HICO Data User s Proposal HICO for Optical Active Constituents Retrieval applied to Amazon floodplain Lakes

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Principal Investigator HICO Data User s Proposal HICO for Optical Active Constituents Retrieval applied to Amazon floodplain Lakes Cláudio Clemente Faria Barbosa, National Institute For Space Research (INPE) Astronautas Avenue, 1758, Jd. Granja, São José dos Campos - São Paulo State Brazil Postal Code : 12227-010 Phone: (55) (12) 3208-6480 claudio@dpi.inpe.br Co Investigators: Evlyn Márcia Leão de Moraes Novo, National Institute For Space Research (INPE), Remote Sensing Division DSR, e-mail address : evlyn@dsr.inpe.br Lênio Soares Galvão, National Institute For Space Research (INPE), Remote Sensing Division DSR, e-mail address : lenio@dsr.inpe.br Enner Herenio de Alcântara. Universidade Estadual Paulista (UNESP) Campus de Presidente Prudente. e-mail address : ennerha@gmail.com Lino Augusto Sander de Carvalho. PhD. Candidate from the Remote Sensing Course, National Institute For Space Research (INPE), e-mail address : lino@dsr.inpe.br Abstract The Solimões-Amazonas floodplain has a singular ecological, biogeochemical and socioeconomic behavior inside the Amazon biome. However, floodplain systems are poorly known and studied, specially the optical components aspects. This proposal focuses on the study of optical properties of the lake Lago Grande Curuai (LGC), which is a part of the Amazon River floodplain. A dataset of Inherent and Apparent Optical Properties have been constructed from in situ measurements and will be used in an inverse modeling approach to retrieve Optical Active Components (OAC) concentrations from airborne and orbital remote sensing. Then, HICO hyperespectral sensor represents an excellent choice because its radiometric and spectral specifications have potential for retrieving OAC from optically complex waters. HICO images will be

used, coupled with in situ data, as an alternative to assess our analytical inverse model approach. A comparison with airborne data is also proposed. Statement of work This research is part of a PhD thesis developed to assess the application of HICO images, integrated with in situ measurements for estimating Total Suspended Solids (TSS) and Chlorophyll-a (Chl) concentrations in highly turbid waters of Amazon River floodplain lakes. In situ measurements of inherent optical properties (absorption, scattering and attenuation coefficients) and apparent (upward radiance, downward irradiance (E d ), remote sensing reflectance (R rs ) and diffuse attenuation coefficient (K d )) are being collected in field campaigns. A specific set of measurements will be carried out concurrently to an airborne mission equipped with the hyperspectral SpecTir. This mission is planned to be held in August 2013, and the dataset will be used on the development and test of Inverse Models for TSS and Chl-a estimation. Our proposal is to take advantage of the field mission effort to acquire HICO images, in order to assess their suitability as input to the Inverse Models. Project description Background The Remote Sensing of Inland Water Group (RSIWG) from the National Institute for Space Research (INPE), in the last two decades has contributed to the understanding of ecological, biogeochemical and socioeconomic factors affect aquatic systems. This effort is mainly focused on the Solimões-Amazonas floodplain lakes, which is a landscape baring extreme natural oscillation on river stage, known as "flood pulse", (Junk 1989). This flood pulse is the largest ecological force acting in the floodplain ecosystem requiring specific adaptations of the biota (Adis and Junk, 2002; Simone et al., 2003; Parolin 2010; Piedade 1997; Arraut 2008). However, Amazon floodplain systems are poorly known and studied, when compared to terrestrial Amazon ecosystems. Estimates made by Sippel et al. (1992) estimated more than 10 000 lakes with an area larger than one hectare (1 ha), in which less than 1% have been adequately studied. Particularly, studies that aim to characterize and estimate OAC concentrations and optical properties are even scarcer due to the dependence on in situ data, remotely sensed data and also well established analytical models. The knowledge built by RSIWG (Novo et al., 2004; Barbosa, 2005; Novo et al., 2006; Rudorff et al., 2007; Barbosa et al., 2009; Rudorff et al. 2009; Lobo et al., 2009, Lobo et al., 2011) shows that the use of in situ data collected under controlled conditions coupled with remote sensing data, allows the retrieval of OAC and their thermal properties (Alcantara et al., 2011), but it is necessary to move forward the use of analytical inversion methods to achieve more robust algorithms.

Some experimental Hyperspectral systems provided valuable insights into the potential of such images to the study of continental aquatic systems (Rudorff et al., 2007; Rudorff et al., 2009; Lobo et al., 2009) in tropical and subtropical regions. However, some of these systems, such as Hyperion / Earth Observing One (EO-1) and the Compact High Resolution Imaging Spectrometer (CHRIS / PROBA) ESA were not suitable for the study of natural and anthropogenic impacts on the Amazon floodplain. The main reasons were : 1) Very narrow swath, covering only partially water bodies area; 2) Unsuitable signal / noise ratio (SNR) for the low levels of radiation registered on water bodies Therefore, we believed that the HICO sensor, which was designed for applications in coastal areas may be suitable for Amazon regions. Table (1) shows HICO s potentialities for Amazon floodplains studies in the range of 400-900 nm. Despite its restrictive spatial resolution when compared to Hyperion and CHRIS / PROBA, HICO s signal to noise ratio and spectral range are more appropriate when applied to low signal water bodies. In relation to MERIS sensor, HICO s spatial resolution and the number of available bands are also encouraging. Table 1 Sensors Comparison Characterístics MERIS Hyperion CHRIS/PROBA HICO Spatial Resolution at nadir (m) 260 x 300 30 18 90 Spectral Resolution (nm) 390-1040 400-2500 410-1050 400-900 Swath (km) 1150 7,6 13.5 42 Number of Bands 15 220 63 87 SNR > 218 < 190 < 250 > 200 Project Goals The main objective of this proposal is to evaluate the application of HICO images to retrieve and map optically active constituents (OAC) in optically complex waters lakes (Case 2), from Amazon River floodplain. Semi-analytical models, based on concurrent in situ measurements (IOP and AOP) and HICO image will be used to retrieve OAC concentrations. A comparative analysis between the retrieves from the HICO and those obtained from the SpecTir will be also carried out. Study site The Lago Grande de Curuai (LGC) floodplain (01º50 S to 02º15 S and 55º00 W to 55º55 W), located along the Amazon River near Óbidos city (Brazil) 900 km upstream from the Atlantic Ocean (Fig. 1), is a complex system of about 30 shallow, interconnected lakes linked to the Amazon River by several channels including open water, flooded savannas and floating grasses. This study site represents the central region of the Amazon floodplain and has been subject of study for over 15 years by our

research group. This region also has suffered from anthropogenic processes that might have interfered in the local ecosystem (Renó et al, 2011) and affected light availability in the aquatic environment. Schedule and Plans Figura 1 Lago Grande Curuai Study Area As part of a Phd thesis from the student Lino Carvalho, three field campaigns were performed on 10/2012, 02/2013 and 03/2013 at 30 sampling stations distributed along the lake. The following data were acquired: profiles of absorption and attenuation coefficients (AC-S WetLabs), backscattering coefficients (Hydroscat 6p), measurements of upward radiance and downward irradiance (Ramses trios), dissolved oxygen, turbidity, ph, concentrations of chlorophyll-a, organic and inorganic colored dissolved organic matter (CDOM) and organic and inorganic suspended matter (TSS). A new field campaign, which includes a flight with a SpecTir airborne sensor, is scheduled for the period from 08/10/2013 to 08/15/2013. Considering the operational constraints, all field measurements follow the standard NASA protocol (Muller et. Al., 2000). Biographical sketch and available facilities Cláudio Clemente Faria Barbosa will lead this study in collaboration with Dr. Evlyn Novo, Dr. Lênio Soares Galvão, Dr. Enner Alcantara and his PhD student Lino Sander Augusto Sander de Carvalho. Dr, Claudio Barbosa is a researcher of the National Institute for Space Research (INPE) and has specialized in the use of remote sensing application to inland waters. During the development of his doctoral thesis, Dr. Claudio studied the water dynamics in the Curuai floodplain / Amazon River system. Dr.

Cláudio is also a professor at INPE s Remote Sensing Graduate Course as well as a Master and PhD advisor. The remote sensing group of inland waters of INPE has developed studies on remote sensing applications for monitoring the floodplain of the Amazonian rivers and reservoirs focusing on: building a spectral library and limnological characterization of Amazonian waters, in spatial dynamic of distribution of suspended sediment and chlorophyll and evaluation of trophic status of lakes in lowland Amazon. (Alcantara et al 2011, Affonso, et al, 2011, Barbosa et al 2010, Lobo et al 2009, Alcantara et al, 2008, Novo et al 2006). More recently the group has focused on measurements of apparent and inherent optical properties of Amazonian waters and hydroelectric reservoirs to support studies of carbon balance and the impact of sugar cane on water bodies. As part of this effort, the group acquired a series of equipment (listed below), and also hired Dr. Curtis Mobley to a two week course on Optical Oceanography and HydroLight. Also Lino Carvalho was selected to enroll on the Calibration and Validation for Ocean Color Remote Sensing, from the Maine University - USA, which will contribute to upgrade the group skills on field measurements and data processing. Available facilities The group has recently acquired the following equipments: a hyperspectral radiometer to measure radiance and irradiance (RAMSES - Trios), field spectrophotometers to measure attenuation and absorption coefficients (ACS-Wetlabs), equipment for measuring the backscatter coefficient (Hydroscat - HOBILabs), particle size meter (LISST - Sequoia) and fluorometers field (Turner Designs). (a) (b) Figura 2 - Equipments Acquired - (a) AC-S Sketch (b) Ship View Output and deliverables

1) A comparative analysis between the results obtained from the HICO data and results obtained from the Spectir airborne sensor for mapping total suspended sediments and chlorophyll in amazon floodplain lakes. 2) Yearly participation in HICO Data Team Meetings to present our ongoing results. References Adis, J.; W.J. Junk. Terrestrial invertebrates inhabiting lowland river floodplains of Central Amazonia and Central Europe: a review. Freshwater Biology, 47: 711 731, (2002). Affonso, A.G.; H. Queiroz,; E.M.L.M. Novo, Limnological characterization of undisturbed floodplain lakes in Central Amazon (Amazonas State, Brasil). Artigo Aceito pela Acta Limnológica Brasiliensia, (2011). Alcântara, E.; E.M.L.M. Novo, C.C.F. Barbosa, M.P. Bonnet, J.L. Stech, J.P. Ometto, Environmental factors associated with long-term changes in chlorophyll-a concentration in the Amazon floodplain. Biogeosciences discussion (Online), 8:3739-3770, (2011). Arraut, E.M. Migração do peixe-boi amazônico: uma abordagem por sensoriamento remoto, radiotelemetria e geoprocessamento. English Title: Migration of the Amazonian manatee (Peixe-Boi): an approach using remote sensing, GIS and radiotelemetry. Thesis in Remote Sensing. Instituto Nacional de Pesquisas Espaciais, São José dos Campos, (2008). Barbosa, C.C.F. Sensoriamento remoto da dinâmica de circulação da água do sistema planície de Curai/Rio Amazonas. English Title : Remote sensing of the water circulation dynamics on the Curai/Rio Amazonas floodplain. Thesis in Remote Sensing. Instituto Nacional de Pesquisas Espaciais, São José dos Campos, (2005). Barbosa, C.C.F., E.M.L.M. Novo, J.M. Melack, Gastil-Buhl, W. Pereira-Filho, Geospatial analysis of spatiotemporal patterns of ph, total suspended sediment and chlorophyll-a on the Amazon floodplain. Limnology, 11(2) :155-166, (2010). Junk,W.; P. B. Bayley, R. E. Sparks. The flood pulse concept in river floodplain system. Spec. Publ. Can. J. Fish. aquat. Sci.;106: 110 127, (1989). Lobo, F. L., C.C.F. Barbosa, E.M.L.M. Novo, J.S. Yunes. Mapping potential cyanobacterial bloom using Hyperion/EO-1 data in Patos Lagoon estuary. Acta Limnologica Brasiliensia, v. 21, n. 3, p. 299-308, (2009). Lobo, F. L., C.C.F. Barbosa, E.M.L.M. Novo, L.S. Galvão. Reference spectra to classify the Amazon water types. International Journal of Remote Sensing, v. 23, p. 3422-3442, (2011).

Novo, E.M.L.M; W. Pereira-Filho, J.M. Melack. Assessing the utility of spectral band operators to reduce the influence of total suspended solids on the relationship between chlorophyll concentration and the bidirectional reflectance factor in Amazon waters. International Journal of Remote Sensing. 25:5105-5116, (2004). Novo, E.M.L.M.; C.C.F. Barbosa, R.M.D. Freitas, Y.E. Shimabukuro, J.M. Melack, W. Pereira-Filho. Seasonal Changes in chlorophyll distributions in Amazon floodplain lakes derived from MODIS images. Limnology, 7:153-161, (2006). Mueller, J. L., C. Davis, R. Arnone, R. Frouin, K. L. Carder, Z. P. Lee, R. G. Steward, S. Hooker, C. D. Mobley, and S. McLean. Above- water radiance and remote sensing reflectance measurement and analysis protocols, NASA Tech. Mem., TM-2002-210004, 171 182, (2002). Parolin, P., C. Lucas, M.T.F. Piedade, F. Wittmann. Drought responses of flood-tolerant trees in Amazonian floodplains. Annals of botany, 105(1):129-39, (2010). Piedade, M. T. F., W.J. Junk, S.P. Long. Nutrient Dynamics of the Highly Productive C4 Macrophyte Echinochloa polystachya on the Amazon floodplain. Functional Ecology, 11(1):60-65, (1997). Renó, V.F., E.M.L.M. Novo, C. Suemitsu, C.D. Rennó, C. D.; T.S.F. Silva. Assessment of deforestation in the Lower Amazon floodplain using historical Landsat MSS/TM imagery. Remote Sensing of Environment, 115: 3446-3456 (2011). Rudorff, C.M.; Novo, E.M.L.M.; Galvão, L.S.; Pereira Filho, W. Análise derivativa de dados hiperespectrais medidos em nível de campo e orbital para caracterizar a composição de águas opticamente complexas na Amazônia. English Title : Derivative analysis of hyperspectral data measured in situ and orbital to characterize the composition of optically complex waters in the Amazon Acta Amazonica, 37:279-290, (2007). Rudorff, C.M.; L.S. Galvão, E.M.L.M. Novo. Reflectance of floodplain waterbodies using EO-1 Hyperion data from high and receding flood periods of the Amazon River. International Journal of Remote Sensing, 30:2713-2720 (2009). Simone, O.D., K. Haase, E. Muller, W.J. Junk, K. Hartmann, L. Schreiber, W. Schmidt. Apoplasmic Barriers and Oxygen Transport Properties of Hypodermal Cell Walls in Roots from Four Amazonian Tree Species. Plant Physiology, 32:206 217, (2003).