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Mechanisms controlling the thermohaline circulation pattern variability in the Aegean–Levantine region. A hindcast simulation (1960–2000) with an eddy resolving model

Mechanisms controlling the thermohaline circulation pattern variability in the Aegean–Levantine region. A hindcast simulation (1960–2000) with an eddy resolving model
Mechanisms controlling the thermohaline circulation pattern variability in the Aegean–Levantine region. A hindcast simulation (1960–2000) with an eddy resolving model
A hindcast simulation in the Aegean–Levantine basins for the years 1960–2000 is performed, using an eddy resolving ocean model (1°/30). The model incorporates a 6-h atmospheric forcing provided by the ARPERA and captures the observed variability of the 40-years. The Eastern Mediterranean Transient (EMT) is the most prominent climatic event of the period. We investigate the impact of the atmospheric versus lateral forcing on the buoyancy content of the Aegean–Levantine basins. During the pre-EMT period, the basins’ buoyancy content is lowered by surface fluxes by about 1.5×10?8 m2 s?3 in the Aegean Sea, mostly related to surface heat loss, and lateral fluxes by about 0.9×10?8 m2 s?3, mostly related to salt flux, with the Levantine changes leading those of the Aegean. Furthermore, while long-term trends of surface and lateral inputs are preconditioning the changes in the Aegean stratification, it is the extreme heat loss pulses, related to the variability of the wind field that is controlling the formation processes by abruptly lowering the buoyancy content. Those events are possibly linked to an eastern Mediterranean bimodal atmospheric oscillation, with the anomalous surface heat fluxes shifting from the Levantine in the 1960s to the Aegean in the 1990s. The central Aegean due to its topography and thermohaline properties trigger events of excessive formation and producing the Aegean’s densest waters. During the EMT winters the central Aegean lower layers contain very dense waters, with ?? larger than 29.3 kg m?3. These waters form the core of the water mass outflowing in the Eastern Mediterranean, after being mixed with ambient waters along their southward flow. The outflowing layer is characterized by density of 29.21 kg m?3. The deepest parts of the NW Levantine is initially filled with the new water mass, which later spreads to the SE parts of the basin, flowing over the Eastern Mediterranean Ridge.
Interannual, Simulation, Eastern Mediterranean Transient, Climate variability
0967-0637
82-97
Vervatis, Vassilios D.
ea81f53a-caf4-4781-9508-2d6a58ef5c80
Sofianos, Sarantis S.
db0e1c6d-b966-4287-a3bd-869a9c7136c1
Skliris, Nikolaos
07af7484-2e14-49aa-9cd3-1979ea9b064e
Somot, Samuel
e9d5b32b-3ab2-44bd-b0da-8e9eaca72478
Lascaratos, Alex
19482135-c40a-4d8c-a9d3-c9d636e12020
Rixen, Michel
72a18112-0cca-45f7-9e0c-1ecfa13d5f5f
Vervatis, Vassilios D.
ea81f53a-caf4-4781-9508-2d6a58ef5c80
Sofianos, Sarantis S.
db0e1c6d-b966-4287-a3bd-869a9c7136c1
Skliris, Nikolaos
07af7484-2e14-49aa-9cd3-1979ea9b064e
Somot, Samuel
e9d5b32b-3ab2-44bd-b0da-8e9eaca72478
Lascaratos, Alex
19482135-c40a-4d8c-a9d3-c9d636e12020
Rixen, Michel
72a18112-0cca-45f7-9e0c-1ecfa13d5f5f

Vervatis, Vassilios D., Sofianos, Sarantis S., Skliris, Nikolaos, Somot, Samuel, Lascaratos, Alex and Rixen, Michel (2013) Mechanisms controlling the thermohaline circulation pattern variability in the Aegean–Levantine region. A hindcast simulation (1960–2000) with an eddy resolving model. Deep Sea Research Part I: Oceanographic Research Papers, 74, 82-97. (doi:10.1016/j.dsr.2012.12.011).

Record type: Article

Abstract

A hindcast simulation in the Aegean–Levantine basins for the years 1960–2000 is performed, using an eddy resolving ocean model (1°/30). The model incorporates a 6-h atmospheric forcing provided by the ARPERA and captures the observed variability of the 40-years. The Eastern Mediterranean Transient (EMT) is the most prominent climatic event of the period. We investigate the impact of the atmospheric versus lateral forcing on the buoyancy content of the Aegean–Levantine basins. During the pre-EMT period, the basins’ buoyancy content is lowered by surface fluxes by about 1.5×10?8 m2 s?3 in the Aegean Sea, mostly related to surface heat loss, and lateral fluxes by about 0.9×10?8 m2 s?3, mostly related to salt flux, with the Levantine changes leading those of the Aegean. Furthermore, while long-term trends of surface and lateral inputs are preconditioning the changes in the Aegean stratification, it is the extreme heat loss pulses, related to the variability of the wind field that is controlling the formation processes by abruptly lowering the buoyancy content. Those events are possibly linked to an eastern Mediterranean bimodal atmospheric oscillation, with the anomalous surface heat fluxes shifting from the Levantine in the 1960s to the Aegean in the 1990s. The central Aegean due to its topography and thermohaline properties trigger events of excessive formation and producing the Aegean’s densest waters. During the EMT winters the central Aegean lower layers contain very dense waters, with ?? larger than 29.3 kg m?3. These waters form the core of the water mass outflowing in the Eastern Mediterranean, after being mixed with ambient waters along their southward flow. The outflowing layer is characterized by density of 29.21 kg m?3. The deepest parts of the NW Levantine is initially filled with the new water mass, which later spreads to the SE parts of the basin, flowing over the Eastern Mediterranean Ridge.

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More information

Published date: April 2013
Keywords: Interannual, Simulation, Eastern Mediterranean Transient, Climate variability
Organisations: Physical Oceanography

Identifiers

Local EPrints ID: 365210
URI: http://eprints.soton.ac.uk/id/eprint/365210
ISSN: 0967-0637
PURE UUID: f55cf4e1-6349-4604-95d8-bb5218e46a9c
ORCID for Nikolaos Skliris: ORCID iD orcid.org/0000-0002-2473-2586

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Date deposited: 27 May 2014 16:14
Last modified: 15 Mar 2024 03:39

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Contributors

Author: Vassilios D. Vervatis
Author: Sarantis S. Sofianos
Author: Samuel Somot
Author: Alex Lascaratos
Author: Michel Rixen

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