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Geostrophic current patterns off the Egyptian Mediterranean coast

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Using objectively analysed hydrographic data, currents have been calculated off the Egyptian Mediterranean coast at the surface and at 30, 50, 75, 100, 200 and 300 m depths for the four seasons. The surface circulation is dominated by an anticyclonic circulation off Salum Bay in winter, spring and summer. In nearshore areas, the current flows eastwards at the shallower levels but westwards at the deeper levels. Off the Nile Delta, the current is almost eastward with a higher velocity in summer and autumn, while in spring it is very weak. Off the area between Port Said and Rafah, there is a clear cyclonic circulation appearing in all seasons except winter. At 50 and 75 m depth, the velocity of the circulation is weak. At 100 m depth, the circulation that appeared between Matruh and Alamen in summer decreases in area and magnitude at the former depths. At 200 and 300 m in winter, the current velocity is quite low. In spring the current flows southwards off the area between Rafah and Port Said. In summer, the current off the area between Port Said and Rafah is quite strong and flows to the south. The situation in autumn is quite similar to that in summer, except in the eastern area, where the current is a westward one.
Czasopismo
Rocznik
Strony
299--310
Opis fizyczny
bibliogr. 14 poz., wykr.
Twórcy
autor
Bibliografia
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  • 6.Kamel M. S., 1999, Seasonal variability of surface current in the eastern Mediterranean Sea, Bull. Nat. Inst. Ocean. Fish., 25, 51-67.
  • 7.Millot C., Taupier-Letage I., 2005, Circulation in the Mediterranean Sea, Handb. Environ. Chem. Vol. 5, Part K, 29-66.
  • 8.Morcos S.A., Hassan H.M., 1976, The water masses and circulation in the southeastern Mediterranean, Acta Adriat., 18 (12), 195-218.
  • 9.Pond S., Pickard G. L., 1983, Introductory dynamical oceanography, Pergamon Press, Oxford, 329 pp.
  • 10.Said M.A., Eid F.M., 1994, Circulation pattern of the Egyptian Mediterranean waters during winter and summer seasons, Pak. J. Mar. Sci., 3 (2), 91-100.
  • 11.Said M.A., Karam A., 1990, On the formation of the intermediate water masses off the Egyptian Mediterranean coast, J. Arch. Hydrobiol., 120 (1), 111-122.
  • 12.Said M.A., Rajkovic B., 1996, A study of water circulation along the Egyptian Mediterranean coast using a three dimensional numerical model, Int. J. Environ. Stud., 50 (3), 223-235.
  • 13.Sharaf El-Din S.H., 1972, Some aspects of the hydrographic conditions of the eastern part of the Mediterranean Sea, Rapp. Comm. Int. Mer Medit., 20 (4), 619-621.
  • 14.Sharaf El-Din S.H., Karam A., 1976, Geostrophic currents in the southern sector of the Mediterranean Sea, Acta Adriat., 18 (13), 221-235.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS8-0003-0008
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