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Circulation and winter deep-water formation in the northern Red Sea

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Water mass characteristics and circulation patterns in the Gulf of Aqaba and northern Red Sea were studied for the first time during the r/v "Meteor" cruise leg 44/2 from February 21st to March 7th 1999 using temperature-salinity profiles and current observations. The deep water in the northern Red Sea had similar characteristics to the well-mixed upper 450 m of water in the Gulf of Aqaba. This indicates that the winter mixed waters of the Gulf of Aqaba contribute significantly to deep-water in the northern Red Sea. Mixing in the Gulf of Aqaba is an annually repeated event that starts with the cooling of the surface water during November-December and reaches a maximum, which in most years extends down the entire water column in March-April. Waters deeper than the mixed layer in the Gulf seems to be rather passive and play no specific role in water mass formation in the northern Red Sea. In contrast to the Gulf of Aqaba, the upper 200 m of the northern Red Sea were stratified (21.5-23.5oC, and 40.0-40.3 PSU). Stratification at the Strait of Tiran was weak (21.6-22.0oC, and 40.3-40.5 PSU) and disappeared abruptly in the Gulf of Aqaba (21.4-21.6oC, and 40.6-40.7 PSU). A well-developed cyclonic gyre with a diameter of about 50-60 km and maximum velocity of about 0.4 m s-1 was observed in the stratified upper 200 m of the northern Red Sea waters. The gyre may contribute to the preconditioning for intermediate water formation in the northern Red Sea.
Słowa kluczowe
Czasopismo
Rocznik
Strony
5--23
Opis fizyczny
Bibliogr. 24 poz., mapa, wykr.
Twórcy
autor
  • Marine Science Station, University of Jordan & Yarmouk University, P.O. Box: 195, 77110 Aqaba, Jordan
autor
  • Marine Science Station, University of Jordan & Yarmouk University, P.O. Box: 195, 77110 Aqaba, Jordan
autor
  • Baltic Sea Research Institute, Seestrasse 15, D-18119 Warnemünde, Germany
autor
  • Baltic Sea Research Institute, Seestrasse 15, D-18119 Warnemünde, Germany
Bibliografia
  • [1] Assaf G., Kessler J., 1976, Climate and energy exchange in the Gulf of Aqaba, Mon. Weath. Rev., 104, 381-385.
  • [2] Badran M. I., 2001, Dissolved oxygen, chlorophyll a and nutrient seasonal cycles in waters of the Gulf of Aqaba, Red Sea, Aquat. Ecosyst. Health Manage., 4, 139-150.
  • [3] Berman T., Paldor N., Brenner S., 2000, Simulation of wind-driven circulation in the Gulf of Elat (Aqaba), J. Mar. Syst., 26, 349-365.
  • [4] Brauner R., 2000, 6.2. Weather and meteorological conditions during leg M44/2, p. 213, [in:] Östliches Mittelmeer – Nördliches Rotes Meer 1999, Cruise No. 44, 22 January – 16 May 1999, J .Pätzold, P. E. Halbach, G. Hempel & H. Weikert (eds.), METEOR-Berichte, Universität Hamburg, 00-3, 240 pp.
  • [5] Cember R. P., 1988, On the sources, formation, and circulation of Red Sea deep water, J. Geophys. Res.-Oceans, 93 (C7), 8175-8191.
  • [6] Clifford M., Horton C., Schmitz J., Kantha L. H., 1997, An oceanographic nowcast/forecast system for the Red Sea, J. Geophys. Res.-Oceans, 102 (C11), 25101-25122.
  • [7] Eshel G., Cane M., Blumenthal M., 1994, Modes of subsurface, intermediate, and deep water renewal in the Red Sea, J. Phys. Oceanogr., 99 (C8), 15941-15952.
  • [8] Eshel G., Naik N., 1996, Climatological coastal jet, intermediate water formation, and general circulation of the Red Sea, J. Phys. Oceanogr., 27 (7), 1233-1257.
  • [9] Hall J., 1975, Bathymetric chart of the Straits of Tiran, Isr. J. Earth Sci., 24, 69-72.
  • [10] Hall J., Ben-Avraham Z., 1978, New bathymetric map of the Gulf of Eilat (Aqaba), Abstracts 10th Int. Conf. Sedimentol., Jerusalem, 1, 285 pp.
  • [11] Hulings N., 1989, A review of marine science research in the Gulf of Aqaba, Marine Science Station, Aqaba (Jordan).
  • [12] Klinker J., Reiss Z., Kropach C., Levanon I., Harpaz H., Halicz E., Assaf G., 1976, Observation on the circulation pattern in the Gulf of Aqaba, Red Sea, Isr. J . Earth Sci., 25, 85-103.
  • [13] Maillard C., 1974, Formation d’eau profonde en mer rouge, [in:] La formation des eaux océaniques profondes, pp. 115-125, Centre Nat. Rech. Sci., CNRS, Paris.
  • [14] Maillard C., Soliman G., 1986, Hydrography of the Red Sea and exchange with Indian Ocean in summer, Oceanol. Acta, 9 (3), 249-269.
  • [15] Morcos S. A., 1970, Physical and chemical oceanography of the Red Sea, Oceanogr. Mar. Biol. Ann. Rev., 8, 73-202.
  • [16] Murray S., Hecht A., Babcock A., 1984, On the mean flow in the Tiran Strait in winter, J. Mar. Res., 42, 265-287.
  • [17] Neumann C., McGill D., 1961, Circulation of the Red Sea in early summer, Deep-Sea Res., 8, 223-235.
  • [18] Paldor N., Anati D., 1979, Seasonal variation of temperature and salinity in the Gulf of Aqaba, Deep-Sea Res., 26 (6A), 661-672.
  • [19] Plaehn O., Baschek B., Badewien T., Walter M., Rhein M., 2002, Important of the Gulf of Aqaba for the formation of bottom water in the Red Sea, J. Geophys. Res., 107 (C8), doi: 10.1029/2000JC000342.
  • [20] Por F.D., Lerner-Seggev R., 1966, Preliminary data about the benthic fauna of the Gulf of Eilat (Aqaba) Red Sea, Isr. J. Zool., 15, 38-50.
  • [21] Quadfasel D., Baudner H., 1993, Gyre-scale circulation cells in the Red Sea, Oceanol. Acta, 16 (3), 221-229.
  • [22] Sverdrup H. U., Johnson M. W., Fleming R. H., 1961, The oceans: their physics, chemistry and general biology, 1st edn., Prentice-Hall, Inc., Englewood Cliffs, NJ.
  • [23] Woelk S., Quadfasel D., 1996, Renewal of deep water in the Red Sea during 1982-1987, J. Geophys. Res., 101, 18155-18165.
  • [24] Wyrtki K., 1974, On the deep circulation of the Red Sea, [in:] La formation des eaux océanigues prefondes, pp. 91-106, Centre Nat. Rech. Sci., CNRS, Paris.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS5-0011-0046
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