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Coastal_Inundation_High_Water_Levels (FeatureServer)

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Service Description: The Coastal Inundation - High Water Level layer includes predicted sea level values across the Auckland region for a range of probability events. High water 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 wave setup. (Dynamic wave processes like wave runup and overtopping are not included and should be considered on top of these water levels).

Service ItemId: ade7248eff3c44f8b79ff9b6a42fb84c

Has Versioned Data: false

Max Record Count: 2000

Supported query Formats: JSON

Supports applyEdits with GlobalIds: False

Supports Shared Templates: False

All Layers and Tables

Layers:

Description:

The high water levels are provided for a range of Average Recurrence Interval (ARI) events. Average recurrence interval is often referred to as a return period. These can be approximately converted to Annual Exceedance Probability (AEP), the probability of occurrence each year, by the following conversion table:

ARI (yr)

AEP (%)

2

50

5

20

10

10

20

5

50

2

100

1

The high water level values (1% AEP + 1 m sea level) are used to calculate the required height of habitable floors for developments in the coastal inundation hazard zone, as per Unitary Plan rules.

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

Credit:

Data supplied by Resilient Land and Coasts, Auckland Council

Use Limitations:

Constraints– General:

The high water level values were collated from tables within Technical Report 2020/024. They are made available in GIS to improve the workflow of Regulatory development engineers, specifically in relation to the calculation of habitable floor levels. The dataset is not meant to stand alone, and users outside of Regulatory should be directed to Technical Report 2020/024.

Constraints– Legal:

There are no legal constraints in relation to this dataset.

Constraints– Security:

Creative Commons – All Records



Copyright Text: Auckland Council

Spatial Reference: 2193 (2193)

Initial Extent:
Full Extent:
Units: esriMeters

Child Resources:   Info

Supported Operations:   Query   ConvertFormat   Get Estimates   Create Replica