The Hula Valley which is part of the Lake Kinneret watershed (2730 km2) in northern Israel is part of the Syrian–African Great Rift Valley. During mid-1980`s-2017 changes in the climate condition (CCC) were recorded in the watershed: Dryness symptoms of rainfall and headwater river discharges have been declining and air temperature has been increasing. The most recent periodical dryness (drought) was recorded in 2014–2019. Although the Hula Valley comprises only about 10% of the entire drainage basin, it is a significant environmental regional component contributing pollutants which is utilized for agricultural cultivation and eco-tourism infrastructure. Until the late 1950s, this valley was covered by swampy wetlands and a shallow old Lake Hula of mean 1.5 m depth and 13 km2 surface area. The valley was drained and converted for agricultural development. The objective of this paper is an evaluation of long-term record of the CCC consequences within the Hula Valley: Headwater discharges, precipitation, air temperature, underground water table (GWT), wind regime (velocity, direction), evaporation, relative humidity, and solar radiation. A partial of CCC within the Hula Valley was confirmed, mostly temperature increase, water deficiency, and ground water table (GWT) lowering. Results indicates that the impact of CCC threatened the optimal appropriate maintenance of the valley. Conclusive future perspectives of supplemental water supply from lake Kinneret to the Hula Valley combined with enhancement of desalinized sea water input into the lake that might improve Hula Valley management and the Kinneret water quality are discussed.
Published in | American Journal of Water Science and Engineering (Volume 7, Issue 4) |
DOI | 10.11648/j.ajwse.20210704.14 |
Page(s) | 165-178 |
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
Copyright |
Copyright © The Author(s), 2021. Published by Science Publishing Group |
Kinneret Watershed, Hula Valley, Climate Conditions Change
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APA Style
Gophen Moshe, Meron Moshe, Tsipris Yosef, Orlov-Levin Valerie, Peres Moti. (2021). Ecological Consequences of Climate Condition Changes (CCC) in Lake Kinneret Watershed. American Journal of Water Science and Engineering, 7(4), 165-178. https://doi.org/10.11648/j.ajwse.20210704.14
ACS Style
Gophen Moshe; Meron Moshe; Tsipris Yosef; Orlov-Levin Valerie; Peres Moti. Ecological Consequences of Climate Condition Changes (CCC) in Lake Kinneret Watershed. Am. J. Water Sci. Eng. 2021, 7(4), 165-178. doi: 10.11648/j.ajwse.20210704.14
AMA Style
Gophen Moshe, Meron Moshe, Tsipris Yosef, Orlov-Levin Valerie, Peres Moti. Ecological Consequences of Climate Condition Changes (CCC) in Lake Kinneret Watershed. Am J Water Sci Eng. 2021;7(4):165-178. doi: 10.11648/j.ajwse.20210704.14
@article{10.11648/j.ajwse.20210704.14, author = {Gophen Moshe and Meron Moshe and Tsipris Yosef and Orlov-Levin Valerie and Peres Moti}, title = {Ecological Consequences of Climate Condition Changes (CCC) in Lake Kinneret Watershed}, journal = {American Journal of Water Science and Engineering}, volume = {7}, number = {4}, pages = {165-178}, doi = {10.11648/j.ajwse.20210704.14}, url = {https://doi.org/10.11648/j.ajwse.20210704.14}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajwse.20210704.14}, abstract = {The Hula Valley which is part of the Lake Kinneret watershed (2730 km2) in northern Israel is part of the Syrian–African Great Rift Valley. During mid-1980`s-2017 changes in the climate condition (CCC) were recorded in the watershed: Dryness symptoms of rainfall and headwater river discharges have been declining and air temperature has been increasing. The most recent periodical dryness (drought) was recorded in 2014–2019. Although the Hula Valley comprises only about 10% of the entire drainage basin, it is a significant environmental regional component contributing pollutants which is utilized for agricultural cultivation and eco-tourism infrastructure. Until the late 1950s, this valley was covered by swampy wetlands and a shallow old Lake Hula of mean 1.5 m depth and 13 km2 surface area. The valley was drained and converted for agricultural development. The objective of this paper is an evaluation of long-term record of the CCC consequences within the Hula Valley: Headwater discharges, precipitation, air temperature, underground water table (GWT), wind regime (velocity, direction), evaporation, relative humidity, and solar radiation. A partial of CCC within the Hula Valley was confirmed, mostly temperature increase, water deficiency, and ground water table (GWT) lowering. Results indicates that the impact of CCC threatened the optimal appropriate maintenance of the valley. Conclusive future perspectives of supplemental water supply from lake Kinneret to the Hula Valley combined with enhancement of desalinized sea water input into the lake that might improve Hula Valley management and the Kinneret water quality are discussed.}, year = {2021} }
TY - JOUR T1 - Ecological Consequences of Climate Condition Changes (CCC) in Lake Kinneret Watershed AU - Gophen Moshe AU - Meron Moshe AU - Tsipris Yosef AU - Orlov-Levin Valerie AU - Peres Moti Y1 - 2021/12/24 PY - 2021 N1 - https://doi.org/10.11648/j.ajwse.20210704.14 DO - 10.11648/j.ajwse.20210704.14 T2 - American Journal of Water Science and Engineering JF - American Journal of Water Science and Engineering JO - American Journal of Water Science and Engineering SP - 165 EP - 178 PB - Science Publishing Group SN - 2575-1875 UR - https://doi.org/10.11648/j.ajwse.20210704.14 AB - The Hula Valley which is part of the Lake Kinneret watershed (2730 km2) in northern Israel is part of the Syrian–African Great Rift Valley. During mid-1980`s-2017 changes in the climate condition (CCC) were recorded in the watershed: Dryness symptoms of rainfall and headwater river discharges have been declining and air temperature has been increasing. The most recent periodical dryness (drought) was recorded in 2014–2019. Although the Hula Valley comprises only about 10% of the entire drainage basin, it is a significant environmental regional component contributing pollutants which is utilized for agricultural cultivation and eco-tourism infrastructure. Until the late 1950s, this valley was covered by swampy wetlands and a shallow old Lake Hula of mean 1.5 m depth and 13 km2 surface area. The valley was drained and converted for agricultural development. The objective of this paper is an evaluation of long-term record of the CCC consequences within the Hula Valley: Headwater discharges, precipitation, air temperature, underground water table (GWT), wind regime (velocity, direction), evaporation, relative humidity, and solar radiation. A partial of CCC within the Hula Valley was confirmed, mostly temperature increase, water deficiency, and ground water table (GWT) lowering. Results indicates that the impact of CCC threatened the optimal appropriate maintenance of the valley. Conclusive future perspectives of supplemental water supply from lake Kinneret to the Hula Valley combined with enhancement of desalinized sea water input into the lake that might improve Hula Valley management and the Kinneret water quality are discussed. VL - 7 IS - 4 ER -