Morocco’s water resources are under increasing pressure from population and industrial growth, irrigated agriculture, urbanization, tourism, climate change, overexploitation of aquifers and deteriorating water quality.

About 98% of Egypt’s fresh water resources originate outside of its borders, such as the Nile River and groundwater aquifers. Indeed, the Nile River provides the country with some 93% of its water requirements

The Sultanate of Oman is holding a strategically important position at the mouth of the Persian Gulf. The population of Oman is 4.43 million (2016).

The limited availability of fresh water in the United Arab Emirates (UAE) has for decades presented a major challenge to the Gulf state’s government and people.

Water resources in the UAE can be classified into two main categories: conventional, such as surface water (including aflaj water systems, springs and dams) and groundwater (shallow and deep aquifers), and non-conventional, such as desalinated water, treated wastewater and cloud seeding.

With an area of 1.8 million km², Sudan is the third-largest country in Africa. It consists generally of flat plains, with a few mountain outcrops such as Jebel Marra in the west, the Red Sea Hills in the east and the Ingessna Hills and the Nuba Mountains in the centre.

The source of the Nile is in the Nyungwe Forest in Rwanda. From there, it travels northwards for 6,718km, making it the longest river in the world

In 2016, Fanack, Land Life Company (LLC) and the Union of Agricultural Work Committees (UAWC) initiated a pilot project to bring the innovative COCOON planting technology to Palestine.

The Islamic Republic of Iran covers a total area of 1.75 million km2 and is bordered by Armenia, Azerbaijan, the Caspian Sea and Turkmenistan to the north, Afghanistan and Pakistan to the east, the Gulf of Oman, the Strait of Hormuz and the Persian Gulf to the south, and Iraq and Turkey to the west.

The total long-term annual renewable water resources are estimated at 120BCM, of which about 78BCM go to surface run-off, and groundwater recharge is estimated at about 42BCM per annum, 11BCM by qanats (underground water supply systems) and springs, plus 31BCM by wells.