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Inter-annual/decadal variability of the north Aegean Sea hydrodynamics over 1960-2000

Inter-annual/decadal variability of the north Aegean Sea hydrodynamics over 1960-2000
Inter-annual/decadal variability of the north Aegean Sea hydrodynamics over 1960-2000
Results from a high-resolution hindcast model experiment, supported by available observations, reveal an increasing salinity trend in the north Aegean during the Eastern Mediterranean Transient (EMT), largely controlled by increases in the flow rate and salinity of water masses of Levantine origin entering the domain through the Myconos-Ikaria strait as a response to an acceleration of the Aegean thermohaline cell. Changes in the Dardanelles inflow (increasing salinity) and in the surface freshwater flux (increasing Evaporation-Precipitation), although both contribute to a higher salt content of the basin during the EMT, play a minor role in the inter-annual/decadal variability of the freshwater budget. A long-term decreasing temperature trend is observed from the 1960s to the early 1990s. It is superimposed on the salinity-preconditioning phase over the 1980s and early 1990s. Both signals are, concomitantly, favouring conditions for intense Dense Water Formation (DWF) in the north Aegean Sea. In addition, the northward displacement of the Black Sea Water front over the EMT, leads to the expansion of convective cells towards the north and to higher formation rates associated with both colder and saltier surface waters.
1108-393X
696-705
Vervatis, Vassilis
65b16950-96bc-463c-9f81-2307ad81e636
Skliris, Nikolaos
07af7484-2e14-49aa-9cd3-1979ea9b064e
Sofianos, Sarantis
1bc845af-01bb-4688-be7e-e7b8159c1fea
Vervatis, Vassilis
65b16950-96bc-463c-9f81-2307ad81e636
Skliris, Nikolaos
07af7484-2e14-49aa-9cd3-1979ea9b064e
Sofianos, Sarantis
1bc845af-01bb-4688-be7e-e7b8159c1fea

Vervatis, Vassilis, Skliris, Nikolaos and Sofianos, Sarantis (2014) Inter-annual/decadal variability of the north Aegean Sea hydrodynamics over 1960-2000. Mediterranean Marine Science, 15 (4), 696-705. (doi:10.12681/mms.852).

Record type: Article

Abstract

Results from a high-resolution hindcast model experiment, supported by available observations, reveal an increasing salinity trend in the north Aegean during the Eastern Mediterranean Transient (EMT), largely controlled by increases in the flow rate and salinity of water masses of Levantine origin entering the domain through the Myconos-Ikaria strait as a response to an acceleration of the Aegean thermohaline cell. Changes in the Dardanelles inflow (increasing salinity) and in the surface freshwater flux (increasing Evaporation-Precipitation), although both contribute to a higher salt content of the basin during the EMT, play a minor role in the inter-annual/decadal variability of the freshwater budget. A long-term decreasing temperature trend is observed from the 1960s to the early 1990s. It is superimposed on the salinity-preconditioning phase over the 1980s and early 1990s. Both signals are, concomitantly, favouring conditions for intense Dense Water Formation (DWF) in the north Aegean Sea. In addition, the northward displacement of the Black Sea Water front over the EMT, leads to the expansion of convective cells towards the north and to higher formation rates associated with both colder and saltier surface waters.

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Published date: 2014

Identifiers

Local EPrints ID: 477836
URI: http://eprints.soton.ac.uk/id/eprint/477836
ISSN: 1108-393X
PURE UUID: 5c706056-f6e9-498e-ae4d-86bc4f9ad0c8
ORCID for Nikolaos Skliris: ORCID iD orcid.org/0000-0002-2473-2586

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Date deposited: 15 Jun 2023 16:48
Last modified: 17 Mar 2024 03:25

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Author: Vassilis Vervatis
Author: Sarantis Sofianos

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