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Dead Sea water trajectories in the T–S space

Abstract

The Dead Sea water column is composed, to a first approximation, of two water bodies: the deep waters, constituting most of the lake's volume, and a shallow upper layer a few meters thick. The temperature and salinity profiles can both be either stabilizing or destabilizing, depending on the regime and the season; if salinity is destabilizing, and double-diffusive processes are attained, the two water bodies mix at a much faster rate than normal turbulent diffusion can account for. The trajectories of the Dead Sea brines since 1977 belong to one of three different categories: upper layer under a meromictic regime, upper layer under a holomictic regime, and lower layer under a holomictic regime. The lower layer during the meromictic regime of 1979– 82 remained constant in its properties and its trajectory is thus represented by one single point.

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References

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Anati, D.A. Dead Sea water trajectories in the T–S space. Hydrobiologia 381, 43–49 (1998). https://doi.org/10.1023/A:1003219322869

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  • DOI: https://doi.org/10.1023/A:1003219322869

  • hypersaline brines
  • stratification
  • T–S space
  • double-diffusive mixing