@ElectronicSource{CostaTelmNovo::SpLiAt,
abstract = "Amazonian waters are commonly classified coarsely as white, black,
and clear, reflecting their differing composition of particulate
and dissolved compounds. Accordingly, the water light field and
the ecology of each of these water types also differ strongly.
Recent changes in land use are causing changes in river water
composition that cause shifts in the water light field.
Consequently, the quality and distribution of ecological habitats
must also be changing. We investigate and quantify changes in the
light field by reporting the first in situ spectral diffuse
attenuation and scalar irradiance measurements and accompanying
water optical constituents, including pigments determined by HPLC,
from a suite of large white, black, and clear rivers of the Amazon
Basin. Using this dataset, we evaluate the potential shifts in the
water light field of waters affected by thousands of small-scale
gold miners. Sampling was done during the high-water period along
a 500 km transect of the Amazon River and six of its larger
tributaries. Water samples were collected from the subsurface and
analyzed for chlorophyll a and other pigments, total suspended
solids, and colored dissolved organic matter. At each station,
vertical profiles of temperature, spectral downwelling irradiance
and upwelling radiance were taken from the surface down to the
depth of 1% light penetration (Zeu). Our results show that, for
the different types of waters, the diffuse attenuation coefficient
has different spectral and penetration depth behavior due to
varying proportions of dissolved and particulate compounds. In
white and black waters, the photosynthetic active radiation
becomes spectrally dominated by red light as a result of the high
attenuation by suspended sediments and colored dissolved organic
matter, respectively. Blue radiation is non-existent below the 0.5
depth. This is not the case for clear waters, which exhibit a
mid-spectra green light peak within the deep Zeu, and blue light
in only attenuated by 2.5 m. Applying these results to clear
waters that have been muddied by the injection of sediment from
mining, we show that significant changes in the distribution of
spectral scalar irradiance must occur, and that this would result
in a decrease (i) in photosynthetic activity, (ii) in the
production of organic matter photoproducts, (iii) in the size of
clear water habitats, and shifts in biological communities. .",
address = "S{\~a}o Jos{\'e} dos Campos",
affiliation = "University of Victoria, Department of Geography, Canada and
University of Victoria, School of Earth and Ocean Sciences,
Victoria, Canada and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
author = "Costa, Maycira P. F. and Telmer, Kevin and Novo, E. M. L. M.",
keywords = "water types, attenuation coefficient, scallar irradiance.",
language = "en",
lastupdatedate = "2006-12-13",
publisher = "Instituto and Nacional and de and Pesquisas and Espaciais",
ibi = "sid.inpe.br/ePrint@80/2006/12.12.17.56",
url = "http://urlib.net/ibi/sid.inpe.br/ePrint@80/2006/12.12.17.56",
targetfile = "v1.pdf",
title = "Spectral light attenuation in Amazonian waters",
typeofmedium = "On-line",
urlaccessdate = "20 maio 2024"
}