The Environmental Atlas of Abu Dhabi Emirate
52°E
53°E
54°E
55°E
147
G ROUNDWATER C HANGE IN S HALLOW TO M EDIUM D EEP A QUIFER FROM 2005 TO 2008
Ra's al-Khaimah
Umm al-Qaiwain
A r a b i a n G u l f
Water use for irrigation in the Emirate’s agricultural, forestry andplantation sectors consumes over 2billion cubic metres of water per year, nearly all of which is extracted from non-renewable groundwater supplies. Since there is negligible groundwater recharge in the Emirate due to the hyper-arid climate, high extraction rates have led to precipitous groundwater level declines, particularly in the Liwa Crescent and in the vicinity of Al Ain, where agriculture is most intensive.
Groundwater extraction creates a localised cone of depression around a well, where groundwater volume within the cone is less than the surrounding area. Once groundwater extraction ceases, often due to exhausted supply, it is not uncommon to see localised recharge over time within the cone of depression. This explains those areas showing positive change in groundwater levels on this map.
Ajman
Sharjah
Qatar
Dubai
25°N
25°N
Mkasib
Qaffay
Abu Dhabi
Muhayyimat
Ghaghah
Musaffah
Bani Yas
Al Ain
Jebel Dhanna
Ruwais
Sila'a
Tarif
24°N
24°N
Oman
Habshan
Ghayathi
Groundwater Change in Agricultural and Forestry Areas
Madinat Zayed
70
Forest Agriculture
Bu Hasa
53
35
Agriculture Forestry Groundwater Change (2005 - 2008) in Research Area
Liwa
18 Percentage
23°N
23°N
Very Strong Rise (>1.5m) Strong Rise (1.0 - 1.5m) Medium Rise (0.5 - 1.0m) Gentle Rise (0.2 - 0.5m) Steady State (-0.2 - 0.2m) Gentle Decline (0.2 - 0.5m) Medium Decline (0.5 - 1.0m) Strong Decline (1.0 - 1.5m) Very Strong Decline (>1.5m) NoData
0
Very Strong Rise ( >1.5m )
Strong Rise ( 1.0 - 1.5m )
MediumRise ( 0.5 - 1.5m )
Gentle Rise ( 0.2 - 0.5m )
Steady State ( -0.2 - 0.2m )
Gentle Decline ( 0.2 - 0.5m )
MediumDecline ( 0.5 - 1.0m )
Strong Decline ( 1.0 - 1.5m )
Very Strong Decline ( >1.5m )
Change in Groundwater Depth (metres)
Saudi Arabia
20
0
20
40 Kilometres
52°E
53°E
54°E
55°E
56°E
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