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IMPACT: International Journal of Research in 
Humanities, Arts and Literature (IMPACT: IJRHAL) 
ISSN (P): 2347-4564; ISSN (E): 2321-8878 
Vol. 7, Issue 6, Jun 2019, 379-388 
© Impact Journals 

I ITi I ct: 


Raisul Bari 

Assistant Professor, Department of West Asian and North African Studies, Aligarh Muslim University, Aligarh, 

Uttar Pradesh, India 

Received: 19 Jun 2019 Accepted: 27 Jun 2019 Published: 04 Jun 2019 


The Jordan River rises in Mount Herrnon, at the juncture of Syria and Lebanon and drains one of the world’s 
driest countries and planet’s most water deficit region. The river runs through Lebanon, Syria, Jordan Israel and Palestine 
for 251 km and finally dribbled down into the Dead Sea. It is an important water source in the region and due to climate 
change, the region is becoming drier with the time. Historically, the river valley had a lush green, wetland ecosystem and 
was the biological heart of the Middle East region. A European explorer once described it as “the crookest river that 
was ”. The river has now seen that over 90 per cent of its water has been diverted and obstructed by the construction of 
dams and diversion for irrigation as well as for domestic use in the region. Competition for limited and scarce water 
resource has generated hydro-political tension among the shareholders of the region; the region is correctly described as 
the “global hotspot of unsustainable water use. Jordan, the world’s third driest country of the world pulls 160 per cent 
from the underground reservoirs than puts in, out of which 60 per cent is consumed for agricultural purposes. Many 
countries of the Fertile Crescent region fall well below the world’s average annual water availability. The upstream dams 
and diversion have totally reduced the flow of the river in the lower region where it flows snakes through various 
ecologically rich smaller lakes. The obstruction of the natural flow of the river has a negative and excruciating impact on 
the biodiversity of the valley region. There is a need for regional cooperation like Red-Dead project for the management 
of water resource in the region based on the principle of environmental sustainability. The study is solely based on 
documentation-including academic research works, government reports, and newspapers. 

KEYWORDS: Jordan River, Hydro-Political Crisis, Environment, Sustainability 


From the beginning of mankind water over the planet has been seen as a basis of mutual cooperation and peace. 
There have been very few occurrences of clashes over the claim and entitlement to water resources in the history of 
civilization as well as in modern period. It is an important water source in the region and due to climate change, the region 
is becoming drier with the time. Historically, the river valley had a lush green, wetland ecosystem and was the biological 
heart of the Middle East region. The rivers of the region have great importance especially Jordan river that is sacred to the 
Judeo-Christian tradition. Water bodies have always nourished human life and supported the flourishing of agriculture 
human settlements, the rise of states and the growth of population. The rivers of Middle-East Asia have been the 
birthplace of modern civilization as well as a theatre of hydro-political conflicts with the establishment of the Israeli state. 

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Raisul Bari 


There has been a tendency to use water as a weapon of the war rather than as a source of nourishing man-kind as well as 
the environment. Some states use water infrastructure as a target in war conflict; others treat as an instrument of violence. 
The Jordan River basin region is one of the world’s tensest areas and the danger of war is not averted yet. The water 
resource and hydrological matters no doubt present another dimension to the Arab-Israeli conflict. Portable water shortage 
is a worldwide phenomenon; however, the water crisis in the Jordan River basin is not only an environmental concern but 
also a political issue that affects the political stability in the basin region. The region fall in the sub-tropical region that is 
characterized by the arid and semi-arid and creates an environment of extreme with very high rainfall, low and meager 
precipitation and high salinity. 


The study is solely based on secondary sources of data obtained through various published and unpublished 
sources. Other related information, literature, documentation-including academic research works, government reports, and 
newspapers. The paper is based on analytical and exploratory research of methods. 


The major objectives of the paper are; 

• To find out the area of scare water resources in the Jordan river Basin 

• To analyze the hydro-political crises and water sharing plans in the Basin 


Francesca (2014) 

In his research work highlighted the various aspects of the vanishing water landscape in the Middle East. He has 
thoroughly studied the genesis and nomenclature of important rivers, watercourses and its utility in the region, he has also 
provided the political narratives and traditional beliefs surrounding water and its scarcity in the extreme arid region of the 
world. There are several of approaches and set of indicators to measure the degree of water scarcity; researchers have tried 
to figure out water scarcity with several indicators, accounting for both physical and economic water scarcity (Falkenmark, 
1989); has used the availability of water per capita to measure the water scarcity in a region. Rijsberman, (2006) in his 
work he has included economic, technological, and political considerations to gauge the degree of water scarcity. 

The Falken Marks 

Indicators are extensively and commonly used to define the extent of water scarcity of a country through its Water 
Scarcity Index (WSI) According to the WSI, there are three types of water scarcity the first one is water stress (1,000 
Cubic Meters to 1,700 CM of freshwater per capita), second one is water scarcity (500 CM to 1,000 CM of freshwater per 
capita); and the last one is severe water scarcity (less than 500 CM of freshwater per capita). Rijsberman(2006) added that 
access to water needs to be also accounted for, as often this is not due to water shortage, but rather due to poor 
infrastructures and mismanagement in the water delivery services. In his work Mehta (2000) has critically examined some 
of the global arguments and narratives related to water scarcity, water crises, and water resources management and 
displays what they are complicating. He has also evaluated various positions on water ranging from those viewing water as 
an economic good to those viewing water as a human right and the commons. He has highlighted how global debates on 

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Environmental Sustainability and Hydro-Political Crisis of Jordan River 381 

Basin in Middle East: An Analysis _ 

water tend to draw on rather ambiguous political, economic expectations rather than on pragmatically grounded facts and 

Movik (2012) 

He has emphasized that there are structural inequality and distribution in the water sector which comes from the 
West Bank, where it has been claimed that water scarcity is an issue of organizational discrimination against Arabs and 
Palestinians people. There has been unrestricted access to water to illegal Israeli settlements like it was in apartheid South 
Africa, where inequalities based on discriminatory policies were extensive. Thewas had been taken various attempts to 
solve the water sharing problems for the whole basin from as early as 1913 when the Franjieh Plan was recommended, and 
1955, when the Johnston Plan was conceived, not one single plan has been utterly adhered to. The Franjieh Plan was 
envisioned for the irrigation of the Jordan Valley, to generate hydropower and to transfer Yarmouk River flow (100 million 
m3) to Lake Tiberias (Sofer et al., 1999). Once Boutros-Gali in his study on water problem in Middle East Asia 
prophesied that “the next war in the Middle East will be over water, not politics” (in Butts, 1997: 65). 

Mirumachi and Zeitoun (2012) 

In his perusal study of the role of treaties, which has always been seen and recognized as a good instance of 
cooperation. They maintained that cooperation is not always good, as treaties can codify existing asymmetrical status quo, 
and treaties can become the issue of the conflict. Homer-Dixon (1991) has analyzed several shared river basins of the 
Middle East as well as of the world and concluded that “the renewable resource most likely to stimulate interstate resource 
war is river water’ ’. Sidahmed (2014) in their study on the crisis of survival in the Middle East evaluated the various 
causes of water-related violence in the region. They are of the view that the destruction of water infrastructure is the most 
widespread characteristics of conflicts in the Jordan river basin region. H Mulholland (2011) in his study entitled ‘water 
politics in the Middle East, has clearly stated that the salient issue of water shortage in the region is overshadowed by 
another different sensational problems like the oil crisis and the Arab Israel disputes, in his studies he has evaluated three 
case studies from the region: Aquifers on the border of Jordan and Saudi Arabia, the Jordan River Basin and Tigris and 
Euphrates river basin. 

The Geography of Jordan River Basin 

The Jordan River Basin is a trans boundary basin with a total area of about 18500 km2 of which 40 percent is 
located in Jordan, 37 percent in Israel, 10 percent in the Syrian Arab Republic, 9 percent in the West Bank, and 4 percent 
in Lebanon (Lehner et al, 2008) (Table 1). The Jordan River basin covers an area of 0.28 per cent of the total area of the 
Middle Eastern countries and it has an annual flow of around 1300 mm3. The headwater of the 250 km long Jordan River 
originates from three rivers, the Dan, the Banias, and the Hasbani, which merge at a point 5 km south of the northern 
Israeli border then flow south through the Hula Valley to join Lake Tiberias. The part of the Jordan River Basin (JRB) 
located above the Sea of Galilee (Lake Tiberias) is known as the upper Jordan and the land area below to it is known as 
Lower Jordan. With the outflow of the Jordan River from Lake Tiberias, the Lower Jordan River receives the water from 
its main tributary, the Yarmouk River. The river encounters other smaller streams in its course like Harod and Yabis, the 
Fariah, Zarqa, and Nusayrat (Hellel, 1994, p. 155). The river then continues flowing south, forming the border between 
Israel and the West Bank to the west and Jordan to the east and finally ends in the Dead Sea (Green Cross Denmark, 2006). 

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Jordan River is a holly river where Jesus the Christ was baptized by the John the Baptist. It played also a well-known role 
in history. The river has its importance because it is located in an area where every drop of water counts. 

The Upper Jordan River Basin, Just north of Lake Tiberias, contributes the vast majority of the water while the 
Lower Jordan River Basin, which represents 40 percent of the entire Jordan River Basin, makes a much smaller 
contribution as the norther part get much more precipitation that the southern part. The western of the Jordan river Basin 
also get more rainfall as compare to the eastern part of the Jordan River Valley that why the eastern part is dry in nature. 
During the summer, most side streams dry up completely and capturing the winter floodwaters is one of the most critical 
aspects of water resources management in the Jordan River Basin. If these waters are not diverted or stored, they flow 
directly to the Dead Sea (Green Cross Italy, 2006). 

The Dan River is the largest tributary of the Jordan river system which rises in northern Israel from the karstic 
area near the base of mountain Hermon. It further fed by rain and multiple springs around the source region which is in Tel 
Dan along underground fault lines. Dan River flows in Palestine (Israel) and is a principle source of the Jordan River share 
more than 50 per cent of the water of upper Jordan river Basin. Banias River is located at the southern foot of Mount 
Hermon north of the Golan Height. It runs for a total length of 9 km and finally merged with the Dan River. The springs 
are the main source of water for the Banias River. It is one of the main tributaries of the Jordan River that form the Jordan 
river’s upper catchment. Hasbani is one of the major and important tributaries of the Jordan River System. The River 
collects most of its water from two main springs in Lebanon the first one is Wazzani and the second one is Haqzbeih the 
latter being a group of springs on the upper course of the Hasbani. The riverdrifts for 25 miles in Lebanon before crossing 
the border at Ghajar and shortly after joining with the Banias and Dan River at a point in northern Israel where it finally 
discharges into River Jordan. For about four kilometers downstream of Ghajar, the Hasbani forms the border between 
Lebanon and the Golan Height. 

Figure 1: Jordan River Basin in the Middle East 

Source: FAO, Equastat, 2009 

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Environmental Sustainability and Hydro-Political Crisis of Jordan River 383 

Basin in Middle East: An Analysis _ 

The Yarmouk river rises on a lava plateau in southern Syria and flows westward through a deep gorge cut 
through limestone surface along the Jordanian border of the Golan Height. The Yarmouk River originates in Jordan, then 
forms the border between Jordan and the Syrian Arab Republic and then between Jordan and Israel, before flowing into the 
Lower Jordan River. The Yarmouk River is the main source of water for the King Abdullah Canal (KAC), the backbone of 
development in the Jordan Valley. A main tributary of the Jordan River in Jordan, controlled by King Talal Dam and also 
feeding the KAC, is the Zarqa River. The Yarmouk River, which is the main watercourse in this latter part of the Valley, 
joins the Jordan River in an area partly occupied by Israel. The riparian river has always been in conflict and war for the 
use of precious water of the river. The Yarmouk river is much smaller than the Euphrates or even the Litani river but 
supplies up to 50 per cent of the water flow in the lower Jordan river The Yarmouk is only 20 miles (32 km) long in a 
straight line, but because of the many convolutions in its course, the total length of the stream is about 50 miles (80 km). 
Technically Yarmoukriver is considered as an independent river in itself. Finally, it empties into the Jordanriver just 6.4 
km south of the Sea of Galilee or Lake Tiberias. The most efficient use of the Yarmouk River is to collect and store excess 
water during the rainy winter season to supplement the dry and extreme summer. The vegetation in this region is 
dominated by short grasses and drought-resistant scrub. 

Table 1: Country wise area in the Jordan River Basin 


Area of Country in 

Percent of Area of 

Per cent of Total Area 
of the Countries 













West Bank 








Environment and Ecosystem 

Ecosystems of the region are extremely diverse, ranging from sub-humid Mediterranean environments to arid 
climates across very small distances. Climate projections for the eastern Mediterranean indicate future aridification 
(GLOWA, 2007). The average annual precipitation in the basin is projected at 380 mm, although it varies all along the 
basin area (New et al, 2002). The Upper Basin, north of Lake Tiberias, has comparatively more annual precipitation than 
the southern part of the basin. In the norther part, annual precipitation is up to 1400 mm, while the Lower Jordan Basin has 
an average annual precipitation rate of 100 mm at its southern end. The largest part of the fertile land in the basin is located 
in Jordan and the West Bank, along the eastern and western banks of the Jordan River and the side wadis, which have the 
annual rainfall of less than 350 mm. The average annual temperature of the whole Jordan River Basin is nearly 18 °C. The 
average temperature of the Jordan River Basin in January is 9 °C, although it can drop to 5 °C in the coldest places. In 
August, the average temperature of the Jordan River Basin reaches 26 °C, rising to 30 °C in the hottest places. 

There are total of four Jordan River Basin riparian countries that include Syria, Lebanon, Israel, and Jordan. 
Palestine is the last and fifth shareholder that consumes the Jordan River’s limited water resources. All the riparian states 
are destined to have an arid environment. Lebanon has some moderate environment whereas, nearly 70 per cent area of 
Syria is arid and desert type, Israel 60 per cent, and more than 80 of the Jordan is desert (Dolatyar and Gray, 2000). Jordan 
is the third driest country in the world. 

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The Jordan Valley was once a lush marshy wetland ecosystem that was known as the biological heart of the 
Middle Eastern region. The region lies in the Great Rift Valley- a meeting point of the Asian, European and African 
continents, which is also at the crossroad of biodiversity. The region is located in the Middle East, which is a unique 
transition zone between three major biographic domains- the Palaearctic, Afrotropical and Oriental realms. The Jordan 
River has a high number of faunal and floral elements of three domains, with the additions of some local and euryhaline 
taxa (an organism that can survive and thrive in a wide range of salinity condition (NisreenAlwan 2013). Lake Hula or 
Hula Emeq, with its surrounding swamps, was one of the richest ecosystems in terms of biodiversity in the Jordan basin. 
There were various species of aquatic invertebrates and vertebrates and other species of aquatic vegetation. The lake was 
also an important nesting place for many peculiar migratory birds. Sea of Galilee also known as the Kinneret is the largest 
natural lake in the Middle East and the lowest freshwater lake on the earth (209 meters) below the sea level. The lake also 
has some biotic diversity relative to that of the Lake Hula. 

The construction dams, canal pumping stations, and diversion of water streams have largely decreased the flow of 
the Jordan River by more than 90 per cent. The highly exploitative natures of the riparian states which are warranted by 
high population growth, urbanization have modified the course of the river that has also altered the hydrology of the river 
systems of the region. Due to the excessive drawing of underground water, there have been cases of deterioration of fresh 
aquifer water of the region. The dumping of sewage, industrial and household wastewater and chemically contaminated 
agricultural runoff has severe damage the freshness and quality of the water of Jordan River Basin that has badly affected 
the biotic life of the region. Competition for scarce water resources in the midst of conflict allowed little room to think 
about the needs of the river. Need and desire for Economic prosperity and the cultural belief in making the desert bloom 
and thereby conquering nature was the prevalent ideology of riparian countries on both sides of the Jordanriver. The river 
converts into a different kind of stream that contains Israeli, Jordanian and Palestinian sewage, saline water and 
agricultural runoff are most of what is left to flow in place of fresh water into it. 

In January 2007, Jordanian and Israel governments have agreed to establish a peace park at the confluence of the 
Jordan and Yarmouk rivers. It will help to aware the citizen about the cost of the precious water resource. There are 
various studies and examination that reveals that the river still flows full of sewage which indicates how much attention is 
required and work is to be done. The incremental policy measures of demand management, water conservation, pricing 
reforms and removal of subsidies are unlikely to attract media attention and therefore gain a high level of political support. 
Conflict, Competition and cultural arrogance have been responsible for the demise of the Jordanriver system. Cooperation 
and mutual collaboration based on the principles of sustainability is what is believed will revive the Jordan and bring peace 
for the population of the most conflict-prone area of the world that is the Middle East especially the Levant region. 

Hydro-Political Crisis 

More than 35 per cent of the existing water resources in the Jordan river basin account as Surface water, 
groundwater aquifers account for 56 percent of the resources, while reused wastewater and other non-conventional sources 
of water represent nearly 9 percent. The surface water of the Jordan River Basin is the main surface water resource 
available for relatively stable use in the region. It is the major source of water for Israel and Jordan and also supports the 
many aquifers in both countries, extending the reliance on the river (Green Cross Italy, 2006). The region has one of the 
lowest per capita water resources worldwide, well below the typical absolute water scarcity threshold of 500 m3/year per 

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Environmental Sustainability and Hydro-Political Crisis of Jordan River 385 

Basin in Middle East: An Analysis _ 

capita, except for Lebanon. Moreover, water demand in the region continues to increase rapidly due to high population 
growth rates and economic development. 

Johnston, envy of US president during 1953-53 advised to distribute its water between riparian countries to avoid 
conflict between sharing countries. According to the Johnston plan of the water sharing and its use has been given in table 
2 . 

Table 2: Johnston Original Plan of Water Sharing During 1953-55 


Share in Jordan River’s Water (Mm3/yr.) 













*at the time of the plan, the Palestine West Bank was ruled by Jordan, therefore the share of Palestine and Jordan 
was set together at 720 Mm3/yr. Some literature estimated the share of Palestine around 257 Mm3/ yr., some other 
estimated it at 215 Mm3/yr. 

However, the present scenario of water uses of Jordan River is a total different one that is shown in table 3. 

Table 3: Share in Jordan River’s Water 


Share in Jordan River’s Water (Mm3/yr.) 





Other riparian countries of 
the region (Jordan, Syria and 




From the above table 3 is clear that Israel uses more than 700 Mm3/yr. which 300 more than its original 
sanctioned volume. The other three riparian states use only 410 Mm3/yr. whereas, Palestine uses nothing. Before 1967 
Arab-Israel war Palestine in the West Bank had access to the Jordan River and could use some its water through a various 
pumping station. After the occupation of the West Bank, Israeli forces destroyed the station or confiscated all the pumping 
station. The water crises of Palestine had warranted the Oslo accord of 1993 that provided sharing water to the Palestinian 
population. Due to some water sharing problems arise after first Oslo accord there were Oslo II pacts which have given 
more right on the water to the Palestinian to its original pact. 

The Jordan Basin conflict can be designated as having gone through two junctures. The power dynamic and 
nature of inter-state relations between Israel and Jordan account for the failure to build a formal water sharing 
arrangements. This is the reason why in 1955, the Arab states rejected to settle negotiations on the Johnston Plan sponsored 
by the United States. Johnston Plan failed due to various reasons. Eric Johnston, the US special envoy, “believed the Arabs 
would cast aside their determination to regain Palestine for the economic good of two basin states, Israel and Jordan.” 
(Lowi, 1995). 

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There is political implication with respect to water rights and territorial supremacy and insecurity. Israel uses the 
Jordan water for domestic consumption as well as industrial and agricultural uses. The stark water shortage in Jordan 
means that using water for the drinking supply is the main concern. For Israel, water has economic value but is a matter of 
survival and existence for Jordan. Syria refuses to exchange water rights with Israel because that would recognize Israel 
sovereignty. Severe water deficiency in Jordan leaves little choice but to talk with Israel, Israel fears negotiating water 
rights because it might encourage the Arab States to claim more territory. 


The Middle East, in general, belongs to the areas of high and rapid population growth rates of the world. The 
socio-cultural and in part of the pro-natality programs and policies of the governments, result in high fertility rates in most 
of the Arab countries. Jordan, Syria and Palestine all exhibits growth rates of more than 3% meaning a double of the 
population each 20-25 years or even sooner. The high population growth rate has marked spreading out of the irrigated 
area in recent years and adaptation of western styles. The consequences are that the available resources are highly over- 
exploited. This means that every drop of available of water is diverted from the natural cycle for human purpose, and even 
more, water is utilized than the cycle provides. The water conservation and protection of the quality of water are of utmost 
important. Along with the quality of water, every industry must include water treatment plants.The should be law and 
governance about the use of water for irrigation as the region comes under the most water scarce region of the world so the 
farmer must use highly advanced irrigation systems. There should be a restriction on the use of water fertilizer. Least but 
not the last, every state of the region must come to a single platform and have cooperation regarding the protection of water 
and equal and proper share of available water. 


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