Skip to main content

Formulating A Regional Policy for the Future of the Dead Sea — The ‘Peace Conduit’ Alternative

  • Chapter
Water Resources in the Middle East

Abstract

The Dead Sea is a severely disturbed ecosystem, greatly damaged by anthropogenic intervention in its water balance. Since the beginning of the 20th century, the Dead Sea level have dropped by more than 20 meters, and presently (2006) it is about 419 meters below mean sea level. The rate of water level drop over the last 10 years is about 1.0 m/yr, representing an annual water deficit of about 650 million cubic meters. The sharp level drop reflects the annual interception by riparian countries of over 1000 million cubic meters of freshwater which in the past drained to the Dead Sea. In addition to the water interception upstream, the Israeli and Jordanian mineral industries contribute to this deficit by artificially maintaining extensive evaporation surfaces in the otherwise now dried southern Dead Sea basin.

Three alternatives for the future of the Dead Sea exist and need to be examined:

  1. 1.

    Maintaining the present situation. The Dead Sea level is expected to decline further to around -550 m, when a new equilibrium between inflow and evaporation will be reached.

  2. 2.

    Changing the regional water policy whereby freshwater from the Jordan and the Yarmouk river systems will be diverted back to the Dead Sea. In view of the severe regional water deficiency, such a program requires unprecedented regional cooperation and investments to compensate for the freshwater that will be diverted back to the Dead Sea.

  3. 3.

    Construction of the ‘Peace Conduit’ that will convey seawater and/or reject brine after desalination, into the Dead Sea. Such a plan has already been announced by Israel and Jordan in 2002 during the Johannesburg World Summit on sustainable development.

The renewed interest by Israel and Jordan in the construction of the ‘Peace Conduit’ is due to a number of related issues: (1) a growing concern that the Dead Sea must be ’saved’. (2) The possibility of utilizing the proposed conduit for desalinization of the inflowing seawater, thereby providing freshwater to the surrounding entities. (3) The development of infrastructure and tourist facilities around the lake has been adversely affected due to the receding shoreline and the danger presented by the regional collapse of the infrastructure. All parties acknowledge that the ‘Peace Conduit’ is an ambitious project that is bound to change the Dead Sea and its surroundings. While the project has the potential to stop and possibly restore damaging processes that currently occur in the Dead Sea and its surrounding, mixing of seawater in the Dead Sea may also lead to undesired changes in the lake.

The impact of changes on the Dead Sea and its surroundings needs to be carefully evaluated before a final decision is made.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 129.00
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 169.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 169.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Abelson, M.; Baer, G.; Shtivelman V.; Wachs, D.; Raz, E.; Crouvi O.; Kurzon, I.; Yechieli, Y., 2003 “Collapse-sinkholes and radar interferometry reveal neotectonics concealed within the Dead Sea basin”, in: Geophysical Research Letters, 30,52: 1–4.

    Google Scholar 

  • Abelson, M.; Yechieli, Y.; Bein, A.; Shtivelman, V.; Crouvi, O.; Calvo, R.; Steinberg, J.; Baer, G.; Wachs, D., 2004: “Classification and mapping of potential level for the development of the Dead Sea sinkholes”, in: Geological Survey of Israel Report, GSI/13/2004 [in Hebrew].

    Google Scholar 

  • Allen, W., 1855: The Dead Sea, A New Route to India (London: Longman, Brown, Green, Longmans).

    Google Scholar 

  • Anati, D.A.; Stiller, M., 1991: “The post-1979 thermohaline structure of the Dead Sea and the role of double-diffusive mixing”, in: Limnology and Oceanography, 36,2:342–354.

    Google Scholar 

  • Avni, Y.; Zilberman, E.; Shirav, M., 2003: “Response of the geomorphologic system the Dead Sea water level declination and its implications on the surrounding infra structure”, in: Geological Survey of Israel Report. GSI/9/03.

    Google Scholar 

  • Baer, G.; Schattner, U.; Wachs, D.; Sandwell, D.; Wdowinski, S.; Frydman, S., 2002: “The lowest place on Earth is subsiding — an InSAR (interferometric synthetic aperture radar) perspective”, in: Geological Society of America Bulletin, 114: 12–23.

    Article  Google Scholar 

  • Bookman, R.; Enzel, Y.; Agnon, A.; Stein, M., 2004: “Late Holocene lake-levels of the Dead Sea”, in: Bulletin of the Geological Society of America, 116: 555–571.

    Article  Google Scholar 

  • Gavrieli, I.; Bein, A.; Oren, A., 2005: “The expected impact of the “Peace Conduit” project (the Red Sea-Dead Sea pipeline) on the Dead Sea, in: Mitigation and Adaptation Strategies for Global Change, 10(1), 3–22. Erratum: p. 739 and pp. 759–777

    Article  Google Scholar 

  • Gavrieli, I.; Lanski, N.; Yaari-Gazit, N.; Oren, A., 2002: “The Impact of the Proposed “Peace Conduit” on the Dead Sea: Evaluation of Current Knowledge on Dead Sea — Seawater Mixing”, in: Geological Survey of Israel, Report GSI/23/2002.

    Google Scholar 

  • Gavrieli, I.; Oren, A., 2004: “The Dead Sea as a dying lake”, in: Nihoul, J.C.J.; Zavialo P.; Micklin P.P (Eds.). Dying and Dead Seas; Climatic versus Anthropogenic causes. NATO ARW/ASI Series, (Dordrecht: Kluwer): 287–306.

    Google Scholar 

  • Gertman, I.; Hecht, A., 2002: “The Dead Sea hydrography from 1992 to 2000”, in: J. Marine Systems, 35: 169–181.

    Article  Google Scholar 

  • Harza JRV Group, 1996: Red Sea-Dead Sea Canal Project, Draft Prefeasibility Report, Main Report. Jordan Rift Valley Steering Committee of the Trilateral Economic Committee.

    Google Scholar 

  • Herzl, T., 1902: Altneuland (Berlin: Verlag Benjamin Harz).

    Google Scholar 

  • Katz, A.; Starinsky, A., Taitel-Goldman, N., Beyth, M.; 1981: “Solubilities of gypsum and halite in the Dead Sea in its mixtures with seawater”, in: Limnology and Oceanography, 26: 709–716.

    Google Scholar 

  • Krumgalz, B.S.; Hecht, A.; Starinsky, A.; Katz, A., 2000: “Thermodynamic constraints on Dead Sea evaporation: can the Dead Sea dry up?”, in: Chemical Geology, 165:1–11.

    Article  Google Scholar 

  • Lensky, N.G.; Dvorkin, Y.; Lyahovsky, V.; Gertman, I.; Gavrieli, I., 2005: “Mass and energy balance of a hypersaline lake: the Dead Sea”, in: Water Resources Research, 41, W12418, doi:10.1029/2005WR004084.

    Article  Google Scholar 

  • Levy, Y., 1984: “The influence of the admixture rate of partly evaporated Mediterranean water to the Dead Sea on the properties of gypsum that is formed in the brine”. Mediterranean — Dead Sea projects, Summary of Research and Surveys. Mediterranean-Dead Sea Company 5, 279–282 [in Hebrew].

    Google Scholar 

  • Levy, Y.; Kushnir, Y., 1981: “Laboratory Measurements of Nucleation Processes and the Growth of Gypsum in the Mediterranean — Dead Sea Mixed Brine”, in: Geological Survey of Israel Report (Rehovot: The Weizmann Institute of Science).

    Google Scholar 

  • Mediterranean-Dead Sea Company, 1984: Mediterranean-Dead Sea Projects. Vol. 5, Summary of Research and Surveys. reports in Hebrew and English.

    Google Scholar 

  • Neev, D.; Emery, K.O., 1967: “The Dead Sea: Depositional Processes and Environments of Evaporites”, in: Geological Survey of Israel Bulletin, 41: 147 pp.

    Google Scholar 

  • Oren, A., 1993: “The Dead Sea-alive again”, in: Experientia, 49: 518–522.

    Article  Google Scholar 

  • Oren, A.; Shilo, M., 1985: “Factors determining the development of algal and bacterial blooms in the Dead Sea: a study of simulation experiments in outdoor ponds”, in: FEMS Microbiology Ecology, 31: 229–237.

    Article  Google Scholar 

  • Oren, A.; Gavrieli, I.; Gavrieli, J.; Lati, J.; Kohen, M.; Aharoni, M., 2004: “Biological effects of dilution of Dead Sea water with seawater: implications for the planning of the Red Sea — Dead Sea ‘Peace Conduit’”, in: Journal of Marine Systems, 46: 121–131.

    Article  Google Scholar 

  • Salameh, E.; El-Naser, H., 2000: “Changes in the Dead Sea level and their impacts on the surrounding groundwater bodies”, in: Acta Hydrochimica et Hydrobiologica, 28:24–33.

    Article  Google Scholar 

  • Stanhill, G., 1994: “Changes in the rate of evaporation from the Dead Sea”, in: International Journal of Climatology, 14, 465–471.

    Article  Google Scholar 

  • Stein, M., 2002: “The fall and rise of the Dead Sea during the post — Glacial and the Younger Dryas event”, in: Geochimica et Cosmochimica Acta 12th Annual Goldschmidt Conference. Davos, Abstract A738.

    Google Scholar 

  • Steinhorn, I., 1985: “The disappearance of the long-term meromictic stratification of the Dead Sea”, in: Limnology and Oceanography, 30, 451–472.

    Article  Google Scholar 

  • Steinhorn, I.; Assaf, G.; Gat, J.R.; Nishri, A.; Nissenbaum, A.; Stiller, M.; Beyth, M.; Neev, D.; Graber, R.; Friedman, G.M.; Weiss, W., 1979: “The Dead Sea: Deepening of the mixolimnion signifies the overturn of the water column”, in: Science, 206: 55–57.

    Article  Google Scholar 

  • Stiller, M.; Chung, Y.C., 1984: “Radium in the Dead Sea: A possible tracer for the duration of meromixis”, in: Limnology and Oceanography, 29: 574–586.

    Google Scholar 

  • Wachs, D.; Yechieli, Y.; Shtivelman, V.; Itamar, A.; Baer, G.; Goldman, M.; Raz, E.; Rybekov, M.; Schattner, U., 2000: “Formation of Sinkholes along the Dead Sea Shore — Summary of Findings from the First Stage of Research”, in: Geological Survey of Israel Report. GSI/41/2000.

    Google Scholar 

  • Yechieli, Y.; Gavrieli, I.; Berkowitz, B.; Ronen D., 1998: “Will the Dead Sea die?”, in: Geology, 26: 755–758.

    Article  Google Scholar 

  • Yechieli, Y.; Abelson, M.; Bein, A.; Cruvi, O.; Shtivelman, V., 2006: “Sinkhole’ swarms’ along the Dead Sea coast: reflection of disturbance of lake and adjacent groundwater systems”, in: Geological Society of America Bulletin, 118: 1075–1087.

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2007 Springer-Verlag Berlin Heidelberg

About this chapter

Cite this chapter

Gavrieli, I., Bein, A. (2007). Formulating A Regional Policy for the Future of the Dead Sea — The ‘Peace Conduit’ Alternative. In: Shuval, H., Dweik, H. (eds) Water Resources in the Middle East., vol 2. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-69509-7_10

Download citation

Publish with us

Policies and ethics