English הצהרה מפת האתר ארועים צור קשר דף הבית  
דף הבית מכוני מחקר ותשתיות המכון הלאומי לאוקיאנוגרפיה חוקרי המכון אליהו ביטון

National Institute of Oceanography 

Eliyahu Biton

Tel: 04 – 8565249


Ph.D. 2011, Weizmann Institute of Science, Israel
At IOLR since 2011

Research interests:
Studies on dynamics of convectively driven marginal seas, sea strait physics, small scale oceanic processes such as density currents and open ocean convection, and air-sea interactions. In particular, over the past several years I have been using oceanic models at various complexities (oceanic general circulation model, box model, hydraulic models for sea straits) combined with different oceanic measurements/proxies to study the dynamics of the Red Sea (during the last 20,000 years) and of the Gulf of Eilat.

Selected publications:
Biton, E., and Gildor, H. (2011). The coupling between exchange flux through a strait and dynamics in a small convectively driven marginal sea: The Gulf of Aqaba (Gulf of Eilat). J. Geophys. Res., doi:10.1029/2011JC006944.

Biton, E., and Gildor, H. (2011). Stepwise seasonal restratification and the evolution of salinity minimum in the Gulf of Aqaba (Gulf of Eilat). J. Geophys. Res ., doi:10.1029/2011JC007106, in press.

Biton, E., and Gildor, H. (2011). The general circulation of the Gulf of Aqaba (Gulf of Eilat) revisited: The interplay between the exchange flow through the Straits of Tiran and surface fluxes. J. Geophys. Res ., doi:10.1029/2010JC006860, in press.

Biton, E., Gildor, H., Trommer, G., Siccha, M., Kucera, M., Van der Meer, M. T. J., and Schouten, S. (2010). Sensitivity of Red Sea circulation to monsoonal variability during the Holocene: An integrated data and modeling study. Paleoceanography , 25, PA4209, doi:10.1029/2009PA001876.

Biton E., Silverman, J., and Gildor, H. (2008). Observations and modeling of a pulsating density current. Geophys. Res. Lett ., 35, L14603, doi:10.1029/2008GL034123.

Biton, E., Gildor, H., and Peltier, W. R. (2008). Red Sea circulation during the Last Glacial Maximum: Implication for sea level reconstruction. Paleoceanography. 23, PA1214, doi:10.1029/2007PA001431.
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