Heat and salt redistribution within the Mediterranean Sea in the Med-CORDEX model ensemble

  • J. Llasses
  • G. Jordà
  • D. Gomis
  • F. Adloff
  • D. Macías
  • A. Harzallah
  • T. Arsouze
  • N. Akthar
  • L. Li
  • A. Elizalde
  • G. Sannino
Article

DOI: 10.1007/s00382-016-3242-0

Cite this article as:
Llasses, J., Jordà, G., Gomis, D. et al. Clim Dyn (2016). doi:10.1007/s00382-016-3242-0

Abstract

Characterizing and understanding the basic functioning of the Mediterranean Sea in terms of heat and salt redistribution within the basin is a crucial issue to predict its evolution. Here we quantify and analyze the heat and salt transfers using a simple box model consisting of four layers in the vertical for each of the two (western and eastern) basins. Namely, we box-average 14 regional simulations of the Med-CORDEX ensemble plus a regional and a global reanalysis, computing for each of them the heat and salt exchanges between layers. First, we analyze in detail the mechanisms behind heat and salt redistribution at different time scales from the outputs of a single simulation (NEMOMED8). We show that in the western basin the transfer between layer 1 (0–150 m) and layer 2 (150–600 m) is upwards for most models both for heat and salt, while in the eastern basin both transfers are downwards. A feature common to both basins is that the transports are smaller in summer than in winter due to the enhanced stratification, which dampen the mixing between layers. From the comparison of the 16 simulations we observe that the spread between models is much larger than the ensemble average for the salt transfer and for the heat transfer between layer 1 and layer 2. At lower layers (below 600 m) there is a set of models showing a good agreement between them, while others are not correlated with any other. The mechanisms behind the ensemble spread are not straightforward. First, to have a coarse resolution prevents the model to correctly represent the heat and salt redistribution in the basin. Second, those models with a very different initial stratification also show a very different redistribution, especially at intermediate and deep layers. Finally, the assimilation of data seems to perturb the heat and salt redistribution. Besides this, the differences among regional models that share similar spatial resolution and initial conditions are induced by more subtle mechanisms which depend on the variable and process analyzed. In order to reduce the uncertainties in the Mediterranean regional climate projections further modelling studies and better observational datasets are needed to constrain the main sources of discrepancies among models. In the absence of those, an ensemble modelling approach as the one followed in the Med-CORDEX initiative seems to be the best solution to evaluate model uncertainties into the future climate projections.

Keywords

Heat fluxes Salt fluxes Mediterranean Sea Ocean regional climate models Med-CORDEX 

Supplementary material

382_2016_3242_MOESM1_ESM.docx (2 mb)
Supplementary material 1 (DOCX 2052 kb)

Copyright information

© Springer-Verlag Berlin Heidelberg 2016

Authors and Affiliations

  • J. Llasses
    • 1
  • G. Jordà
    • 1
  • D. Gomis
    • 1
  • F. Adloff
    • 2
  • D. Macías
    • 3
  • A. Harzallah
    • 4
  • T. Arsouze
    • 5
  • N. Akthar
    • 6
  • L. Li
    • 5
  • A. Elizalde
    • 7
  • G. Sannino
    • 8
  1. 1.Mediterranean Institute for Advanced Studies (IMEDEA, UIB-CSIC)EsporlesSpain
  2. 2.CNRM Météo-France/CNRSToulouseFrance
  3. 3.Water Research Unit, Institute for Environment and SustainabilityEuropean Commission, Joint Research CenterIspraItaly
  4. 4.Institut National des Sciences et Technologies de la MerTunisTunisia
  5. 5.Laboratoire de Météorologie DynamiqueCNRS/Ecole Polytechnique/ENS/UPMCPalaiseau Cedex, ParisFrance
  6. 6.Institute for Atmospheric and Environmental SciencesGoethe UniversityFrankfurt/MainGermany
  7. 7.Max Planck Institute for MeteorologyHamburgGermany
  8. 8.ENEA Centro Ricerche CasacciaRomeItaly

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