Identification of major moisture sources across the Mediterranean Basin

• Published in: Climate Dynamics
• Main Authors: Batibeniz, Fulden, Ashfaq, Moetasim, Önol, Barış, Turuncoglu, Ufuk Utku, Mehmood, Shahid, Evans, Katherine J.
• Other Authors: U.S. Department of Energy, Türkiye Bilimsel ve Teknolojik Araştirma Kurumu, Bilimsel Araştirma Projeleri Birimi, Istanbul Üniversitesi, National Science Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Science and Business Media LLC 2020
• Subjects: Atmospheric Science; North Atlantic; North Atlantic oscillation
• Online Access: http://dx.doi.org/10.1007/s00382-020-05224-3; http://link.springer.com/content/pdf/10.1007/s00382-020-05224-3.pdf; http://link.springer.com/article/10.1007/s00382-020-05224-3/fulltext.html

Abstract We employ a Lagrangian based moisture back trajectory method on an ensemble of four reanalysis datasets to provide a comprehensive understanding of moisture sources over the Mediterranean land region (30° N–49.5° N and 9.75° W–61.5° E) at seasonal timescales for 1980–2013 period. Using a source region between 10° S–71.35° N along the latitude and 80° W–84.88° E along the longitude that is subdivided into ten complimentary sub-regions, our analyses is able to backtrack up to > 90% of seasonal precipitation at each grid point within the target region. Our results indicate a significant role of moisture advected from the North Atlantic and Mediterranean Sea, and locally recycled moisture over the target region in shaping the spatial organization of seasonal precipitation. However, a clear east–west contrast is witnessed in determining the relative importance of each of these major moisture sources where the North Atlantic dictates the moisture supply over the western Mediterranean while moisture from Mediterranean Sea and local recycling play a key role over the eastern Mediterranean. Our analyses also demonstrate a major footprint of the North Atlantic Oscillation (NAO) on precipitation variability over the Mediterranean land as dynamic and thermodynamic anomalies during the negative phase of NAO match with those during wet years and vice versa. The findings reported here are generally consistent across the four reanalysis datasets. Overall, this study establishes the relative roles of adjacent and far-off oceanic and terrestrial evaporative sources over the Mediterranean land and should help in understanding the drivers of precipitation variability and change at varying timescales.