2018
DOI: 10.3390/atmos9030107
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Detecting Coastline Change with All Available Landsat Data over 1986–2015: A Case Study for the State of Texas, USA

Abstract: Coastline change often results from social and natural factors, such as human activities in the coastal zone, long-term and short-term sea level change, hurricane occurrences, subsequent recovery, and so on. Tracking coastline change is essential to deepen our understanding of coastal responses to these factors. Such information is also required for land use planning and sustainable development of coastal zones. In this context, we aimed to collect all available Landsat data (TM: Thematic Mapper, ETM+: Enhance… Show more

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Cited by 76 publications
(70 citation statements)
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References 65 publications
(84 reference statements)
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“…The method described in this work start from a rough shoreline at the pixel level for each of the Landsat scenes that defines the set of initial pixels where the analysis starts. Note that this initial line can be obtained in various ways such as the thresholds implemented in [20,[49][50][51]. Any other accessible line can also be used (such as the shoreline provided by the Instituto Hidrográfico de la Marina for the Spanish territory) but usually these are biased in a magnitude about one Landsat pixel (25-35 m).…”
Section: New Sub-pixel Methodological Solutionmentioning
confidence: 99%
“…The method described in this work start from a rough shoreline at the pixel level for each of the Landsat scenes that defines the set of initial pixels where the analysis starts. Note that this initial line can be obtained in various ways such as the thresholds implemented in [20,[49][50][51]. Any other accessible line can also be used (such as the shoreline provided by the Instituto Hidrográfico de la Marina for the Spanish territory) but usually these are biased in a magnitude about one Landsat pixel (25-35 m).…”
Section: New Sub-pixel Methodological Solutionmentioning
confidence: 99%
“…We selected only cloud-free and atmospherically corrected 30-m Landsat (TM: Thematic Mapper and OLI: Operational Image Processor) images acquired in non-flooding pre-monsoon season (Dec-April) to evaluate the geomorphological change of the coastline [27,35]. All the Landsat CDR (climate data records) images were pre-processed to L1T level (i.e., after standard terrain correction) with consistent geo-registration and within the prescribed tolerances (i.e., 12 m root-mean-square error) [11]. Due to the data availability and tidal level constraint (≤2.8 m), only some of the cloud-free images were suitable.…”
Section: Zonementioning
confidence: 99%
“…The coastline which has a dynamic nature refers to the most important line features on earth's surface (Alesheikh et al, 2007;Winarso et al, 2001). Monitoring coastline changes in time is essential to provide fundamental information about the situation that the environment in; due to this reason it is necessary to monitor the coastline dynamics with large spatial scales and for long time periods (Xu, 2018;Lui et al, 2017;Papakonstantinou et al, 2016). Calibrating and verifying numerical models (Kraus, 1988), assessment of sea level rise (Leatherman, 2001), identification of legal property boundaries (Morton and Speed, 1998) and coastal survey-monitoring (Smith and Jackson, 1992) are examples of coastline investigations conducted (Boak and Turner, 2005).…”
Section: Introductionmentioning
confidence: 99%