Type
ArticleKAUST Department
Earth Science and Engineering ProgramPhysical Science and Engineering (PSE) Division
Date
2016-09-30Online Publication Date
2016-09-30Print Publication Date
2017-01Permanent link to this record
http://hdl.handle.net/10754/622721
Metadata
Show full item recordAbstract
The 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.Citation
Zolina 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.Sponsors
The 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.Publisher
American Meteorological SocietyJournal
Journal of HydrometeorologyAdditional Links
http://journals.ametsoc.org/doi/10.1175/JHM-D-16-0048.1ae974a485f413a2113503eed53cd6c53
10.1175/JHM-D-16-0048.1