Details zur Publikation

Kategorie Textpublikation
Referenztyp Zeitschriften
DOI 10.1002/hyp.13598
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Titel (primär) Discharge estimation of submarine springs in the Dead Sea based on velocity or density measurements in proximity to the water surface
Autor Munwes, Y.Y.; Geyer, S. ORCID logo ; Katoshevski, D.; Ionescu, D.; Licha, T.; Lott, C.; Laronne, J.B.; Siebert, C. ORCID logo
Quelle Hydrological Processes
Erscheinungsjahr 2020
Department CATHYD
Band/Volume 34
Heft 2
Seite von 455
Seite bis 472
Sprache englisch
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Keywords Dead Sea; water balance; ubmarine groundwater; submarine springs; jet flow; plume
Abstract The Dead Sea is a closed lake, the water level of which is lowering at an alarming rate of about 1 m/yr. Factors difficult to determine in its water balance are evaporation and groundwater inflow, some of which emanate as submarine groundwater discharge. A vertical buoyant jet generated by the difference in densities between the groundwater and the Dead Sea brine forms at submarine spring outlets. To characterize this flow field and to determine its volumetric discharge, a system was developed to measure the velocity and density of the ascending submarine groundwater across the center of the stream along several horizontal sections and equidistant depths while divers sampled the spring. This was also undertaken on an artificial submarine spring with a known discharge to determine the quality of the measurements and the accuracy of the method. The underwater widening of the flow is linear and independent of the volumetric spring discharge. The temperature of the Dead Sea brine at lower layers primarily determines the temperature of the surface of the upwelling, produced above the jet flow, as the origin of the main mass of water in the submarine jet flow is Dead Sea brine. Based on the measurements, a model is presented to evaluate the distribution of velocity and solute density in the flow field of an emanating buoyant jet. This model allows the calculation of the volumetric submarine discharge, merely requiring either the maximum flow velocity or the minimal density at a given depth.
dauerhafte UFZ-Verlinkung https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=22325
Munwes, Y.Y., Geyer, S., Katoshevski, D., Ionescu, D., Licha, T., Lott, C., Laronne, J.B., Siebert, C. (2020):
Discharge estimation of submarine springs in the Dead Sea based on velocity or density measurements in proximity to the water surface
Hydrol. Process. 34 (2), 455 - 472 10.1002/hyp.13598