Method for comprehensive computing of water flows geodynamics in the Dead Sea basin

Research output: Contribution to conferencePaperpeer-review

Abstract

The Dead Sea (DS) is a lowest place at the Earth with a unique physical-chemical water composition. The most important physical factor of this basin is the vertical gradient of water density: from 1150 kg/m3 at the DS surface up to 1430 kg/m3 at the depth of 310-330 m. The new mathematical solution obtained for stratified, rotating and compressible liquid (with utilization of gravity, density, temperature and acoustic data) permits to create a solvable system of differential equations and utilize it for development of exact physical/mathematical/geological model of the DS basin.

Original languageEnglish
DOIs
StatePublished - 2010
Event16th European Meeting of Environmental and Engineering Geophysics, Near Surface 2010 - Zurich, Switzerland
Duration: 6 Sep 20108 Sep 2010

Conference

Conference16th European Meeting of Environmental and Engineering Geophysics, Near Surface 2010
Country/TerritorySwitzerland
CityZurich
Period6/09/108/09/10

Fingerprint

Dive into the research topics of 'Method for comprehensive computing of water flows geodynamics in the Dead Sea basin'. Together they form a unique fingerprint.

Cite this