2012
DOI: 10.2112/jcoastres-d-11-00229.1
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Discrimination of Seagrass Species and Cover Classes within situHyperspectral Data

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Cited by 29 publications
(20 citation statements)
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“…Therefore, while the related VIs for seagrass species S were significantly different from those for the other two seagrass species, T and H (Table 5), such differences might reflect the influence of sediment type. However, in an earlier paper we found that spectral signatures of S measured in controlled laboratory setting were indeed distinct from T and H (Pu et al, 2012b). More samples of all seagrass species over different sediment types (if possible) may be needed to interpret better the results reported here.…”
Section: Discussionmentioning
confidence: 57%
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“…Therefore, while the related VIs for seagrass species S were significantly different from those for the other two seagrass species, T and H (Table 5), such differences might reflect the influence of sediment type. However, in an earlier paper we found that spectral signatures of S measured in controlled laboratory setting were indeed distinct from T and H (Pu et al, 2012b). More samples of all seagrass species over different sediment types (if possible) may be needed to interpret better the results reported here.…”
Section: Discussionmentioning
confidence: 57%
“…As a result, bottom (e.g., seagrass, sediment, etc.) spectra may be modified, thereby limiting the use of remote sensing (Dierssen et al, 2010;Holden and LeDrew, 2002;Pu et al, 2012b).…”
Section: Introductionmentioning
confidence: 99%
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“…Perbandingan sebaran rata-rata reflektansi spektral lamun menunjukkan pola yang memiliki dua puncak pada panjang gelombang sinar tampak yaitu hijau-kuning (500-650 nm) dan panjang gelombang merah (700-750 nm). Hal tersebut sesuai dengan penelitian Pu et al (2012) dan Fyfe (2003) yang mengukur pola reflektansi spektral lamun dan menunjukkan adanya puncak di panjang gelombang 500-650 nm dan 700-800 nm. Adanya kesamaan pola reflektansi tidak menunjukkan lima jenis lamun memiliki nilai yang sama karena pada dasarnya menurut Indarto (2014) reflektansi spektral setiap objek di permukaan bumi umumnya unik (bersifat khusus atau khas yang mencirikan objek) sehingga memiliki nilai yang berbeda dengan cirinya masingmasing.…”
Section: Pengukuran Reflektansi Spektralunclassified