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Krieged BroadScale Substrate Map of Fulmar rMCZ

A geostatistical analysis of the data is reported leading to the selection of a linear model of corregionalization for the composition of the sediment, based on the additive log-ratio transformation of data on mud, sand and gravel content. This model is then used for spatial prediction on a 250-m grid. At each grid node a prediction distribution is obtained, conditional on neighbouring data and the selected model. By sampling from this distribution, and backtransforming onto the original compositional simplex of the data, we obtain a conditional expectation for the proportions of sand, gravel and mud at each location, a 95% confidence interval for the value at each node, and the probability that each of the four sediment texture classes that underlie the EUNIS habitat classification is found at the node.

Simple

Alternate title

GB400007

Date (Creation)
2015-03-30
Date (Publication)
2018-04-26
Citation identifier
EMODnetSeabedHabitats / GB400007
Point of contact
Organisation name Individual name Electronic mail address Role

Defra

open@defra.gsi.gov.uk

Owner

JNCC

habitatmapping@jncc.gov.uk

Custodian

GEMET - INSPIRE themes, version 1.0

  • Habitats and biotopes

http://inspire.ec.europa.eu/codelist/ReferenceHabitatTypeSchemeValue

  • Eunis

Use limitation

┬® Defra. Data may be re-used under the terms of the Open Government Licence.

Use limitation

geossAttribution

Access constraints
Other restrictions
Other constraints

no limitation

Spatial representation type
Vector
Denominator
100000
Language
English
Topic category
  • Biota
  • Oceans
N
S
E
W
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Begin date
2012-01-01
End date
2012-12-31
Supplemental Information

Lark, R.M.. 2015 Mapping seabed sediments of the Fulmar rMCZ. Nottingham, UK, British Geological Survey, 12pp. (OR/15/015) (Unpublished) Available from: http://nora.nerc.ac.uk/id/eprint/510587/

Reference system identifier
EPSG / WGS 84 (EPSG:4326) / 7.9

Topology level
Geometry only
Distribution format
Name Version

ESRI Shapefile

1.0

OnLine resource
Protocol Linkage Name

WWW:LINK-1.0-http--link

https://www.emodnet-seabedhabitats.eu/access-data/launch-map-viewer/?zoom=10&center=2.17705,56.35055&layerIds=501&baseLayerId=1&activeFilters=NobwRANghgngpgJwJIBMwC4CsAGAjAGjADMBLCAF0VQwBYB2Q0ixAGQHs2BrAVwAdUAzhmABdRmUoIAKnAAe5DGADiAIRrYN2OmAC+IoA

EMODnet Seabed Habitats Map Viewer

OGC:WMS

https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_view_maplibrary/wms?

gb400007

OGC:WFS

https://ows.emodnet-seabedhabitats.eu/geoserver/emodnet_open_maplibrary/wfs?

gb400007

WWW:LINK-1.0-http--link

https://files.emodnet-seabedhabitats.eu/data/EMODnetSBHsurvey_GB400007.zip

EMODnet Seabed Habitats download

Hierarchy level
Dataset

Conformance result

Title

Corrigendum to INSPIRE Metadata Regulation published in the Official Journal of the European Union, L 328, page 83

Date (Publication)
2009-12-15
Explanation

See the referenced specification

Pass
Yes

Conformance result

Title

Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services

Date (Publication)
2010-12-08
Explanation

See the referenced specification

Pass
Yes
Statement

The data used in this work were obtained by Cefas in 2012 (Ware & Meadows, 2013). A total of 65 stations were sampled by 0.1 m2 Hamon grab on a pre-planned survey grid. JNCC required that only PSA data supplied by JNCC specifically for this work should be used to produce the outputs. This is to remove compatibility issues arising from the use of PSA data originating from differing grab techniques. The data provided are percent by mass of gravel (particles diameter > 2mm), mud (particles diameter < 0.063 mm) and sand (particles 2mm > diameter > 0.063 mm).



Before modelling the linear coregionalization, exploratory spatial analysis was undertaken. There is a pronounced cluster of observations in the south west corner of the rMCZ, and the exploratory analysis indicated that this clustering was a potential source of artefacts for spatial modelling. Whilst some close-spaced observations are desirable for the estimation of spatial models, this pronounced clustering can cause problems because of over-representation of one part of the region (e.g. Marchant et al., 2013). For this reason the cluster of points was removed leaving 52 data for spatial modelling. All 65 data were used subsequently for mapping, as described in section 2.3. Auto-variograms and cross-variograms of the alr-transformed data were estimated from the data. The same method-of-moments estimator (MoM) was used as described by Lark et al. (2012). The linear model of coregionalization (LMCR) was fitted to the MoM estimates of the auto- and cross-variograms by weighted least squares, as described by Lark et al. (2012).



Lark et al. (2012) describe the cokriging procedure used to obtain conditional expectations of the transformed variables and covariance matrices for these at target points. This procedure was undertaken to form predictions at nodes of a 250-m grid. At this stage all 65 observations in the data set were used. The simulation method used by Lark et al. (2012) was then used to generate 5000 independent realizations from the joint prediction distribution at each node. For each realization a back-transformation was undertaken to give values of gravel, mud and sand. Over all realizations the mean value of gravel, mud and sand were computed as the conditional expectation of these variables, and the 0.025 and 0.975 quantiles of the realizations were computed as confidence intervals for the predictions. It should be noted that these predictions and confidence intervals should be considered for each variable in turn. For each realization, the EUNIS level 3 sediment texture classes (Long, 2006) were identified. At each grid node the proportion of realizations that occurred in each class is an estimate of the conditional probability of finding that class at the location. One may report the probability for each class, one may also report the class of maximum probability. The uncertainty attached to treating a site as if the class of maximum probability were the true class, can be evaluated by examining that maximum probability value, which may range from just over 1/k (where k is the number of classes) to 1.0.

Metadata

File identifier
5e247290-6076-48d4-9fe3-93a097f4ae83 XML
Metadata language
English
Character set
MD_CharacterSetCode_utf8
Hierarchy level
Dataset
Date stamp
2020-01-15T12:07:36
Metadata standard name

ISO19115

Metadata standard version

2003/Cor.1:2006

Metadata author
Organisation name Individual name Electronic mail address Role

JNCC

HabitatMapping@jncc.gov.uk

Point of contact
 
 

Overviews

Spatial extent

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Keywords

GEMET - INSPIRE themes, version 1.0

Habitats and biotopes


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