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Coastal_StormTide_Sea_Levels (FeatureServer)

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Service Description: The Coastal Inundation - High Water Level layer includes maximum sea levels values across the Auckland region. Extreme sea-levels for Auckland are based on the joint probability of a high tide, a storm surge (which is the rise in sea-level caused by wind action and low barometric pressure related to storm events), and waves. These processes can combine in a number of ways to inundate low-lying coastal margins, and coastal flooding occurs when the high water level exceeds the height of the land. The high water level values were used to determine the coastal inundation hazard along Auckland’s coastline, which is covered in a separate Geomaps layer.

Service ItemId: 4d1cae33bbe04e20a00835770fc63833

Has Versioned Data: false

Max Record Count: 2000

Supported query Formats: JSON

Supports applyEdits with GlobalIds: False

Supports Shared Templates: True

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Layers:

Description:

The high water level values (1% AEP + 1 msl) are used to calculate the required height of habitable floors for developments in the coastal inundation hazard zone, as per Unitary Plan rules. The dataset is primarily for the use of Regulatory and is included as part of the “Calculating Coastal Inundation Levels for the Auckland Region” training.

High sea level values for Auckland were collected between 2013 and 2019, via four separate studies:

  • In 2013, Auckland Council’s Civil Defence & Emergency Management Department commissioned NIWA to calculate and model coastal-storm inundation elevations for the entire Auckland region, primarily for emergency management purposes. NIWA calculated extreme high-water level values at fixed locations across the region, focusing on the open coasts and harbour areas.

  • In 2016, NIWA calculated high water level values for the east coast estuaries.

  • In 2020, DHI calculated high water levels for the Parakai/Helensville area to the south of the Kaipara Harbour. Inundation in this area is particularly complex due to the wide, low lying coastal plains sitting above the confluence of the Kaipara river with the harbour.

  • Also in 2019, NIWA calculated high water levels for Great Barrier and Little Barrier for 16 sites at ARI scenarios of 1, 2, 5, 10, 20, 50 and 100 years

Details of each study and the high water level calculations are available in Technical Report 2020/024 (Auckland’s Exposure to Coastal Inundation by Storm-tides and Waves December 2020).



Copyright Text: This has been consolidateted data from NIWA and Auckland Council’s Civil Defence & Emergency Management Department. This data has been provided to us by Tracy Howe Capex Programme, Engineering & Technical Services.

Spatial Reference: 2193 (2193)

Initial Extent:
Full Extent:
Units: esriMeters

Child Resources:   Info   SharedTemplates

Supported Operations:   Query   ConvertFormat   Get Estimates   Create Replica