Applying Airborne LiDAR to Map Salt Marsh Inland Boundaries

The determination of rates and stocks of carbon storage in salt marshes, as well as their protection, require that we know where they and their boundaries are. Marsh boundaries are conventionally mapped through recognition of plant communities using aerial photography or satellite imagery. We examin...

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Autores principales: Lee B. van Ardenne, Gail L. Chmura
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Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/b5e1f33675bf4007b521018f87d895a3
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spelling oai:doaj.org-article:b5e1f33675bf4007b521018f87d895a32021-11-11T18:51:10ZApplying Airborne LiDAR to Map Salt Marsh Inland Boundaries10.3390/rs132142452072-4292https://doaj.org/article/b5e1f33675bf4007b521018f87d895a32021-10-01T00:00:00Zhttps://www.mdpi.com/2072-4292/13/21/4245https://doaj.org/toc/2072-4292The determination of rates and stocks of carbon storage in salt marshes, as well as their protection, require that we know where they and their boundaries are. Marsh boundaries are conventionally mapped through recognition of plant communities using aerial photography or satellite imagery. We examined the possibility of substituting the use of 1 m resolution LiDAR-derived digital elevation models (DEMs) and tidal elevations to establish salt marsh upper boundaries on the New Brunswick coasts of the Gulf of St. Lawrence and the Bay of Fundy, testing this method at tidal ranges from ≤2 to ≥4 m. LiDAR-mapped marsh boundaries were verified with high spatial resolution satellite imagery and a subset through field mapping of the upland marsh edge based upon vegetation and soil characteristics, recording the edge location and elevation with a Differential Geographic Positioning System. The results show that the use of high-resolution LiDAR and tidal elevation data can successfully map the upper boundary of salt marshes without the need to first map plant species. The marsh map area resulting from our mapping was ~30% lower than that in the province’s aerial-photograph-based maps. However, the difference was not primarily due to the location of the upper marsh boundaries but more so because of the exclusion of mudflats and large creeks (features that are not valued as carbon sinks) using the LiDAR method that are often mapped as marsh areas in the provincial maps. Despite some minor limitations, the development of DEMs derived from LiDAR can be applied to update and correct existing salt marsh maps along extensive sections of coastlines in less time than required to manually trace from imagery. This is vital information for governments and NGOs seeking to conserve these environments, as accurate mapping of the location and area of these ecosystems is a necessary basis for conservation prioritization indices.Lee B. van ArdenneGail L. ChmuraMDPI AGarticleblue carbontidal marsh limitsDEMGulf of St. LawrenceBay of FundyScienceQENRemote Sensing, Vol 13, Iss 4245, p 4245 (2021)
institution DOAJ
collection DOAJ
language EN
topic blue carbon
tidal marsh limits
DEM
Gulf of St. Lawrence
Bay of Fundy
Science
Q
spellingShingle blue carbon
tidal marsh limits
DEM
Gulf of St. Lawrence
Bay of Fundy
Science
Q
Lee B. van Ardenne
Gail L. Chmura
Applying Airborne LiDAR to Map Salt Marsh Inland Boundaries
description The determination of rates and stocks of carbon storage in salt marshes, as well as their protection, require that we know where they and their boundaries are. Marsh boundaries are conventionally mapped through recognition of plant communities using aerial photography or satellite imagery. We examined the possibility of substituting the use of 1 m resolution LiDAR-derived digital elevation models (DEMs) and tidal elevations to establish salt marsh upper boundaries on the New Brunswick coasts of the Gulf of St. Lawrence and the Bay of Fundy, testing this method at tidal ranges from ≤2 to ≥4 m. LiDAR-mapped marsh boundaries were verified with high spatial resolution satellite imagery and a subset through field mapping of the upland marsh edge based upon vegetation and soil characteristics, recording the edge location and elevation with a Differential Geographic Positioning System. The results show that the use of high-resolution LiDAR and tidal elevation data can successfully map the upper boundary of salt marshes without the need to first map plant species. The marsh map area resulting from our mapping was ~30% lower than that in the province’s aerial-photograph-based maps. However, the difference was not primarily due to the location of the upper marsh boundaries but more so because of the exclusion of mudflats and large creeks (features that are not valued as carbon sinks) using the LiDAR method that are often mapped as marsh areas in the provincial maps. Despite some minor limitations, the development of DEMs derived from LiDAR can be applied to update and correct existing salt marsh maps along extensive sections of coastlines in less time than required to manually trace from imagery. This is vital information for governments and NGOs seeking to conserve these environments, as accurate mapping of the location and area of these ecosystems is a necessary basis for conservation prioritization indices.
format article
author Lee B. van Ardenne
Gail L. Chmura
author_facet Lee B. van Ardenne
Gail L. Chmura
author_sort Lee B. van Ardenne
title Applying Airborne LiDAR to Map Salt Marsh Inland Boundaries
title_short Applying Airborne LiDAR to Map Salt Marsh Inland Boundaries
title_full Applying Airborne LiDAR to Map Salt Marsh Inland Boundaries
title_fullStr Applying Airborne LiDAR to Map Salt Marsh Inland Boundaries
title_full_unstemmed Applying Airborne LiDAR to Map Salt Marsh Inland Boundaries
title_sort applying airborne lidar to map salt marsh inland boundaries
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/b5e1f33675bf4007b521018f87d895a3
work_keys_str_mv AT leebvanardenne applyingairbornelidartomapsaltmarshinlandboundaries
AT gaillchmura applyingairbornelidartomapsaltmarshinlandboundaries
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