@Article{MedeirosZoFrCoCeKa:2022:BiPrBr,
author = "Medeiros, Thais Andrade Galv{\~a}o de and Zoffoli, Mar{\'{\i}}a
Laura and Frouin, Robert and Cortivo, F{\'a}bio Dall and Cesar,
Gabriel Moiano and Kampel, Milton",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Consiglio
Nazionale delle Ricerche (CNR)} and {University California San
Diego} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Bio-optical properties of the Brazilian Abrolhos Bank?s shallow
coral-reef waters",
journal = "Frontiers in Remote Sensing",
year = "2022",
volume = "3",
pages = "986013",
keywords = "bio-optical properties, coral reefs, shallow water, Hyperspectral
remote sensing, PRISMA.",
abstract = "The Abrolhos Bank harbors the richest coral reef ecosystem in the
South Atlantic Ocean. It exhibits unique geomorphologic
structures, is localized in shallow depths, and is divided into
two reef regions with an inner arc close to the coast (320 m
depth) and an outer deeper arc (530 m depth). This study aims to
describe some bio-optical properties of the Abrolhos Bank waters
and to evaluate the performance of the inversion Hyperspectral
Optimization Processing Exemplar (HOPE) model, developed to
retrieve optical properties in shallow waters, in the region. To
this end, measurements at 75 stations during two field campaigns
conducted during the 2013 and 2016 wet seasons were analyzed, and
the HOPE model was applied to both in situ remote sensing
reflectance (Rrs) spectra and PRecursore IperSpettrale della
Missione Applicativa (PRISMA) imagery. Significant differences in
optical and biological properties were found between the two arcs.
The empirical relationships between chlorophyll-a concentration
(Chl-a) and absorption coefficient of phytoplankton at 440 nm
(aphy(440)) diverged from Bricauds models, suggesting differences
in phytoplankton diversity and cell size. In both arcs, total
non-water absorption coefficient at 440 nm (aT-w(440)) was
dominated by colored dissolved organic matter (CDOM) by ~60%.
Absorption coefficient by CDOM (acdom) presented a higher
variability within the outer arc, with the lowest contribution
from non-algal particles (NAPs), and the spectral slopes of aCDOM
resembled those of the inner arc. The spectral slopes of the NAP
absorption coefficient suggested a dominance by organic rather
than mineral particles that probably originated from biological
production. The HOPE model applied to in situ Rrs performed
satisfactorily for depth in the Abrolhos Bank waters, although
retrievals of aphy(440), CDOM plus NAP (adg(440)) and aT-w(440)
were underestimated with a relative bias of \−27.9%,
\−32.1% and \−45.8%, respectively. The HOPE model
retrievals from the PRISMA image exhibited low aphy(440) values
over the whole scene and the highest adg(440) values in the
Caravelas river plume. Very shallow depths (\≤3 m), bottom
substrate reflectance used as input in the HOPE model, model
parametrization associated with the water complexity in the study
site, and uncertainties associated to Rrs measurements used as
input might be responsible for differences found when comparing
HOPE retrievals with in situ measurements.",
doi = "10.3389/frsen.2022.986013",
url = "http://dx.doi.org/10.3389/frsen.2022.986013",
issn = "2673-6187",
label = "lattes: 0063119667740811 6 MedeirosZoFrCoCeKa:2022:BiPrBr",
language = "pt",
targetfile = "frsen-03-986013.pdf",
urlaccessdate = "20 maio 2024"
}