Decadal‐scale dynamics of an Amazonian mangrove caused by climate and sea level changes: Inferences from spatial–temporal analysis and digital elevation models

• Published in: Earth surface processes and landforms Vol. 43; no. 14; pp. 2876 - 2888
• Main Authors: Cohen, Marcelo C.L., Souza, Adriana V., Rossetti, Dilce F., Pessenda, Luiz C.R., França, Marlon Carlos
• Format: Journal Article
• Language: English
• Published: Bognor Regis Wiley Subscription Services, Inc 01.11.2018
• Subjects: Basins; Bragança mangrove; Climate change; Climate models; digital elevation model; Digital Elevation Models; Digital imaging; Dynamics; Earth; Elevation; Forces (mechanics); Mangroves; Migration; Organic chemistry; Photogrammetry; Pore water; Rain; Rainfall; Salinity; Salinity effects; Satellite imagery; Satellites; Sea level; Sea level changes; Sea level rise; Spatial analysis; Surveying; Temporal variations; Tidal flats; Tidal flooding; Time series; Topography (geology)
• DOI: 10.1002/esp.4440
• ISSN: 0197-9337

Sea level rise and climate change are major forces driving wetland dynamics. The northern Brazilian coast has one of the largest continuous mangrove areas on Earth, with the mangroves from the Bragança Peninsula, in eastern Amazonia, being the most representative ones. These mangroves have migrated into higher tidal flats over recent years. We analyzed spatial–temporal changes of vegetation units adapted to different physical–chemical conditions along the Bragança Peninsula in order to decipher possible causes responsible for such recent mangrove dynamics. The investigation was based on time series analysis of a 33‐year (1984–2017) database consisting of satellite and drone images. These data were combined with digital elevation models based on topographical data obtained by photogrammetry, theodolite and hydrotopographic devices. During this time frame, mangroves invaded 2.7 km2 of inner tidal flats, which is compatible with a rise in relative sea level (RSL) and with a rainfall decreasing. Such topography‐dependent dynamic suggests that an increased frequency of tidal inundation decreased porewater salinity and caused mangroves to expand into topographically higher grounds. However, the study area contains small basins, that are less affected by tidal inundation, and Avicennia trees are dying in these locations due to increased porewater salinity, probably caused by a decreased rainfall. We propose that climate and RSL are responsible for driving the death of mangroves in the study area, and their migration into the topographically highest tidal flats. Assuming a RSL rise of 5 mm/yr under stable rainfall, or a RSL rise of 3 mm/yr accompanied by decreased rainfall, it is projected that mangrove areas will expand by 2.93 or 1.35 km2, respectively, by the end of this century. The combination of photogrammetry with theodolite/hydrotopographic surveying proved to be an efficient and innovative process for monitoring and evaluating the impacts of global changes on mangroves. © 2018 John Wiley & Sons, Ltd. Surface Data Models obtained by photogrammetry (drone surveying) and theodolite/hydrotopographic surveying.