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(a) Location of the island of Niuatoputapu in the far north of the Lau Archipelago–Kingdom of Tonga. (b) True-color WorldView-2 satellite image of Niuatoputapu. (c) Digital terrain model derived from the image shown in panel b. (d ) Object-based classification of 18 ecologically meaningful seabed classes defined via interrogation of the image shown in panel b and examination of an exhaustive suite of ground-truth information collected in the field. Maps adapted with permission from the Khaled bin Sultan Living Oceans Foundation Global Reef Expedition. 

(a) Location of the island of Niuatoputapu in the far north of the Lau Archipelago–Kingdom of Tonga. (b) True-color WorldView-2 satellite image of Niuatoputapu. (c) Digital terrain model derived from the image shown in panel b. (d ) Object-based classification of 18 ecologically meaningful seabed classes defined via interrogation of the image shown in panel b and examination of an exhaustive suite of ground-truth information collected in the field. Maps adapted with permission from the Khaled bin Sultan Living Oceans Foundation Global Reef Expedition. 

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... Consequently, new methods have evolved that use satellite data to generate bathymetric charts [12,13]. Land-viewing sensors might not always have excellent spatial resolution when it comes to oceanic pixels located near shorelines whereas land-viewing sensors may not have great rates in terms of time leading to fewer number of satellite images which are cloud-free although this may particularly occur more often in areas such as rainy coastal tropics where cloudiness is frequent and high [7]. Moreover, bathymetric algorithms based on satellite telemetry, often draw on field data calibration [8,9,11,16,17] or a large number of calculations aimed at physically modeling general properties of the water column [10,12,13,14,15,18,19], and are frequently restricted to a single scene portrayed in either multispectral or hyperspectral images taken by space orbiters. ...
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Marine protected areas (MPAs) are the main tool for the conservation of coastal and marine ecosystems. However, historically their establishment and design has been driven by ease of implementation and political and socioeconomic concerns. Given the high cost of administrating large areas and small availability of resources, mainly economic, conservation should focus on areas where the efforts invested are efficient to minimize the loss of biodiversity and ecosystem services. In this study, using a systematic approach, we integrated habitat beta-diversity models and seascape metrics for the selection of priority conservation areas in Puerto Morelos Reef National Park (PMRNP). Five habitat classes were recognized from the analysis of quantitative estimates of benthic substrates from 111 sites: 1) seagrass dominated, 2) medium seagrass and sand cover, 3) sand dominated, 4) medium cover to algal dominance over calcareous matrix, and 5) reef crest. The habitat classes were employed to produce a thematic reef benthic habitat map (overall accuracy of 85.16% and a Kappa index of 0.80) using a supervised classification on a PlanetScope high-resolution satellite image from December 2021. The resulting thematic map was used to calculate shape complexity, connectivity, and habitat beta-diversity. The maps obtained were used to perform an iterative weighted overlay analysis, using all possible combinations of weighting values with 10% increments between layers. The resulting 83 layers were then integrated to obtain an optimal map that describes the priority conservation areas of the PNAPM, identifying four priority zones where management activities should be focused. The current zonation in the MPA’s management plan is not consistent with the priority areas identified from the spatially explicit analysis conducted. Therefore, the results obtained can help the managers in this important protected area to improve conservation efforts.
... However, LiDAR is still expensive for large-scale investigations. Similarly, drones with fluid lensing and structure-from-motion (SFM) technologies [50] facilitate centimeter-scale resolution [51] bathymetric mapping. But drone investigations are limited to comparatively small areas due to battery restrictions of quadcopters and fixed-wing remote-controlled aerial vehicles. ...
... The GBM rivers system is the mainstay of lowland water discharge and stability of the lowland biodiversity of the Bengal basin. These initiate in the Himalayas and transmit the expected yearly sediment of ~5 00 million tons to ~1 .4 billion tons [65][66][67]; Fig. 3d], discharge ~1 .5 million m 3 s − 1 during peak periods [68], and have a strong effect on the lowlands through sedimentation, though sedimentation is gradually decreasing in the delta (Fig. 3d) from the upstream due to anthropogenic activities [19,43,51]. In the Indian Green vegetation 1989 726 201 163 565 5118 2000 1271 358 235 811 4096 2014 660 1244 768 2761 1233 2020 397 2415 1457 2256 138 Fig. 7. MNDWI classification results from 1989 to 2020 and trend lines. ...
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Waterlogging is one of the major global problems which affects agro-economic activities around the world. In the coastal areas of Bangladesh, especially the southwestern coast, drainage congestion and waterlogging are very common which makes the area uninhabitable. Therefore, timely checking of drainage systems and surface water, and conveying data on the dynamics of drainages and surface water are important for plan and supervisory processes. The present study took an effort to illustrate the waterlogging and morphological change of the rivers in the southwestern coast of Bangladesh through the Modification Normalized Difference Water Index (MNDWI) values which are valuable indicators for monitoring the water area and land use pattern change. Landsat images (Landsat L8 Oli TIRS, Landsat ETM+, Landsat TM) were used in the research. The study reveals that from 1989 to 2020, the shallow water area (mostly covered with rivers) decreased by ~14.30 km2 yr− 1 , whereas the wet-land area (mostly covered with beels and water logging areas) increased by ~ 67.12 km2 yr− 1 . The bare land area also increased at a rate of ~ 36.90 km2 yr− 1 . On the other hand, the green vegetation decreased at a rate of ~166.1 km2 yr− 1 , whereas the moderate green vegetation area increased by ~ 69.77 km2 yr− 1 for the same period. In the coastal zones of Bangladesh, the polders, embankments, upstream dams, etc., enhance more sedimentation within the channels rather than in the nearby tidal plains. As a result, the shallow water area which is mostly covered by rivers is gradually decreasing. Moreover, due to increase in wet-land areas with salinity intrusions which affect the vegetation. Therefore, the green vegetation area is regularly declining due to demolition or conversion to moderate green vegetation. The findings of the research will be supportive for coastal scientists worldwide, policy makers & planners, and finally supportive for sustainable management of the coastal areas including Bangladesh.