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A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

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A METHODOLOGICAL APPROACH TO STUDY THE DIFFERENCESBETWEEN THE RESULTS OBTAINED FROM THE SINOP-MT TOWER ANDOTHER LBA TOWERSSérgio Roberto de Paulo (iraesergio@uol.com.br), Nicolau Priante Filho, José de SouzaNogueira, Franklin Anderson de Oliveira Souza, Marcelo Sacardi Biudes e MauroMassao Shiota HayashiUniversidade Federal de M<strong>at</strong>o Grosso, Av. Fernando Correa da Costa s/n 78060-900George Louis Vourlitis (georgev@csusm.edu) Biological Sciences Program- CaliforniaSt<strong>at</strong>e University- San Marcos, CA 92096-0001, USAD<strong>at</strong>a concerning micrometeorological measurements obtained from towers installed in<strong>the</strong> <strong>Amazon</strong> Forest have indic<strong>at</strong>ed a mean carbon absorption r<strong>at</strong>e of 1-6 tC ha -1 yr -1 . Thetower situ<strong>at</strong>ed in Sinop-MT is an exception. D<strong>at</strong>a from Sinop tower have indic<strong>at</strong>edequilibrium of carbon flux when a whole year period is considered. The explan<strong>at</strong>ion for<strong>the</strong> difference between Sinop tower d<strong>at</strong>a and <strong>the</strong> d<strong>at</strong>a from <strong>the</strong> o<strong>the</strong>r towers can possiblybe found in <strong>the</strong> differences of <strong>the</strong> local ecosystem (<strong>the</strong> Sinop tower is situ<strong>at</strong>ed in <strong>at</strong>ransition forest), differences of <strong>the</strong> methodological procedures employed in Sinop (adifferent running mean, for example), or both. Here we consider a methodologicalprocedure to study <strong>the</strong>se differences applying it for 6 days Sinop d<strong>at</strong>a. This procedure isbased on three main analyses of <strong>the</strong> Sinop tower d<strong>at</strong>a th<strong>at</strong> basically is constituted bymethodological approaches employed by o<strong>the</strong>r LBA research groups in analyzing <strong>the</strong>ird<strong>at</strong>a. The three analyses are <strong>the</strong> following: 1) The applic<strong>at</strong>ion of an “u* filter” on <strong>the</strong>d<strong>at</strong>a in order to find some regularity between <strong>the</strong> carbon and energy balance closure and<strong>the</strong> level of turbulence of <strong>the</strong> air and wind velocity; 2) <strong>the</strong> recalcul<strong>at</strong>ion, from <strong>the</strong> rawd<strong>at</strong>a available when all equipment was running well, <strong>the</strong> micrometeorological variablesby employing a 800 s running mean, which is a value normally used by o<strong>the</strong>r eddy fluxmeasurement groups; and 3) <strong>the</strong> applic<strong>at</strong>ion of a Fourier analysis of <strong>the</strong> d<strong>at</strong>a in order toknow <strong>the</strong> diurnal and nocturnal low and high frequency of <strong>the</strong> variability of <strong>the</strong> d<strong>at</strong>a.The applic<strong>at</strong>ion of <strong>the</strong> three analyses possibly should improve <strong>the</strong> knowledge of <strong>the</strong>researchers of <strong>the</strong> LBA program on some open questions involved in <strong>the</strong> <strong>the</strong>oretical andexperimental procedures employed in <strong>the</strong> towers.

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