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Book Chapter

The hydrology and paleohydrology of the Dead Sea tributaries

By
Noam Greenbaum
Noam Greenbaum
1
Department of Geography and Environmental Studies and Department of Natural Resources and Environmental Management, University of Haifa, Mount Carmel, Haifa 31905, Israel
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Arie Ben-Zvi
Arie Ben-Zvi
2
Israel Hydrological Service, P.O. Box 36118, Jerusalem 91360, Israel, and the Negev Academic College for Engineering, P.O. Box 45, Beer Sheva 81400, Israel
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Itai Haviv
Itai Haviv
3
Institute of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram, Jerusalem 91904, Israel
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Yehouda Enzel
Yehouda Enzel
4
Institute of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram, Jerusalem 91904, Israel, and Department of Geography, The Hebrew University of Jerusalem, Mount Scopus, Jerusalem 91905, Israel
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Published:
January 01, 2006

The Dead Sea (drainage area of ∼42,200 km2) is a terminal lake fed from the north by the Jordan River. The main water source into the Dead Sea is runoff, and its level is highly sensitive to the annual rainfall in the upper Jordan River drainage basin. Here, we summarize relevant data about present and past surface-water hydrology in the drainage basin and water input into the Dead Sea. The lower Jordan River, with a natural mean annual discharge of ∼1100 106 m3 yr−1, drains Mediterranean to semiarid areas in northern Israel, Jordan, Syria, and Lebanon. Additional water is contributed from tributaries such as the Zarqa River (64 106 m3 yr−1). The diversion of water from these and other sources since the 1960s to an inflow of only ∼210 106 m3 yr−1 caused a 20 m decline of the Dead Sea level. The ephemeral Nahal Arava drains hyperarid areas south of the Dead Sea and contributes small volumes of water (∼5 106 m3 yr−1) but experiences occasional large floods (up to 1000 m3 s−1); the smaller, steep ephemeral tributaries west of the Dead Sea produce relatively large floods (up to 775 m3 s−1) due to their wetter headwaters, but their volumes are relatively small (<3 106m3). The annual inflow (∼200 106m3 yr−1) to the Dead Sea from the eastern, semiarid tributaries is divided between base flows (∼65% of annual discharge) and winter floods. In the arid part of the basin, transmission losses and recharge into the shallow alluvial aquifers and probably also to the deeper aquifers during floods are directly related to flow volume. Transmission losses in Nahal Zin decrease with flood magnitude from ∼86% to 100% in small floods of <10 m3 s−1 to ∼10% for large floods of up to 1500 m3 s−1. During the largest floods, the volume of these losses can exceed 4 106 m3.

Rare paleofloods during the past 2000 yr in the Negev were 2–3 times larger than present-day measured floods. The temporal distribution of paleofloods shows that periods with a high frequency of large floods alternate with periods of few large floods. Periods with a high frequency of large floods correlate with high Dead Sea levels, and a low frequency of floods correlates with low lake levels.

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Contents

GSA Special Papers

New Frontiers in Dead Sea Paleoenvironmental Research

Yehouda Enzel
Yehouda Enzel
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Amotz Agnon
Amotz Agnon
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Mordechai Stein
Mordechai Stein
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Geological Society of America
Volume
401
ISBN print:
9780813724010
Publication date:
January 01, 2006

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