A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
A Look at Amazon Basin Seasonal Dynamics with the Biophysical ... A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
Long term measurements of carbon dioxide, water and energy combined with thefetch analysis in central Amazonia.Araujo, A. C. de 1 , Nobre, A. D. 1 , Kruijt, B. 2 , Dallarosa, R. G. 1 , Von Randow, C .3 ,Manzi, A., Xavier, H. B. 1 , A. O. 3 , Dolman, A. J. 4 , Waterloo, M. J. 4 , Evans, J. G. 5 , Gash,J. H.C. 5 , Hodnett, M. G. 5 , Pacheco, V. B. 1 , Kabat, P. 21 Instituto Nacional de Pesquisas da Amazônia - INPA, Manaus, Brazil2 Alterra, Wageningen University, The Netherlands3 Centro de Previsão do Tempo e Estudos Climáticos – CPTEC, São Paulo, Brazil4 Vrije University, Amsterdam, The Netherlands5Centre for Ecology and Hydrology – CEH, Wallingford, United KingdomAv. André Araújo, 2936, INPA, Petropólis, Aloj 09, Projeto LBA - ManausFlux,CEP:69083-000, Tel: 00 55 92 643 3255E-mail: carioca@inpa.gov.brStudies by Grace et al. (1996) and Malhi et al. (1998) show high rates of net CO 2uptake by Amazon rain forest, suggesting that such forests may represent the “missing”carbon sink that is required to close the Earth's carbon budget. In contrast, atmosphericinversion models and analyses of satellite images suggest that important terrestrial sinksare located in the northern hemisphere (Schulze & Schimel, 2001). Therefore, muchuncertainty exists about the real location of the missing carbon sink. Araújo et al. (2002)and Aubinet et al. (2001) revealed variation in carbon uptake rates, distributed overdifferent areas in the same ecosystem. Such differences could be related to thetopography, associated with variation in soil water content and the depth to which wateris available to plants, leading to contrasting edaphic conditions for the functioning of thevegetation (Chauvel et al., 1987 e Hodnett et al., 1997). Fluxes of CO 2 , water andenergy have been measured by the eddy correlation technique for several years nearManaus. An investigation of the location of sources responsible for the measured fluxeswas performed using footprint models in the context of such landscape. Analysis offetch related to availability of energy has shown that when the wind blows from thenorthwest and southwest quadrants less radiation is available than in the others, withconsequently lower net carbon uptake rates. Also, the respiration rates are highersuggesting that the CO 2 respired from the valleys or drained from the plateaus is beingcaptured by the eddy covariance system.
- Page 120: Aerosols and Clouds in Amazonia: Dy
- Page 124: mechanisms involving ice particles,
- Page 128: Abstract submitted for presentation
- Page 132: Microscopic images of atmospheric a
- Page 136: Atmospheric Attenuation Of Total So
- Page 140: Effect of smoke aerosol particles f
- Page 144: Comparison of Rainwater composition
- Page 148: George VourlitisHudson SilvaCalifor
- Page 152: Sérgio de PauloTim BakerUniversida
- Page 156: Long-term data indicate a strong ne
- Page 160: Atmospheric boundary layer measurem
- Page 164: 10 . Richey, J. E., Melack, J. M.,
- Page 168: Carbon Release from Stems and Branc
- Page 174: Spatial variation of soil propertie
- Page 178: AbstractChris DoughtyUC IrvineLBA-e
- Page 182: Photosynthesis light curves of sun
- Page 186: Seasonality of Stem Respiration at
- Page 192: The role of seasonal variations in
- Page 196: Oxygen isotope ratio of CO 2 in for
- Page 200: ESTIMATION OF LEAF AREA INDEX USING
- Page 204: An attempt to model Manaus k34, k14
- Page 210: LEAF AREA INDEX MEASUREMENTS AT CAX
- Page 214: Modeling Net Ecosystem Exchange fro
- Page 218: Estimating above ground biomass in
Long term measurements of carbon dioxide, w<strong>at</strong>er and energy combined <strong>with</strong> <strong>the</strong>fetch analysis in central <strong>Amazon</strong>ia.Araujo, A. C. de 1 , Nobre, A. D. 1 , Kruijt, B. 2 , Dallarosa, R. G. 1 , Von Randow, C .3 ,Manzi, A., Xavier, H. B. 1 , A. O. 3 , Dolman, A. J. 4 , W<strong>at</strong>erloo, M. J. 4 , Evans, J. G. 5 , Gash,J. H.C. 5 , Hodnett, M. G. 5 , Pacheco, V. B. 1 , Kab<strong>at</strong>, P. 21 Instituto Nacional de Pesquisas da Amazônia - INPA, Manaus, Brazil2 Alterra, Wageningen University, The Ne<strong>the</strong>rlands3 Centro de Previsão do Tempo e Estudos Climáticos – CPTEC, São Paulo, Brazil4 Vrije University, Amsterdam, The Ne<strong>the</strong>rlands5Centre for Ecology and Hydrology – CEH, Wallingford, United KingdomAv. André Araújo, 2936, INPA, Petropólis, Aloj 09, Projeto LBA - ManausFlux,CEP:69083-000, Tel: 00 55 92 643 3255E-mail: carioca@inpa.gov.brStudies by Grace et al. (1996) and Malhi et al. (1998) show high r<strong>at</strong>es of net CO 2uptake by <strong>Amazon</strong> rain forest, suggesting th<strong>at</strong> such forests may represent <strong>the</strong> “missing”carbon sink th<strong>at</strong> is required to close <strong>the</strong> Earth's carbon budget. In contrast, <strong>at</strong>mosphericinversion models and analyses of s<strong>at</strong>ellite images suggest th<strong>at</strong> important terrestrial sinksare loc<strong>at</strong>ed in <strong>the</strong> nor<strong>the</strong>rn hemisphere (Schulze & Schimel, 2001). Therefore, muchuncertainty exists about <strong>the</strong> real loc<strong>at</strong>ion of <strong>the</strong> missing carbon sink. Araújo et al. (2002)and Aubinet et al. (2001) revealed vari<strong>at</strong>ion in carbon uptake r<strong>at</strong>es, distributed overdifferent areas in <strong>the</strong> same ecosystem. Such differences could be rel<strong>at</strong>ed to <strong>the</strong>topography, associ<strong>at</strong>ed <strong>with</strong> vari<strong>at</strong>ion in soil w<strong>at</strong>er content and <strong>the</strong> depth to which w<strong>at</strong>eris available to plants, leading to contrasting edaphic conditions for <strong>the</strong> functioning of <strong>the</strong>veget<strong>at</strong>ion (Chauvel et al., 1987 e Hodnett et al., 1997). Fluxes of CO 2 , w<strong>at</strong>er andenergy have been measured by <strong>the</strong> eddy correl<strong>at</strong>ion technique for several years nearManaus. An investig<strong>at</strong>ion of <strong>the</strong> loc<strong>at</strong>ion of sources responsible for <strong>the</strong> measured fluxeswas performed using footprint models in <strong>the</strong> context of such landscape. Analysis offetch rel<strong>at</strong>ed to availability of energy has shown th<strong>at</strong> when <strong>the</strong> wind blows from <strong>the</strong>northwest and southwest quadrants less radi<strong>at</strong>ion is available than in <strong>the</strong> o<strong>the</strong>rs, <strong>with</strong>consequently lower net carbon uptake r<strong>at</strong>es. Also, <strong>the</strong> respir<strong>at</strong>ion r<strong>at</strong>es are highersuggesting th<strong>at</strong> <strong>the</strong> CO 2 respired from <strong>the</strong> valleys or drained from <strong>the</strong> pl<strong>at</strong>eaus is beingcaptured by <strong>the</strong> eddy covariance system.