%0 Journal Article
%4 sid.inpe.br/plutao/2014/12.01.13.22.27
%2 sid.inpe.br/plutao/2014/12.01.13.22.28
%@doi 10.1016/j.rse.2014.06.013
%@issn 0034-4257
%F lattes: 2691497637313274 4 CurtarelliOgasAlcāStec:2014:CoReSe
%T Coupling remote sensing bio-optical and three-dimensional hydrodynamic modeling to study the phytoplankton dynamics in a tropical hydroelectric reservoir
%D 2015
%9 journal article
%A Curtarelli, Marcelo Pedroso,
%A Ogashawara, Igor,
%A Alcāntara, Enner Herenio de,
%A Stech, José Luiz,
%@affiliation Instituto Nacional de Pesquisas Espaciais (INPE)
%@affiliation Instituto Nacional de Pesquisas Espaciais (INPE)
%@affiliation Universidade Estadual Paulista (UNESP)
%@affiliation Instituto Nacional de Pesquisas Espaciais (INPE)
%@electronicmailaddress mpedroso@dsr.inpe.br
%@electronicmailaddress igoroga@dsr.inpe.br
%@electronicmailaddress enner@fct.unesp.br
%@electronicmailaddress stech@dsr.inpe.br
%B Remote Sensing of Environment
%V 157
%P 185-198
%K Bio-optical model, Horizontal surface phytoplankton distribution, Hydrodynamic modeling, Mixing regimes, Remote sensing.
%X The goal of this study was to determine the extent to which mixing and stratification processes influence the horizontal surface phytoplankton distribution in a tropical hydroelectric reservoir in Brazil. We used a synergistic approach that combines remote sensing bio-optical empirical and three-dimensional hydrodynamic modeling to represent phytoplankton dynamics. Seasonal differences were evaluated by simulating the bio-optical and the three-dimensional hydrodynamic models for two periods: the austral summer and winter of 2009. The three-dimensional hydrodynamic model simulations showed that the water column was completely mixed during winter; the water column remained stratified during summer. We also noticed a permanent thermocline during the summer between 15 and 25m in the reservoir. In both seasons, the surface current was wind driven and preferentially directed eastward. The bio-optical model showed that the horizontal surface phytoplankton distribution, as indicated by chlorophyll-a concentration, was heterogeneous during winter and homogenous during summer. Moreover, higher concentrations were observed by the empirical bio-optical model during winter (the highest mean areal concentration was 24μgL-1) than in summer (2.1μgL-1). This difference was explained by short timescale events, such as cold front passages, which contributed to the proliferation of phytoplankton in winter by enhancing vertical mixing in the water column. Lake number analysis showed that upwelling events were the most common mechanisms driving the mixing process during winter (LN<1 82% of the time). Combining remote sensing and three-dimensional hydrodynamic modeling makes it possible to more fully analyze the dynamics of the horizontal surface phytoplankton distribution under different meteorological conditions. The two modeling techniques can be used in a complementary manner and serve as an essential tool for the environmental monitoring of aquatic systems.
%@language en
%3 coupling remote.pdf