Dataset
Greenland 1980 and 2010s landcover grids from Landsat 5 and Landsat 8
Abstract
This dataset consists of two landcover grids representing Greenland in the late 1980s and late 2010s, utilising Landsat 5 Thematic Mapper Top-Of-Atmosphere (TM TOA) and Landsat 8 Operational Land Imager Top-Of-Atmosphere (OLI TOA) imagery respectively.
The data creation involved rigorous preprocessing and image classification methodologies, detailed extensively in the paper by Grimes, M., Carrivick, J.L., Smith, M.W., et al. (2024), "Land cover changes across Greenland dominated by a doubling of vegetation in three decades," Sci Rep, 14, 3120. DOI: 10.1038/s41598-024-52124-1. The full methodology is also discussed in the supplementary material of the publication.
The resultant .tif grids are in integer format with values from 1 to 9 representing landcover class:
1 - Bad data/Cloud/Shadow
2 - Snow and Ice
3 - Wet ice and meltwater
4 - Freshwater
5 - Coarse sediment
6 - Fine-grained sediment
7 - Bedrock
8 - Tundra vegetation
9 - Dense/wet vegetation
The tif grids were produced using Google Earth Engine. All summer Landsat imagery was filtered by metadata, followed by topographical correction, resulting in a best-pixel mosaic for Greenland's periphery. Band ratios (NDSI, NDVI, NDWI) were computed and stacked with visible, NIR, and SWIR bands. A principal component analysis was conducted, retaining the first six principal components as bands, which were subsequently classified using a K-means clusterer and refined with a supervised random-forest classifier and a slope threshold was applied to discriminate shadows from dark water bodies more effective.
This dataset was generated through a NERC-funded PhD project at the University of Leeds (Grant NE/L002574/1).
Details
Previous Info: |
No news update for this record
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Previously used record identifiers: |
No related previous identifiers.
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Access rules: |
Public data: access to these data is available to both registered and non-registered users.
Use of these data is covered by the following licence(s): http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/ When using these data you must cite them correctly using the citation given on the CEDA Data Catalogue record. |
Data lineage: |
The data creation involved rigorous preprocessing and image classification methodologies and the full methodology is discussed in the supplementary material of the publication Grimes, M., Carrivick, J.L., Smith, M.W., et al. (2024), "Land cover changes across Greenland dominated by a doubling of vegetation in three decades," Sci Rep, 14, 3120. DOI: 10.1038/s41598-024-52124-1. |
File Format: |
TIF files
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Process overview
Instrument/Platform pairings
Landsat 8 Operational Land Imager (OLI) and Thermal InfraRed Sensor (TIRS) | Deployed on: Landsat 8 |
Mobile platform operations
Mobile Platform Operation 1 | Mobile Platform Operation for: Landsat 8 |
Instrument/Platform pairings
LANDSAT5 Thematic Mapper (TM) | Deployed on: Landsat 5 |
Mobile platform operations
Mobile Platform Operation 1 | Mobile Platform Operation for: Landsat 5 |
Computation Element: 1
Title | Computation for Greenland 1980 and 2010s landcover grids from Landsat 5 and Landsat 8 |
Abstract | the tif grids were produced using Google Earth Engine. All summer Landsat imagery was filtered by metadata, followed by topographical correction, resulting in a best-pixel mosaic for Greenland's periphery. Band ratios (NDSI, NDVI, NDWI) were computed and stacked with visible, NIR, and SWIR bands. A principal component analysis was conducted, retaining the first six principal components as bands, which were subsequently classified using a K-means clusterer and refined with a supervised random-forest classifier and a slope threshold was applied to discriminate shadows from dark water bodies more effective. |
Input Description | None |
Output Description | None |
Software Reference | None |
Output Description | None |
Output Description | None |
No variables found.
Temporal Range
1986-07-01T00:00:00
2019-09-30T00:00:00
Geographic Extent
84.0000° |
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-76.0000° |
-10.0000° |
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59.0000° |