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Field spectroscopy of estuarine intertidal habitats

Forster, R.M. and Jesus, B. (2006) Field spectroscopy of estuarine intertidal habitats. International Journal of Remote Sensing, 27, 3657-3669. ISSN 0143-1161.

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Official URL: http://dx.doi.org/10.1080/01431160500500367

Abstract

The recent introduction of portable, low‐cost hyperspectral radiometers for measuring the reflectance of marine intertidal habitats has considerable promise, first as a source of reference spectra for airborne and satellite remote sensing, and second as a survey technique in its own right. This paper reports on the results of an intercalibration exercise in which two designs of commercially available instruments were used to measure reflectance spectra across a diverse, intertidal site. The substrates sampled included seagrasses, macroalgae, and sediments which varied in wetness and grain size. Spectra were compared statistically using several measures of similarity, and the results showed a high degree of correlation between the measured reflectance spectra. There were no significant differences between instruments from different manufacturers in the shape of reflectance spectra, but the signal‐to‐noise ratio varied considerably between individual instruments. Spectra measured by operators with lesser experience in field spectrometry tended to be more variable than those of more experienced operators, indicating that training and adherence to set protocols are important when implementing this method in the field situation. Spatial plots derived from field spectra showed essentially the same trends in surface features as plots created using traditional sampling and remote sensing methods. Furthermore, the use of field spectrometry as a stand‐alone, low‐cost method for rapidly mapping the distribution of major habitat types was demonstrated by the results of a survey of a large intertidal sandbank.

Item Type:Article
Institutes:Nederlands Instituut voor Ecologie (NIOO)
ID Code:11943
Deposited On:23 Nov 2011 01:00
Last Modified:31 Mar 2014 10:22

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