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

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

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Evidence of non-existence of a "spectral-gap" in turbulent d<strong>at</strong>ameasured above Rondonia, Brazil. Part II: <strong>Amazon</strong>ian PastureGannab<strong>at</strong>hula S.S.D. Prasad 1,* , Margarete O. Domingues 1 , Leonardo D. A. Sá 1 , Celso vonRandow 1 , Antônio O. Manzi 1 , Bart Kruijt 31. Labor<strong>at</strong>ório Associado de Meteorologia e Oceanografia, Centro de Previsão deTempo e Estudos Climáticos, Instituto Nacional de Pesquisas Espaciais, CP 515,12201-970, São José dos Campos, Brazil2. Alterra, P.O. Box 47,Wageningen, Ne<strong>the</strong>rlandsAbstract:Wavelet and Fourier analyses are used to identify <strong>the</strong> spectral characteristics of windvelocity (u, v, w components), temper<strong>at</strong>ure, humudity and CO 2 concentr<strong>at</strong>ion d<strong>at</strong>a sets,obtained during dry and wet seasons in a pasture in a deforested area in <strong>Amazon</strong>ian. Thed<strong>at</strong>a were measured in August (dry-season) and in December (wet-season), year of 2000, asa part of <strong>the</strong> Brazil/European Union LBA Tower Consortium, in southwestern part of<strong>Amazon</strong>ian region. Measurements are made <strong>at</strong> micrometeorological tower loc<strong>at</strong>ed in <strong>the</strong>Nossa Senhora Farm (10 o 045.7´ S, 62 o 21.4´ W) county of Ouro Preto D’Oeste. The fastresponse wind speed and temper<strong>at</strong>ure measurements, sampled <strong>at</strong> 10.42 Hz r<strong>at</strong>e, were madeusing a three-dimensional sonic anemometer (Solent A1012R, Gill Instruments), <strong>at</strong> aheight of 4 m. Analyses are performed over a wide frequency range, from <strong>the</strong> inertialsubrange domain up to one day time-scale. D<strong>at</strong>a are studied for a five day only spectrumand for one day mean spectra and cospectra. Results showed th<strong>at</strong> is not possible to identifyspectra gap in any of <strong>the</strong> investig<strong>at</strong>ed variables. This has important consequence in th<strong>at</strong>separ<strong>at</strong>ing <strong>the</strong> turbulence flow into mean and fluctu<strong>at</strong>ion components may not be valid.This also makes it difficult to determine a cutoff frequency for filtering <strong>the</strong> d<strong>at</strong>a. Thisabsence of a spectral gap is probably due to <strong>the</strong> non-st<strong>at</strong>ionary characteristics of turbulentfields above deforested area. A comparison is made <strong>with</strong> <strong>the</strong> turbulent spectra computedabove <strong>the</strong> <strong>Amazon</strong> rain forest in Rebio Jaru. Possible physical phenomena in tropicalmeteorology are proposed to explain <strong>the</strong> findings.__________________* Corresponding author.E-mail address: prasad@cptec.inpe.br

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