Modelling global-scale climate impacts of the late Miocene Messinian Salinity Crisis

Ivanovic, Ruza. F., Valdes, Paul. J., Flecker, Rachel and Gutjahr, Marcus (2014) Modelling global-scale climate impacts of the late Miocene Messinian Salinity Crisis Climate of the Past, 10 (2). pp. 607-622. DOI 10.5194/cp-10-607-2014.

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Abstract

Late Miocene tectonic changes in Mediterranean–Atlantic connectivity and climatic changes caused Mediterranean salinity to fluctuate dramatically, including a ten-fold increase and near-freshening. Recent proxy- and model-based evidence suggests that at times during this Messinian Salinity Crisis (MSC, 5.96–5.33 Ma), highly saline and highly fresh Mediterranean water flowed into the North Atlantic Ocean, whilst at others, no Mediterranean Outflow Water (MOW) reached the Atlantic. By running extreme, sensitivity-type experiments with a fully coupled ocean–atmosphere general circulation model, we investigate the potential of these various MSC MOW scenarios to impact global-scale climate.

The simulations suggest that although the effect remains relatively small, MOW had a greater influence on North Atlantic Ocean circulation and climate than it does today. We also find that depending on the presence, strength and salinity of MOW, the MSC could have been capable of cooling mid–high northern latitudes by a few degrees, with the greatest cooling taking place in the Labrador, Greenland–Iceland–Norwegian and Barents seas. With hypersaline MOW, a component of North Atlantic Deep Water formation shifts to the Mediterranean, strengthening the Atlantic Meridional Overturning Circulation (AMOC) south of 35° N by 1.5–6 Sv. With hyposaline MOW, AMOC completely shuts down, inducing a bipolar climate anomaly with strong cooling in the north (mainly −1 to −3 °C, but up to −8 °C) and weaker warming in the south (up to +0.5 to +2.7 °C).

These simulations identify key target regions and climate variables for future proxy reconstructions to provide the best and most robust test cases for (a) assessing Messinian model performance, (b) evaluating Mediterranean–Atlantic connectivity during the MSC and (c) establishing whether or not the MSC could ever have affected global-scale climate.

Document Type: Article
Additional Information: WOS:000335374600013
Keywords: Messinian Salinity Crisis, Mediterranean Outflow Water, Global Circulation Model, GCM, North Atlantic, AMOC, Mediterranean–Atlantic connectivity, salinity variation
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
Refereed: Yes
DOI etc.: 10.5194/cp-10-607-2014
ISSN: 1814-9324
Related URLs:
Date Deposited: 14 Apr 2014 11:37
Last Modified: 02 Jun 2014 13:30
URI: http://eprints.uni-kiel.de/id/eprint/24195

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