Intermediate and deep currents of the Black Sea, obtained from autonomous profiling floats

Korotaev G., Oguz T., Riser S.

DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, cilt.53, ss.1901-1910, 2006 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 53
  • Basım Tarihi: 2006
  • Doi Numarası: 10.1016/j.dsr2.2006.04.017
  • Dergi Adı: DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.1901-1910
  • Anahtar Kelimeler: Black Sea, profiling floats, deep currents, mesoscale activity, topographic control, UPPER LAYER CIRCULATION, MID-DEPTH CIRCULATION, VARIABILITY, OCEAN, SURFACE, TRANSPORT, DRIFTER, WATER, ARGO
  • Orta Doğu Teknik Üniversitesi Adresli: Hayır

Özet

Float trajectories observed at three depths (200, 750 and 1550m) in the Black Sea during a 1.5-yr period offer new insights on the circulation below the permanent pycnocline. The float observations for the first time provided direct, quantitative evidence for strong currents and a well-organized flow structure at intermediate and deep layers, in contrast to prior ideas of a rather sluggish deep circulation of the Black Sea. The magnitudes of intermediate and deep currents are typically about 5-10% of the surface currents, reaching as much as 5cms(-1) at 1550m, adjacent to the steep topographic slope on the periphery. The combination of float and sea-level height altimeter data suggests that a well-defined cyclonic circulation extends from the surface to the bottom, without reversal in its direction. Deep currents are steered by the steep topographic slope, and well correlated with surface currents at seasonal and longer time scales. (c) 2006 Published by Elsevier Ltd.