Regional Hydrological Cycle over the Red Sea in ERA-Interim

Olga Zolina, Ambroise Dufour, Sergey K. Gulev, Georgiy L. Stenchikov

Research output: Contribution to journalArticlepeer-review

25 Scopus citations


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.
Original languageEnglish (US)
Pages (from-to)65-83
Number of pages19
JournalJournal of Hydrometeorology
Issue number1
StatePublished - Sep 30 2016

Bibliographical note

KAUST Repository Item: Exported on 2020-10-01
Acknowledgements: 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.


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