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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Sub-pixel mapping for change detection in fluvial environments</dc:title><dc:creator>Stančič,	Liza	(Avtor)
	</dc:creator><dc:creator>Oštir,	Krištof	(Avtor)
	</dc:creator><dc:creator>Kokalj,	Žiga	(Avtor)
	</dc:creator><dc:creator>Čonč,	Špela	(Recenzent)
	</dc:creator><dc:creator>Rusjan,	Simon	(Recenzent)
	</dc:creator><dc:subject>bedload</dc:subject><dc:subject>gravel bars</dc:subject><dc:subject>monitoring</dc:subject><dc:subject>mountainous areas</dc:subject><dc:subject>multispectral data</dc:subject><dc:subject>optical images</dc:subject><dc:subject>remote sensing</dc:subject><dc:subject>rivers</dc:subject><dc:subject>soft classification</dc:subject><dc:subject>spectral mixture analysis</dc:subject><dc:subject>sub-pixel mapping</dc:subject><dc:description>Gravel   bars   are   dynamic   areas   of   bedload   deposition   in   rivers.   They   perform   important  ecological  functions  and  are  considered  indicators  of  changes  in  the  hydrological  characteristics  of  rivers.  Satellite  images  with  a  frequent  revisit  period  and  a  large  area  of  simultaneous  coverage  are  an  ideal  data  source  for  monitoring  many  natural  features  including  gravel  bars.  Openly  and  freely  available  remote  sensing data from the Sentinel-2 and Landsat systems have a spatial resolution that may be too coarse for accurate detection of gravel bars, especially in mountainous areas  where  rivers  and  related  features  are  narrow.  We  therefore  developed  a  sub-pixel mapping method based on spectral mixture analysis. Very high resolution aerial orthophotos and satellite images, as well as field mapping, were used as reference. Sentinel-2  and  Landsat  spectral  bands  were  supplemented  with  spectral  indices  to  increase  the  separability  between  land  cover  classes  of  interest.  Automatically  selected endmembers led to results with similar accuracy as when manually selected endmembers  were  used.  Endmembers  selected  on  one  image  of  the  study  area  during the leaf-on season could be used to analyse another image of the same study area acquired with the same remote sensing system at a different time. The fraction maps  were  found  to  be  more  accurate  than  maps  produced  by  hard  classification  with Spectral Angle Mapper using the same input data. Considering these findings, we  produced  fraction  maps  of  gravel,  vegetation,  and  water  presence  for  the  Soča  and Sava rivers in Slovenia, and the Vjosa river in Albania for a period of over 30 years. The  thematic  accuracy  of  the  maps  was  within  90%.  We  also  tested  the  ability  of  fraction maps for change detection and found that changes of at least 400 m2 could be  accurately  detected.  The  time  series  plots  can  also  be  used  to  detect  gravel  removal  as  demonstrated  at  known  excavation  sites  near  the  Dolje  settlement  on  Soča  and  near  Kranj  on  Sava.  The  current  study  contributes  to  science  with  new  insights   about   the   application   of   sub-pixel   mapping   for   monitoring   natural   processes.  The  developed  method  can  be  applied  to  study  areas  where  less  in  situ  data  are  available.  More  informed  management  decisions  can  be  made  based  on  newly acquired knowledge.</dc:description><dc:publisher>Založba ZRC</dc:publisher><dc:date>2026</dc:date><dc:date>2026-03-07 14:32:49</dc:date><dc:type>Neznano</dc:type><dc:identifier>28038</dc:identifier><dc:identifier>UDK: 528.8:553.624(0.034.2)</dc:identifier><dc:identifier>ISBN: 978-961-05-1094-9</dc:identifier><dc:identifier>DOI: 10.3986/9789610510949</dc:identifier><dc:identifier>COBISS_ID: 266440451</dc:identifier><dc:language>sl</dc:language><dc:rights>Nosilci avtorskih pravic na prispevkih so avtorji in ZRC SAZU</dc:rights></metadata>
