The Amazon Tall Tower Observatory (ATTO) in the remote Amazon basin: overview of first results from ecosystem ecology, meteorology, trace gas, and aerosol measurements.

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dc.contributorM. O. ANDREAE, Max Planck Institute for Chemistry / University of California San Diego
dc.contributorO. C. ACEVEDO, Universidade Federal Santa Maria
dc.contributorALESSANDRO CARIOCA DE ARAUJO, CPATU
dc.contributorP. ARTAXO, USP
dc.contributorC. G. G. BARBOSA, UFPR
dc.contributorH. M. J. BARBOSA, USP
dc.contributorJ. BRITO, USP
dc.contributorS. CARBONE, USP
dc.contributorX. CHI, Max Planck Institute for Chemistry
dc.contributorB. B. L. CINTRA, INPA
dc.contributorN. F. DA SILVA, INPA
dc.contributorN. L. DIAS, UFPR
dc.contributorC. Q. DIAS-JÚNIOR, IFPA / INPA
dc.contributorF. DITAS, Max Planck Institute for Chemistry
dc.contributorR. DITZ, Max Planck Institute for Chemistry
dc.contributorA. F. L. GODOI, UFPR
dc.contributorR. H. M. GODOI, UFPR
dc.contributorM. HEIMANN, Max Planck Institute for Biogeochemistry
dc.contributorT. HOFFMANN, Johannes Gutenberg University
dc.contributorJ. KESSELMEIER, Max Planck Institute for Chemistry
dc.contributorT. KÖNEMANN, Max Planck Institute for Chemistry
dc.contributorM. L. KRÜGER, Max Planck Institute for Chemistry
dc.contributorJ. V. LAVRIC, Max Planck Institute for Biogeochemistry
dc.contributorA. O. MANZI, INPA
dc.contributorD. MORAN-ZULOAGA, Max Planck Institute for Chemistry
dc.contributorA. C. NÖLSCHER, Max Planck Institute for Chemistry
dc.contributorD. SANTOS NOGUEIRA, CENSIPAM
dc.contributorM. T. F. PIEDADE, INPA
dc.contributorC. PÖHLKER, Max Planck Institute for Chemistry
dc.contributorU. PÖSCHL, Max Planck Institute for Chemistry
dc.contributorL. V. RIZZO, USP
dc.contributorC.-U. RO, Inha University
dc.contributorN. RUCKTESCHLER, Max Planck Institute for Chemistry
dc.contributorL. D. A. SÁ, INPE
dc.contributorM. D. O. SÁ, INPA
dc.contributorC. B. SALES, INPA / CESP/UEA
dc.contributorR. M. N. D. SANTOS, UEA
dc.contributorJ. SATURNO, Max Planck Institute for Chemistry
dc.contributorJ. SCHÖNGART, Max Planck Institute for Chemistry / INPA
dc.contributorM. SÖRGEL, Max Planck Institute for Chemistry
dc.contributorC. M. DE SOUZA, INPA / UFAM/ICSEZ-Parintins
dc.contributorR. A. F. DE SOUZA, UEA
dc.contributorH. SU, Max Planck Institute for Chemistry
dc.contributorN. TARGHETTA, INPA
dc.contributorJ. TÓTA, UEA / UFOPA
dc.contributorI. TREBS, Max Planck Institute for Chemistry
dc.contributorS. TRUMBORE, Max Planck Institute for Biogeochemistry
dc.contributorA. VAN EIJCK, Johannes Gutenberg University
dc.contributorD. WALTER, Max Planck Institute for Chemistry
dc.contributorZ. WANG, Max Planck Institute for Chemistry
dc.contributorB. WEBER, Max Planck Institute for Chemistry
dc.contributorJ. WILLIAMS, Max Planck Institute for Chemistry
dc.contributorJ. WINDERLICH, Max Planck Institute for Chemistry / Max Planck Institute for Biogeochemistry
dc.contributorF. WITTMANN, Max Planck Institute for Chemistry
dc.contributorS. WOLFF, Max Planck Institute for Chemistry / INPA
dc.contributorA. M. YÁÑEZ-SERRANO, Max Planck Institute for Chemistry / INPA.
dc.creatorANDREAE, M. O.
dc.creatorACEVEDO, O. C.
dc.creatorARAUJO, A.
dc.creatorARTAXO, P.
dc.creatorBARBOSA, C. G. G.
dc.creatorBARBOSA, H. M. J.
dc.creatorBRITO, J.
dc.creatorCARBONE, S.
dc.creatorCHI, X.
dc.creatorCINTRA, B. B. L.
dc.creatorSILVA, N. F. da
dc.creatorDIAS, N. L.
dc.creatorDIAS-JÚNIOR, C. Q.
dc.creatorDITAS, F.
dc.creatorDITZ, R.
dc.creatorGODOI, A. F. L.
dc.creatorGODOI, R. H. M.
dc.creatorHEIMANN, M.
dc.creatorHOFFMANN, T.
dc.creatorKESSELMEIER, J.
dc.creatorKÖNEMANN, T.
dc.creatorKRÜGER, M. L.
dc.creatorLAVRIC, J. V.
dc.creatorMANZI, A. O.
dc.creatorMORAN-ZULOAGA, D.
dc.creatorNÖLSCHER, A. C.
dc.creatorNOGUEIRA, D. S.
dc.creatorPIEDADE, M. T. F.
dc.creatorPÖHLKER, C.
dc.creatorPÖSCHL, U.
dc.creatorRIZZO, L. V.
dc.creatorRO, C.-U.
dc.creatorRUCKTESCHLER, N.
dc.creatorSÁ, L. D. A.
dc.creatorSÁ, M. D. O.
dc.creatorSALES, C. B.
dc.creatorSANTOS, R. M. N. dos
dc.creatorSATURNO, J.
dc.creatorSCHÖNGART, J.
dc.creatorSÖRGEL, M.
dc.creatorSOUZA, C. M. de
dc.creatorSOUZA, R. A. F. de
dc.creatorSU, H.
dc.creatorTARGHETTA, N.
dc.creatorTÓTA, J.
dc.creatorTREBS, I.
dc.creatorTRUMBORE, S.
dc.creatorEIJCK, A. van
dc.creatorWALTER, D.
dc.creatorWANG, Z.
dc.creatorWEBER, B.
dc.creatorWILLIAMS, J.
dc.creatorWINDERLICH, J.
dc.creatorWITTMANN, F.
dc.creatorWOLFF, S.
dc.creatorYÁÑEZ-SERRANO, A. M.
dc.date2015-12-14T11:11:11Z
dc.date2015-12-14T11:11:11Z
dc.date2015-12-14
dc.date2015
dc.date2015-12-14T11:11:11Z
dc.date.accessioned2026-06-30T23:42:29Z
dc.descriptionThe Amazon Basin plays key roles in the carbon and water cycles, climate change, atmospheric chemistry, and biodiversity. It already has been changed significantly by human activities, and more pervasive change is expected to occur in the next decades. It is therefore essential to establish long-term measurement sites that provide a baseline record of present-day climatic, biogeochemical, and atmospheric conditions and that will be operated over coming decades to monitor change in the Amazon region as human perturbations increase in the future. The Amazon Tall Tower Observatory (ATTO) has been set up in a pristine rain forest region in the central Amazon Basin, about 150 km northeast of the city of Manaus. An ecological survey including a biodiversity assessment has been conducted in the forest region surrounding the site. Two 80 m towers have been operated at the site since 2012, and a 325 m tower is nearing completion in mid-2015. Measurements of micrometeorological and atmospheric chemical variables were initiated in 2012, and their range has continued to broaden over the last few years. The meteorological and micrometeorological measurements include temperature and wind profiles, precipitation, water and energy fluxes, turbulence components, soil temperature profiles and soil heat fluxes, radiation fluxes, and visibility. A tree has been instrumented to measure stem profiles of temperature, light intensity, and water content in cryptogamic covers. The trace gas measurements comprise continuous monitoring of carbon dioxide, carbon monoxide, methane, and ozone at 5 to 8 different heights, complemented by a variety of additional species measured during intensive campaigns (e.g., VOC, NO, NO2, and OH reactivity). Aerosol optical, microphysical, and chemical measurements are made above the canopy as well as in the canopy space. They include light scattering and absorption, aerosol fluorescence, number and volume size distributions, chemical composition, cloud condensation nuclei (CCN) concentrations, and hygroscopicity. Initial results from ecological, meteorological, and chemical studies at the ATTO site are presented in this paper.
dc.identifierAtmospheric Chemistry and Physics Discuss, v. 15, n. 18, p. 11599-11726, 2015.
dc.identifierhttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1031648
dc.identifier10.5194/acpd-15-11599-2015
dc.identifier.urihttp://hdl.handle.net/123456789/388432
dc.languagepor
dc.rightsopenAccess
dc.subjectMonitoramento
dc.subjectClima
dc.subjectAmazonia
dc.titleThe Amazon Tall Tower Observatory (ATTO) in the remote Amazon basin: overview of first results from ecosystem ecology, meteorology, trace gas, and aerosol measurements.
dc.typeArtigo de periódico

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Embrapa Amazonía Oriental (CPATU)