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
Climate variability and deep water mass characteristics in the Aegean Sea
Date
2015-01-15
Author
Georgiou, S.
Mantziafou, A.
Sofianos, S.
Gertman, I.
Ozsoy, E.
Somot, S.
Vervatis, V.
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
242
views
0
downloads
Cite This
The main objective of this study is to investigate the variability of the thermohaline characteristics of the deep-water masses in the Aegean Sea and the possible impact of the regional atmospheric forcing variability by analyzing the available oceanographic and atmospheric datasets for the period of 1960-2012. During this period the variability of the deep water characteristics of the Aegean sub-basins is found to be very large as well as the diversity of the deep water characteristics among the sub-basins. The Central Aegean seems to play the key role in the Aegean deep water formation processes. Due to its small size, the Aegean Sea surface responds rapidly to the meteorological changes and/or the variability of the lateral fluxes and this variability propagates in the thermohaline characteristics of the deep water masses of the basin through deep water formation processes. There are many episodes characterized by a tight coupling of the atmosphere and the ocean during the examined period, with the Eastern Mediterranean Transient (EMT) being the most prominent case. We suggest that deep water formation is triggered mostly by the combination of preconditioning during early winter and/or previous winters together with the number of subsequent extreme events during present winter and not only by the total amount of the extreme heat loss winter days.
Subject Keywords
Aegean Sea
,
Deep water
,
Climate variability
URI
https://hdl.handle.net/11511/68385
Journal
ATMOSPHERIC RESEARCH
DOI
https://doi.org/10.1016/j.atmosres.2014.07.023
Collections
Graduate School of Marine Sciences, Article
Suggestions
OpenMETU
Core
Water-mass properties and circulation on the west Antarctic Peninsula Continental Shelf in Austral Fall and Winter 2001
Klinck, JM; Hofmann, EE; Beardsley, RC; Salihoğlu, Barış; Howard, S (2004-01-01)
Hydrographic measurements made during the US Southern Ocean Global Ocean Ecosystem Dynamics cruises, which took place from April to June and July to September 2001, provide a description of changes in water-mass distributions and circulation patterns in the Marguerite Bay region of the west Antarctic Peninsula continental shelf that result from seasonal variability and offshore forcing by the southern boundary of the Antarctic Circumpolar Current (ACC). The primary seasonal change in water-mass properties i...
Surface circulation in the Alboran Sea (western Mediterranean) inferred from remotely sensed data
Renault, L.; Oguz, T.; Pascual, A.; Vizoso, G.; Tintore, J. (2012-08-03)
In this study, for the first time at regional scale, the combined use of remote sensing data (altimetry and sea surface temperature records) provides a description of the persistent, recurrent and transient circulation regimes of the Alboran Sea circulation. The analysis of 936 altimeter-derived weekly absolute dynamic topography (ADT) and surface geostrophic current maps for 1993-2010 reveals the presence of a dominant annual signal and of two interannual modes of variability. The winter-spring phase is ch...
Seasonal Changes in the Composition and Abundance ofZooplankton in the Seas of the Mediterranean Basin
Kovalev, Av; Mazzocchı, Mg; Toklu Alıçlı, Benin; Skryabın, Va; Kıdeyş, Ahmet Erkan (2003-01-01)
Seasonal changes in the composition, abundance and biomass of zooplankton in the seas of the Mediterranean basin (the Mediterranean, Black and Azov seas) have been reviewed using our own data and data from the literature. In the deep-water central regions of the seas, the seasonal cycle of zooplankton abundance is characterised by one maximum occurring in spring or summer. In the coastal regions, two to three peaks (spring, summer and autumn) exist for the zooplankton abundance. The amplitude of seasonal fl...
Determinants of temperature and salinity in the Levantine Sea using in-situ data
Serimözü, Cem; Taşıran, Ali Cevat; Sustainable Environment and Energy Systems (2019-8)
The Levantine Sea, part of the Eastern Mediterranean where international interests collide and exposed to rising anthropogenic pressure, is our focus in this study. Additionally, four of its sub-regions: Cilician and Levantine Basins, Coastal Nile Delta and Rhodes Gyre are chosen. On account of the relative scarcity of scientific studies of these regions, we aimed to contribute to the investigation of Sea Water Temperature and Salinity, two critical oceanographic parameters in the context of climate change....
Climate change effects on extreme flows of water supply area in Istanbul: utility of regional climate models and downscaling method
Kara, Fatih; Yücel, İsmail (2015-09-01)
This study investigates the climate change impact on the changes of mean and extreme flows under current and future climate conditions in the Omerli Basin of Istanbul, Turkey. The 15 regional climate model output from the EU-ENSEMBLES project and a downscaling method based on local implications from geophysical variables were used for the comparative analyses. Automated calibration algorithm is used to optimize the parameters of Hydrologiska Byrans Vattenbalansavdel-ning (HBV) model for the study catchment ...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
S. Georgiou et al., “Climate variability and deep water mass characteristics in the Aegean Sea,”
ATMOSPHERIC RESEARCH
, pp. 146–158, 2015, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/68385.