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Layer: Groundwater Monitoring Wells (0)

Name: Groundwater Monitoring Wells

Display Field: WellName

Type: Feature Layer

Geometry Type: esriGeometryPoint

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Type ID Field: null

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• OBJECTID ( type: esriFieldTypeOID, alias: OBJECTID )
• WellName ( type: esriFieldTypeString, alias: Well Name, length: 254 )
• Location ( type: esriFieldTypeString, alias: Location, length: 254 )
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Layer: Static Groundwater Level Contour 2017 (1)

Name: Static Groundwater Level Contour 2017

Display Field: created_user

Type: Feature Layer

Geometry Type: esriGeometryPolyline

Description: Field Descriptions:- OBJECTID_1: A unique, not null integer field used to uniquely identify rows in tables in a geodatabase- Shape: Field which shows the stored geometry type created through ArcGIS (Point, Line, Polygon, Multipoint or Multipatch)- OBJECTID: A unique, not null integer field used to uniquely identify rows in tables in a geodatabase- Contour: Value of Contour lines for the groundwater level in Abu Dhabi (2017) [m AMSL]- HideContou:Value for labeling purposes- Shape_Length: Represents the total length of a polygon's perimeter, in the units used by the feature class' coordinate system- RuleID: Needed for labeling purposes in represantations- Override: A BLOB field that stores feature-specific override to the representation rulesProcessing Steps(DCI 2018): Available Input data:Water below Ground Level:• Reference Day Measurements (RDM)• Water Level Measurements from the Well Inventory (WIP 2016/2017)Reference Point above sea level:• Differential GPS Measurements from GWAP Project (DGPS GWAP)• Differential GPS Measurements from Al Ain University (DGPS Al Ain)• Abu Dhabi Digital Elevation Model supplied from EAD (AD DEM)• Aster Digital Elevation Model (Aster DEM)The following water level information was generated from this information:• If possible, DGPS GWAP and RDM measurements were combined (92 values). These were quality checked with available data to match the DGPS and WL reference points.• DGPS Al Ain information was not used. It differs from DGPS GWAP values and no new information can be gained from it. The RDM that intersect with DGPS Al Ain also intersect with DGPS GWAP.• The remaining RDM were not matched with AD DEM, since only one more data point would be gained from it• Where applicable, DGPS GWAP was then combined with WIP 2016/2017 measuring points. The values were quality checked with available data to match the DGPS and WL reference points• AD DEM was the combined with WIP 2016/2017. Values were corrected with the WSI Reference point information.• Some of the AD DEM values were 0 or -9999, at these points WIP 2016/2017 was combined with Aster DEMThe resulting datasets were quality checked to remove any measurements with missing data.As a next step all WL measuring points within a distance of 100m of operational wells were excluded. Of the remaining, all values derived from RDM and WIP 2017 were used. WIP 2016 were only included in the places where they were more than 1 km away from a WIP 2017 or RDM measurement point. This process is to ensure that the water levels from 2016 and 2017 are not interfering and the result follows the water level 2017 as close as possible. WIP 2016 values were primarily used in the Remah area. Due to the more differentiated nature of the aquifer in this region, only WIP 2016 measurements were taken that have information about the total depth of the well. And then only the measurements were 0<TD<220 m. 220m appeared to be roughly the cut-off value where the aquifer changes.ESRI ArcGIS specific the data derived in this way was interpolated with Topo to Raster (additional data: coastline as 0m contour; Topo Raster with No Enforce, 100m cell size, primary source: spot).Of the interpolated raster the 20m contours were exported. While displaying the gathered water level points, these contours were redrawn to root out the influence from single wells. The redrawn contours were then interpolated with the well points again (topo to raster, no enforcement, 100m cell size). This time 10m contour lines were exported. These were used to remodel the 10m contour lines in between the already existing 20m contour lines. Special caution has been used to specifically weigh points were RDM were taken and DGPS data was available. Several 5m contour lines were added in places of interest, to enhance the information density in the southern part of the Emirate.The contours along the coast and in the south eastern region are based on very little information. These were adapted to ensure that the water table is lower than the surface level as much as possible.With these contours a background raster was interpolated and extracted to AD Emirate extent.Resolution: n/aData Quality: Data was QC checked for consistency and to match the water level measurements as close as possible.

Service Item Id: 335f1c2b6ad14dfd801c2e8abda7b139

Copyright Text: Source Agency: DCI (2018) Collection Agency: DCI (2016/17) Maintenance Agency: EAD Custodial Agency: EAD Contact: EAD - Environment Information, Science & Outreach Management (EISOM)

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Layer: Groundwater Salinity 2017 (2)

Name: Groundwater Salinity 2017

Display Field: created_user

Type: Feature Layer

Geometry Type: esriGeometryPolygon

Description: Two areas of freshwater with low mineral content are found in Abu Dhabi Emirate:In the northeast, rainfall from the Hajjar Mountains recharges the aquifer and slowly flows towards the Arabian Gulf. The longer the water remains in the aquifer, the more time it has to dissolve minerals and interact with the rocks: In general, the water gets more saline as it flows towards the sea. Another area of low salinity is found north of Liwa, where recharge from rainfall is minimal and the resulting groundwater is older. Most of it entered the aquifer thousands of years ago, in a time with a more humid climate. Very slow groundwater flow, uniform sandy lithology, and a distinct vertical salinity gradient in the aquifer have kept the uppermost groundwater fresh for centuries. Along the coast in the west, as well as in the southeast, the groundwater table is very shallow. In these sabkha flats, the groundwater comes close to the surface and some of it evaporates. The dissolved minerals stay behind and lead to a further salinisation of the groundwater. Water in these regions can be as salty as 140,000 mg/L; that is more than three times as salty as the water of the Arabian Gulf.Field Descriptions:-OBJECTID:A unique, not null integer field used to uniquely identify rows in tables in a geodatabase.-Shape:Field which shows the stored geometry type created through ArcGIS (Point, Line, Polygon, Multipoint or Multipatch)-Classes:Consecutively numbered classes of Salinity (0-7)-Value_Max:Upper value of TDS [mg/L] for the selected, corresponding salinity class-Shape_Length:Represents the total length of a polygon's perimeter, in the units used by the feature class' coordinate system-Shape_Area:Represents the total area of a polygon, in square units of the linear distance unit used by the feature class' coordinate system-RuleID:Range of salinity class in mg/L for labeling purposes-Override:A BLOB field that stores feature-specific override to the representation rulesProcessing Steps: Geospatial TDS data from groundwater sampling has been interpolated using Kriging to create polygons showing the distribution of groundwater salinity in eight classes ranging from 0 to 50,000 mg/LResolution: n/aData Quality: data was QC checked for consistency

Service Item Id: 335f1c2b6ad14dfd801c2e8abda7b139

Copyright Text: Source Agency: DCI (2018) Collection Agency: DCI (2016/17) Maintenance Agency: EAD Custodial Agency: EAD Contact: EAD - Environment Information, Science & Outreach Management (EISOM)

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Type ID Field: null

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• RuleID ( type: esriFieldTypeInteger, alias: Rule ID , Coded Values: [1: < 500 Fresh (WHO Standard)] , [2: 500 - <1,000 Fresh (Abu Dhabi Standard)] , [3: 1,000 - <1,500 Fresh] , ...6 more... )
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Layer: Waterlevel Change 2005 to 2017 (3)

Name: Waterlevel Change 2005 to 2017

Display Field: Classes

Type: Feature Layer

Geometry Type: esriGeometryPolygon

Description: Changes in the groundwater level of Abu Dhabi Emirate are closely linked to agricultural activity. Areas with a strongly declining water table coincide with the areas of highest groundwater abstraction for agricultural irrigation. The areas around Remah and Al Wagan illustrate this best. In the course of 25 years, the water level in groundwater monitoring wells has dropped by more than 50 m. The map shows the groundwater level change between 2005 and 2017. While yellow and red areas face a continued decline of groundwater levels, in blue areas a relative rise is observed. This relative rise is mainly attributed to a small reduction in agricultural activity and shut-down of well fields. Though between 2005 and 2017 the groundwater level slightly increased in these areas, an absolute drawdown prevails compared with the natural state. True rising of the water table takes place only in the vicinity of Al Ain, where losses from the water network and excessive landscape irrigation leads to rising water levels above the natural state.Processing Steps (DCI 2018): 648 available water level measurements from 2005 were joined with the closest of the water level measurements 16/17 that was used for the calculation of the water table. Only values with a join distance of less than 600 meters were considered further (341 remaining).The change in water level from the two measurements (2005 and 2016/17) was calculated and interpolated with topo to raster, no enforce, primary source spot.The raster was classified and exported as polygon file.Field Descriptions:- OBJECTID:A unique, not null integer field used to uniquely identify rows in tables in a geodatabase- Shape: Field which shows the stored geometry type created through ArcGIS (Point, Line, Polygon, Multipoint or Multipatch)- Classes: Classes from 0 to 8 according to EAD standard for GW Level Change- Value_Min: Minimum Value of Groundwater Change in the respective Class- Value_Max: Maximum Value of Groundwater Change in the respective Class- Shape_Length:Represents the total length of a polygon's perimeter, in the units used by the feature class' coordinate system- Shape_Area:Represents the total area of a polygon, in square units of the linear distance unit used by the feature class' coordinate system- RuleID: Needed for labeling purposes in represantationsResolution: 1024x1024mData Quality: data was QC checked for consistency

Service Item Id: 335f1c2b6ad14dfd801c2e8abda7b139

Copyright Text: Source Agency: DCI (2018), GWAP (2005) Collection Agency: DCI (2016/17), GWAP Maintenance Agency: EAD Custodial Agency: EAD Contact: EAD - Environment Information, Science & Outreach Management (EISOM)

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MaxRecordCount: 2000

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• RuleID ( type: esriFieldTypeInteger, alias: RuleID , Coded Values: [1: Area with exceptional Water Level Rise (between 1.5 to 5m)] , [2: Area with high Water Level Rise (between 1.0 to 1.5m)] , [3: Area with medium Water Level Rise (between 0.5 to 1m)] , ...7 more... )
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Layer: Groundwater Salinity 2008 (4)

Name: Groundwater Salinity 2008

Display Field: Comment

Type: Feature Layer

Geometry Type: esriGeometryPolygon

Description:

Service Item Id: 335f1c2b6ad14dfd801c2e8abda7b139

Copyright Text:

Default Visibility: false

MaxRecordCount: 2000

Supported Query Formats: JSON, geoJSON, PBF

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Has Labels: false

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• Value: 10
  Label: 100000 - 125000 ppm Brine
  Description: N/A
  Symbol:
  Style: esriSFSSolid
  Color: [242, 78, 32, 255]
  Outline:
  Style: esriSLSNull
  Color: [110, 110, 110, 255]
  Width: 0
• Value: 11
  Label: 125000 - 160000 ppm Brine
  Description: N/A
  Symbol:
  Style: esriSFSSolid
  Color: [233, 17, 22, 253]
  Outline:
  Style: esriSLSNull
  Color: [110, 110, 110, 255]
  Width: 0
Transparency: 0
Labeling Info:
Advanced Query Capabilities:
Supports Statistics: true
Supports OrderBy: true
Supports Distinct: true
Supports Pagination: true
Supports TrueCurve: true
Supports Returning Query Extent: true
Supports Query With Distance: true
Supports Sql Expression: true
Supports Query With ResultType: false
Supports Returning Geometry Centroid: false
Supports Binning LOD: false
Supports Query With LOD Spatial Reference: false
Supports Percentile Statistics: true
Supports Having Clause: true
Supports Count Distinct: true
Supports Time Relation: true
Supports Sql Format: false
Supports Query Analytic: true
Supports Query With Current User: true


HasZ: true

HasM: false

Has Attachments: false

HTML Popup Type: esriServerHTMLPopupTypeAsHTMLText

Type ID Field: null

Fields:
• OBJECTID ( type: esriFieldTypeOID, alias: OBJECTID )
• Classes ( type: esriFieldTypeInteger, alias: Classes )
• Value_Min ( type: esriFieldTypeDouble, alias: Value_Min )
• Value_Max ( type: esriFieldTypeDouble, alias: Value_Max )
• RuleID ( type: esriFieldTypeInteger, alias: RuleID , Coded Values: [1: 0 - 500 ppm Fresh] , [2: 500 - 1000 ppm Fresh] , [3: 1000 - 1500 ppm Fresh] , ...9 more... )
• Shape ( type: esriFieldTypeGeometry, alias: SHAPE )

Layer: Groundwater Depleted Area (5)

Name: Groundwater Depleted Area

Display Field: created_user

Type: Feature Layer

Geometry Type: esriGeometryPolygon

Description:

Service Item Id: 335f1c2b6ad14dfd801c2e8abda7b139

Copyright Text:

Default Visibility: false

MaxRecordCount: 2000

Supported Query Formats: JSON, geoJSON, PBF

Min Scale: 0.0

Max Scale: 0.0

Supports Advanced Queries: true

Supports Statistics: true

Has Labels: false

Can Modify Layer: true

Can Scale Symbols: false

Use Standardized Queries: true

Supports Datum Transformation: true

Extent:
XMin: 53.64549299300006
YMin: 22.954653180000037
XMax: 56.01796902500007
YMax: 24.807361361000062
Spatial Reference: 4326  (4326)  LatestVCSWkid(0)



Drawing Info:
Renderer:
Simple Renderer:
Symbol:
Style: esriSFSBackwardDiagonal
Color: [230, 0, 0, 255]
Outline:
Style: esriSLSSolid
Color: [230, 0, 0, 255]
Width: 0
Label: N/A
Description: N/A
Transparency: 0
Labeling Info:
Advanced Query Capabilities:
Supports Statistics: true
Supports OrderBy: true
Supports Distinct: true
Supports Pagination: true
Supports TrueCurve: true
Supports Returning Query Extent: true
Supports Query With Distance: true
Supports Sql Expression: true
Supports Query With ResultType: false
Supports Returning Geometry Centroid: false
Supports Binning LOD: false
Supports Query With LOD Spatial Reference: false
Supports Percentile Statistics: true
Supports Having Clause: true
Supports Count Distinct: true
Supports Time Relation: true
Supports Sql Format: false
Supports Query Analytic: true
Supports Query With Current User: true


HasZ: false

HasM: false

Has Attachments: false

HTML Popup Type: esriServerHTMLPopupTypeAsHTMLText

Type ID Field: null

Fields:
• OBJECTID ( type: esriFieldTypeOID, alias: OBJECTID )
• DepletedArea ( type: esriFieldTypeDouble, alias: DepletedArea )
• SHAPE ( type: esriFieldTypeGeometry, alias: SHAPE )
• SHAPE.STArea() ( type: esriFieldTypeDouble, alias: SHAPE.STArea() )
• SHAPE.STLength() ( type: esriFieldTypeDouble, alias: SHAPE.STLength() )