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The Dead Sea Future Elevation

Bashitialshaer, Raed LU and Persson, Kenneth M LU (2011) In International Journal of Sustainable Water and Environmental Systems 2(2). p.67-67
Abstract
In this paper water and salt mass balances for the Dead Sea were modeled. Precipitation, evaporation, river discharges, ground water flows, input/output from potash companies and salt production, and brine discharge were included in the models. The mixing time in the Dead Sea was modeled using a single-layer (well-mixed) a two-layer (stratified) system. Using the single-layer approach the water level was predicted to change from 411 m below mean sea level (bmsl) (in 1997) to 391 m and 479 m bmsl (in 2097) based on water mass balances including and excluding brine discharge, respectively, and to reach 402 m and 444 m for the two cases based on a salt mass balance. In the two-layer approach the water level after 100 years was predicted to... (More)
In this paper water and salt mass balances for the Dead Sea were modeled. Precipitation, evaporation, river discharges, ground water flows, input/output from potash companies and salt production, and brine discharge were included in the models. The mixing time in the Dead Sea was modeled using a single-layer (well-mixed) a two-layer (stratified) system. Using the single-layer approach the water level was predicted to change from 411 m below mean sea level (bmsl) (in 1997) to 391 m and 479 m bmsl (in 2097) based on water mass balances including and excluding brine discharge, respectively, and to reach 402 m and 444 m for the two cases based on a salt mass balance. In the two-layer approach the water level after 100 years was predicted to change from 411 m bmsl (1997) to 397 m and 488 m for a water mass balance including and excluding brine discharge, respectively, and to reach 387 m and 425 m for the two cases using a salt mass balance. The water mixing time using the single-layer description increased from 58 to 116 years when excluding brine discharge. Using the two-layer approach the exchange or mixing time increased in both layers, when adding brine discharge to the system, from 1.2 to 1.7 years and 11 to 15.3 years in the upper and lower layers, respectively. Good agreement was found between the models and historical data. (Less)
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author
and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Water-Salt balance, Red Sea-Dead Sea Canal (RSDSC), Single-Layer and Two-Layer system, Mixing time
in
International Journal of Sustainable Water and Environmental Systems
volume
2
issue
2
article number
10
pages
76 pages
publisher
International Association for Sharing Knowledge and Sustainability (IASKS)
ISSN
1923-7545
language
English
LU publication?
yes
id
1ce3d18a-c703-41bf-ad94-63bc250ec669
alternative location
http://iasks.org/volume-02-issue-2-2011/
date added to LUP
2020-06-09 10:48:14
date last changed
2020-06-09 13:37:10
@article{1ce3d18a-c703-41bf-ad94-63bc250ec669,
  abstract     = {{In this paper water and salt mass balances for the Dead Sea were modeled. Precipitation, evaporation, river discharges, ground water flows, input/output from potash companies and salt production, and brine discharge were included in the models. The mixing time in the Dead Sea was modeled using a single-layer (well-mixed) a two-layer (stratified) system. Using the single-layer approach the water level was predicted to change from 411 m below mean sea level (bmsl) (in 1997) to 391 m and 479 m bmsl (in 2097) based on water mass balances including and excluding brine discharge, respectively, and to reach 402 m and 444 m for the two cases based on a salt mass balance. In the two-layer approach the water level after 100 years was predicted to change from 411 m bmsl (1997) to 397 m and 488 m for a water mass balance including and excluding brine discharge, respectively, and to reach 387 m and 425 m for the two cases using a salt mass balance. The water mixing time using the single-layer description increased from 58 to 116 years when excluding brine discharge. Using the two-layer approach the exchange or mixing time increased in both layers, when adding brine discharge to the system, from 1.2 to 1.7 years and 11 to 15.3 years in the upper and lower layers, respectively. Good agreement was found between the models and historical data.}},
  author       = {{Bashitialshaer, Raed and Persson, Kenneth M}},
  issn         = {{1923-7545}},
  keywords     = {{Water-Salt balance; Red Sea-Dead Sea Canal (RSDSC); Single-Layer and Two-Layer system; Mixing time}},
  language     = {{eng}},
  number       = {{2}},
  pages        = {{67--67}},
  publisher    = {{International Association for Sharing Knowledge and Sustainability (IASKS)}},
  series       = {{International Journal of Sustainable Water and Environmental Systems}},
  title        = {{The Dead Sea Future Elevation}},
  url          = {{https://lup.lub.lu.se/search/files/80416290/10.11648.j.ajep.20130206.19.pdf}},
  volume       = {{2}},
  year         = {{2011}},
}