 and then increased until the 2010s. Associated changes in the moisture export were provided primarily by the increasing intensity of the breeze-associated transports. The transports above the boundary layer, while being strong across the western and the eastern coasts, have a smaller effect on the net moisture export. The interannual variability of the moisture export in the near-surface layer was found to be closely correlated with the variability in sea surface temperature, especially in summer. Implications of the observed changes in the moisture advection for the hydrological cycle of the Middle East are discussed.
dc.description.sponsorshipThe ERA-Interim data were made available courtesy of ECMWF. The suggestions and criticisms of the two anonymous reviewers regarding the first version of themanuscript are greatly appreciated. This work was supported by CNRS/Laboratoire de Glaciologie etGéophysique de l'Environnement (LGGE) and Université Grenoble Alpes (UGA) through the CNRS Chair of Excellence Programme. We also appreciate the support from the King Abdullah University of Science and Technology (KAUST) for G.S. and for O.Z. during her sabbatical visit. O.Z. also benefited from the support of Russian Science Foundation Grant 14-50-00095 and S.K.G. from the Russian Science Foundation Grant 14-17-00697.
dc.publisherAmerican Meteorological Society
dc.relation.urlhttp://journals.ametsoc.org/doi/10.1175/JHM-D-16-0048.1
dc.rights© Copyright [date of publication] American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. All AMS journals and monograph publications are registered with the Copyright Clearance Center (http://www.copyright.com). Questions about permission to use materials for which AMS holds the copyright can also be directed to the AMS Permissions Officer at permissions@ametsoc.org. Additional details are provided in the AMS Copyright Policy statement, available on the AMS website (http://www.ametsoc.org/CopyrightInformation).
dc.subjectHydrologic cycle
dc.subjectMoisture/moisture budget
dc.subjectRegional effects
dc.titleRegional Hydrological Cycle over the Red Sea in ERA-Interim
dc.typeArticle
dc.contributor.departmentEarth Science and Engineering Program
dc.contributor.departmentPhysical Science and Engineering (PSE) Division
dc.identifier.journalJournal of Hydrometeorology
dc.eprint.versionPublisher's Version/PDF
dc.contributor.institutionLaboratoire de Glaciologie et Géophysique de l'Environnement, Grenoble, France
dc.contributor.institutionP. P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russian Federation
kaust.personStenchikov, Georgiy L.
refterms.dateFOA2017-06-21T00:00:00Z
dc.date.published-online2016-09-30
dc.date.published-print2017-01


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