MMO1065 Terrain Ruggedness Index of the South Plan area
This raster represents the Terrain Ruggedness Index (TRI) of the south plan area, as part of the exploritary work in the MMO1065 Enhancing our understanding of Seabed Habitats and Topographic Features project. Using updated digital terrain models, a TRI was created and used as the method to determine the ruggedness of the seabed.
dataset
http://environment.data.gov.uk/ds/catalogue/#/bf97a232051726a1ec83c6b832904ff4
description: A link to the web service or dataset
http://environment.data.gov.uk/ds/catalogue/#/catalogue
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MMO500009
eng
urn:ogc:def:crs:EPSG::4258
elevation
inlandWaters
revision
2008-01-06
revision
2009-11-16
-4.0589
2.0599
51.7124
49.3232
creation
1954-01-01
Bristol Channel
creation
1954-01-01
English Channel
creation
1954-01-01
North Sea
creation
2014-05-16
VIIf
creation
2014-05-16
IVc
creation
2014-05-16
VIIe
creation
2014-05-16
VIId
2014-04-22
2016-08-22
publication
2014-04-22
creation
2014-04-22
revision
2014-04-22
asNeeded
There are several mathematical approaches to calculating the ruggedness of a surface, all of which are based on the distribution or variations of height values in a given data sample. The method used in the MMO1065 project was a Terrain Ruggedness Index (TRI) mainly because it was developed for bathymetry-based analysis. In this approach, the TRI value is calculated by comparing the bathymetry value of a central pixel with the values of its 8 neighbours. The absolute differences between the value of the central pixel and the values of its neighbours are summed and then divided by 8 to calculate the TRI for the central pixel. A TRI score of 0 would indicate a completely flat surface; the bigger the number the more rugged the surface. To calibrate the TRI to produce a new hard/soft substrate classification system, the TRI results were assessed against ground truth data from both nautical charts from the UKHO and sediment and hard surface samples provided by BGS. TRI values for the bathymetry grid varied between 0 and 17.16, with a mean value of 0.19. By comparison a TRI value of 1 would indicate that a given cell was 1 m higher or lower than all its neighbouring cells. In the context of the Defra DEM, a TRI of 1 would mean a change in height of the seabed of about 4% between grid cells The TRI, created using the GDALDEM TRI algorithm, uses the method introduced by Valentine et al. (2004) that was an adaptation of the method developed by Riley et al. (1999) specifically for bathymetric analysis of the seabed. The algorithm was then applied for seafloor habitat mapping by Wilson et al. (2007).
Open Government Licence. Acknowledgement of Marine Management Organisation as source is required.
No limitations on access, however copyright should be used at all times.
Data/GIS Officer
Marine Management Organisation
originator
Data/GIS Officer
Marine Management Organisation
custodian
Data/GIS Officer
Marine Management Organisation
pointOfContact
2016-08-22