Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
A SYNTHESIS OF THE LEVANTINE BASIN CIRCULATION AND HYDROGRAPHY, 1985-1990
Date
1993-01-01
Author
OZSOY, E
HECHT, A
UNLUATA, U
BRENNER, S
SUR, HI
BISHOP, J
LATIF, MA
ROZENTRAUB, Z
OGUZ, T
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
187
views
0
downloads
Cite This
The Levantine Basin circulation derived from recent data consists of a series of sub-basin-scale to mesoscale eddies interconnected by jets. The basin-scale circulation is masked by eddy variability that modulates and modifies it on seasonal and interannual time scales. Long-term qualitative changes in the circulation are reflected in the bifurcation patterns of the mid-basin jets, relative strengths of eddies and the hydrographic properties at the core of these eddies. Confinement within the Basin geometry strongly influences the co-evolution of the circulation features.
Subject Keywords
Oceanography
URI
https://hdl.handle.net/11511/68503
Journal
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
DOI
https://doi.org/10.1016/0967-0645(93)90063-s
Collections
Graduate School of Marine Sciences, Article
Suggestions
OpenMETU
Core
A REVIEW OF THE LEVANTINE BASIN CIRCULATION AND ITS VARIABILITY DURING 1985-1988
OZSOY, E; HECHT, A; UNLUATA, U; BRENNER, S; OGUZ, T; BISHOP, J; LATIF, MA; ROZENTRAUB, Z (Elsevier BV, 1991-04-01)
The variability of the Levantine Basin circulation and hydrography is reviewed based on a collection of recent data sets. The major emphasis is placed on the complexity of the associated dynamics. The region is shown to be populated with synoptic and mesoscale dynamic features. In addition to the complexity arising due to the heterogeneity of water masses and the variability of the atmospheric and thermohaline forcing, the confines of the relatively small basin causes the sub-basin-scale gyres to be in c...
Extension of sea surface temperature unpredictability
Akhmet, Marat; Alejaily, Ejaily Milad (Springer Science and Business Media LLC, 2019-02-01)
The sea surface temperature (SST) variability is clearly affected by global climate patterns, which involve large-scale ocean-atmosphere fluctuations similar to the El Nino-Southern Oscillation (ENSO). We give mathematical arguments for the SST to be unpredictable over oceans. Sensitivity (unpredictability) is the core ingredient of chaos. Several researches suggested that the ENSO might be chaotic. It was Vallis (Science 232:243-245, 1986) who revealed unpredictability in ENSO by reducing his model to the ...
A 2-LAYER MODEL OF WATER EXCHANGE THROUGH THE DARDANELLES STRAIT
OGUZ, T; SUR, HI (1989-01-01)
Water exchange through the Dardanelles Strait is studied by a two-layer model which considers the laterally averaged flow formed by two homogeneous layers of differing density separated by an entraining interface. The model response is discussed in terms of observations from the strait. In particular, the observed asymmetry and rapid transition at the interface depth as weil as the intense mixing which occurs in the southwestern reaches of the strait are found to be related to the hydraulic characteristics ...
On the summer mesoscale variability of the Black Sea
Besiktepe, ST; Lozano, CJ; Robinson, AR (Journal of Marine Research/Yale, 2001-07-01)
The evolution of the Black Sea temperature, salinity and circulation, from large scale to mesoscale, is studied using a data-driven primitive equation simulation. The data are drawn from (i) a basin-wide hydrographic survey, CoMSBlack'92, obtained in the Summer of 1992; (ii) wind stress derived from wind analyses of the Sevastopol MSIA/URHI Office; (iii) climatological heat fluxes; and (iv) climatological river outflows. The primitive equation model is from the Harvard Ocean Prediction System. The simulatio...
A search for new phenomena in pp collisions at root s=13TeV in final states with missing transverse momentum and at least one jet using the alpha(T) variable
Khachatryan, V.; et. al. (Springer Science and Business Media LLC, 2017-05-01)
A search for new phenomena is performed in final states containing one or more jets and an imbalance in transverse momentum in pp collisions at a centre-of-mass energy of 13 TeV. The analysed data sample, recorded with the CMS detector at the CERN LHC, corresponds to an integrated luminosity of 2.3 fb(-1). Several kinematic variables are employed to suppress the dominant background, multijet production, as well as to discriminate between other standard model and new physics processes. The search provides se...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
E. OZSOY et al., “A SYNTHESIS OF THE LEVANTINE BASIN CIRCULATION AND HYDROGRAPHY, 1985-1990,”
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
, pp. 1075–1119, 1993, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/68503.