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.