1378 IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 41, NO. 6, JUNE 2003
Satellite Hyperspectral Remote Sensing
for Estimating Estuarine and
Coastal Water Quality
Vittorio E. Brando and Arnold G. Dekker
Abstract—The successful launch of Hyperion in November
2000 bridged the gap between the high-resolution (spatial and
spectral) airborne remote sensing and the lower resolution satellite
remote sensing. Although designed as a technical demonstration
for land applications, Hyperion was tested for its capabilities
over a range of water targets in Eastern Australia, including
Moreton Bay in southern Queensland. Moreton Bay was the only
Australian Earth Observing 1 (EO-1) Hyperion coastal site used
for calibration/validation activities. This region was selected due
to its spatial gradients in optical depth, water quality, bathymetry,
and substrate composition. A combination of turbid and humic
river inputs, as well as the open ocean flushing, determines the
water quality of the bay. The field campaigns were coincident
with Hyperion overpasses, retrieved inherent optical properties,
apparent optical properties, substrate reflectance spectra, and
water quality parameters. Environmental noise calculations
demonstrate that Hyperion has sufficient sensitivity to detect
optical water quality concentrations of colored dissolved organic
matter, chlorophyll, and suspended matter in the complex waters
of Moreton Bay. A methodology was developed integrating
atmospheric and hydrooptical radiative transfer models (MOD-
TRAN-4, Hydrolight) to estimate the underwater light field. A
matrix inversion method was applied to retrieve concentrations
of chlorophyll, colored dissolved organic matter, and suspended
matter, which were comparable to those estimated in the field on
the days of the overpass.
Index Terms—Coastal waters, imaging spectrometry, numerical
radiative transfer modeling, remote sensing.
I. INTRODUCTION
T
HE EARTH Observing One (EO-1) satellite is the first
earth-observing platform of the National Aeronautics and
Space Administration’s (NASA) New Millennium Program
(NMP) designed for new technologies and strategies for
improving the quality of observations for NASA’s future plan-
etary and earth missions. The Hyperion Imaging Spectrometer
is the first high spatial resolution imaging spectrometer to
successfully orbit the earth [1]. The EO-1 orbit is almost
synchronous with the Landsat-7 and the Terra platform. The
results presented here form part of the Australian contribution
to the Hyperion Science Validation Team (SVT) Southern
Manuscript received July 1, 2002; revised January 8, 2003. This work was
supported in part by the Commonwealth Scientific and Industrial Research Or-
ganization Earth Observation Center and by the Cooperative Research Center
for Coastal Zone, Estuary and Waterways Management.
The authors are with the Commonwealth Scientific and Industrial Research
Organization Land and Water, Canberra, ACT 2601, Australia (e-mail
vittorio.brando@csiro.au; arnold.dekker@csiro.au).
Digital Object Identifier 10.1109/TGRS.2003.812907
Hemisphere campaign. The coastal site of Moreton Bay in
southeast Queensland, Australia, was chosen, as it has been
studied extensively and has a number of major active coastal
water quality monitoring and management projects. Moreton
Bay (Fig. 1) serves as a multiuse resource for a large population
in the Brisbane and southeast Queensland urban area and
requires regular monitoring information to ensure this resource
is being sustained. Research groups from the University of
Queensland (UQ) and the Commonwealth Scientific and
Industrial Research Organization (CSIRO) are cooperatively
developing remote sensing solutions to environmental moni-
toring [2].
During the SVT Southern Hemisphere campaign, Moreton
Bay imagery was acquired six times from December 2000 to
July 2001. A summer, autumn, and winter image are cloud free
for Deception Bay (January 12, 2001, April 2, 2001, July 7,
2001). During each Hyperion overpass, a limited set of spec-
troradiometric measurements and in situ sampling was carried
out by the UQ in Deception Bay. Two extensive joint field cam-
paigns were carried out in February 2001 and June 2001 to pa-
rameterize a biooptical model for Moreton Bay in both opti-
cally deep and shallow waters. The field campaign collected in-
herent and apparent optical properties, as well as concentrations
of water constituents and substrate reflectances. Using these
data as input to an analytical optical model, it was possible to
simulate the effect on subsurface irradiance reflectance
at any range of water quality variable concentrations, such as
colored dissolved organic matter, chlorophyll, and suspended
matter present at the time of a Hyperion overpass (provided the
specific inherent optical properties do not vary significantly).
By inverting this analytical model, it becomes possible to de-
termine the capacity of Hyperion to estimate concentrations of
water quality variables with a known degree of precision and
accuracy. The precision and accuracy of these estimates are a
function of the sensitivity of Hyperion, of the preprocessing,
and of the (inversion of the) analytical model. The resulting ap-
proaches demonstrate the potential of hyperspectral data and se-
lected bandwidths for water quality monitoring.
II. IMAGE PREPROCESSING
A. Radiometric Calibration
During the first year of the science validation, we received
Hyperion imagery at an “interim level of radiometric calibra-
tion” Level 1A_2. The most recent radiometric calibration dis-
tribution is at Level 1B_1, incorporating the knowledge gained
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