Validation of a radiometric color model applicable to optically complex water bodies

Citation
Rp. Bukata et al., Validation of a radiometric color model applicable to optically complex water bodies, REMOT SEN E, 77(2), 2001, pp. 165-172
Citations number
16
Categorie Soggetti
Earth Sciences
Journal title
REMOTE SENSING OF ENVIRONMENT
ISSN journal
00344257 → ACNP
Volume
77
Issue
2
Year of publication
2001
Pages
165 - 172
Database
ISI
SICI code
0034-4257(200108)77:2<165:VOARCM>2.0.ZU;2-T
Abstract
A radiometric color model relating the color of optically complex (non-Case 1) waters to the organic and inorganic color-producing agents (CPA) respon sible for that color has been previously applied to the waters of Lake Onta rio. Canada and Lake Ladoga, Russia. Additional underwater optical measurem ents and water quality data from Lakes Erie and Michigan and several boreal takes in northern Ontario, as well as comparable data from the European ta kes Krasnoye, Zug, and Lucerne are utilized to illustrate both the validity of the model, as well as the universality of its application. It was found that, due to the limited availability of specific spectral scattering and absorption properties (optical cross-section spectra) for CPA indigenous to natural water bodies on a global scale, the use of optical cross-section s pectra appropriate to the CPA indigenous to Lake Ontario and those appropri ate to the CPA indigenous to Lake Ladoga provided a more-than-adequate surr ogate for the water bodies considered herein (inclusive of river systems in the British Columbia Canadian Cordillera for which results of a study rela ting river water color to hydrographic basin features are also revisited). Similarities among the optical cross-section spectra pertinent to freshwate r biota and similarities among the optical cross-section spectra pertinent to freshwater dissolved organic matter would appear to allow such a liberal use of site-specific aquatic optical properties. However., greatest discre pancies in indigenous inland water CPA optical cross-section spectra are co nsequences of global geologic diversities. A compensation for geologic dive rsities is illustrated by the use of Lake Ladoga cross-section spectra with the European lakes and the Lake Ontario cross-section spectra with the Nor th American lakes., also providing validation of both the radiometric model and its universality. Such geologic similarities could alleviate labor-, t ime-, and cost-intensive determinations of optical cross-section spectra fo r many inland water bodies. (C) 2001 Elsevier Science Inc. All rights reser ved.