Sitios
L. V.
S. T.Discuss., 2010, 10, 18139–18195.
Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d [[http://pubs.rsc.org/en/content/articlelanding/2013/fd/c3fd00052d|link]]
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Instrumentation running at ZF2 is shown shown.
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!! Instruments
ZF2 - Rebio Cuieras - TT34
Sitios.Manaus-ZF2 History
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* Coarse mode particle number size distributions were measured using an OPC-Grimm Model 1.109 (300 nm–20 μm) (Optical Particle Counter).
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* Coarse mode particle number size distributions are measured using an OPC-Grimm Model 1.109 (300 nm–20 μm) (Optical Particle Counter).
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* Coarse mode particle number size distributions were measured using an OPC-Grimm Model 1.109 (300 nm–20 μm) (Optical Particle
Counter).
Counter).
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* Coarse mode particle number size distributions were measured using an OPC-Grimm Model 1.109 (300 nm–20 μm) (Optical Particle Counter).
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Measurements at this site varied from time to time. It generally includes:
* Aerosol particle absorption are measured using a MAAP photometer (MultiAngle Absorption Photometry – Thermo Inc., Model 5012) (Petzold et al., 2005).
* Aerosol particle scattering coefficients are measured using a three wavelength integrating nephelometer (TSI Model 3563) operating at 450, 550 and 700 nm (Anderson et al., 1996).
* Aerosol particle number size distribution in fine mode are measured using a mobility particle size spectrometers (10–500 nm) a TSI 3936 SMPS (Scanning Mobility Particle Sizer).
* Coarse mode particle number size distributions were measured using an OPC-Grimm Model 1.109 (300 nm–20 μm) (Optical Particle
Counter).
* Particle number concentrations are measured with condensation particle counters (TSI CPC models 3010, 3785 or 3772).
* Stacked Filter Units (SFU) are used to collect fine mode (Dp <2.0 μm) and coarse mode (Dp >2.0 μm) aerosols, with integrating periods ranging from 2 to 5 days.
* Aerosol particle absorption are measured using a MAAP photometer (MultiAngle Absorption Photometry – Thermo Inc., Model 5012) (Petzold et al., 2005).
* Aerosol particle scattering coefficients are measured using a three wavelength integrating nephelometer (TSI Model 3563) operating at 450, 550 and 700 nm (Anderson et al., 1996).
* Aerosol particle number size distribution in fine mode are measured using a mobility particle size spectrometers (10–500 nm) a TSI 3936 SMPS (Scanning Mobility Particle Sizer).
* Coarse mode particle number size distributions were measured using an OPC-Grimm Model 1.109 (300 nm–20 μm) (Optical Particle
Counter).
* Particle number concentrations are measured with condensation particle counters (TSI CPC models 3010, 3785 or 3772).
* Stacked Filter Units (SFU) are used to collect fine mode (Dp <2.0 μm) and coarse mode (Dp >2.0 μm) aerosols, with integrating periods ranging from 2 to 5 days.
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[[http://www.atmos-chem-phys.net/13/2391/2013/acp-13-2391-2013.html|L. V. Rizzo, P. Artaxo, T. Muller, A. Wiedensohler, M. Paix~ao, G. G. Cirino, A. Arana, E. Swietlicki, P. Roldin, E. O. Fors, K. T. Wiedemann, L. S. M. Leal and M. Kulmala, Long term measurements of aerosol optical properties at a primary forest site in Amazonia, Atmos. Chem. Phys., 2013, 13, 1–23]]
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[[http://www.atmos-chem-phys.net/10/11415/2010/acp-10-11415-2010.html|S. T. Martin, M. O. Andreae, D. Althausen, P. Artaxo, H. Baars, S. Borrmann, Q. Chen, D. K. Farmer, A. Guenther, S. S. Gunthe, J. L. Jimenez, T. Karl, K. Longo, A. Manzi, T. Pauliquevis, M. D. Petters, A. J. Prenni, U. P ̈oschl, L. V. Rizzo, J. Schneider, J. N. Smith, E. Swietlicki, J. Tota, J. Wang, A. Wiedensohler and S. R. Zorn, An overview of the Amazonian Aerosol Characterization Experiment 2008 (AMAZE-08), Atmos. Chem. Phys., 2010, 10, 11415-11438.]]
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[[http://pubs.rsc.org/en/content/articlelanding/2013/fd/c3fd00052d|
Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d ]]
Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d ]]
to:
[[http://pubs.rsc.org/en/content/articlelanding/2013/fd/c3fd00052d|Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d ]]
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[[http://pubs.rsc.org/en/content/articlelanding/2013/fd/c3fd00052d|
Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d ]]
Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d ]]
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Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d
to:
Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d [[http://pubs.rsc.org/en/content/articlelanding/2013/fd/c3fd00052d|link]]
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[[Attach:zf2_inside.png|Attach:zf2_inside_tb.png]]
Instrumentation running at ZF2 is shown shown.
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[[Attach:zf2_slide1.png|Attach:zf2_slide1_tb.png]]
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[[Attach:zf2_tower.png|Attach:zf2_tower_tb.png]][[Attach:zf2_cont.png|Attach:zf2_cont_tb.png]]
Detail of the TT34 tower at ZF2 (left) and measurement station (right) are shown.
Detail of the TT34 tower at ZF2 (left) and measurement station (right) are shown.
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!! Instruments
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This site is representative of near-pristine conditions during the wet season.
This forest site is located 60 km northwest to Manaus urban area, at the ZF2 Ecological Station (2.59S, 60.21W, 110 m asl), within the INPA (Brazilian National Institute for Amazonian Research) Cuieiras forest reserve.
There, fromthe point of view of aerosol properties, the wet season corresponds to the period Jan–Jun, whereas the dry season corresponds to Jul– Dec [Rizzo et al., 2013].
No biomass burning occurs in the reservation or close to the site. Most of the time, the prevailing trade winds blow over vast expanses of intact tropical forest before reaching the measurement tower. However, the site is affected by regional transport of pollutants, most of it from long-range transported biomass burning emissions during part of the year.
Observations are taken at the TT34 tower
All measurements are taken under dry conditions (RH 30–40%) by use of an automatic diffusion dryer in the sampling line[]. An inlet with 50% aerodynamic cut-off of 7 um is used for sampling. Inlet lines run fromthe measurement level (39 m agl, about 10 m above the canopy height) to an air-conditioned container at ground level. Housing for the researchers and a diesel generator that provide the power supply were located respectively 0.33 km and 0.72 km to the west of the sampling site (downwind). A detailed description of the ZF2 TT34 tower measurement site and surrounding area can be found in Martin et al [2010].
This forest site is located
There, from
No biomass burning occurs in the reservation or close to the site. Most of the time,
Observations are taken at the TT34 tower
All measurements are taken under dry conditions (RH 30–40%) by use of an automatic diffusion dryer in the sampling line[]. An inlet with 50% aerodynamic cut-off of 7 um is used for sampling. Inlet lines run from
to:
This forest site is located 60 km northwest to Manaus urban area, at the ZF2 Ecological Station (2.59S, 60.21W, 110 m asl), within the INPA (Brazilian National Institute for Amazonian Research) Cuieiras forest reserve. There, from the point of view of aerosol properties, the wet season corresponds to the period Jan–Jun, whereas the dry season corresponds to Jul– Dec [Rizzo et al., 2013].
No biomass burning occurs in the reservation or close to the site. During the wet season, the prevailing trade winds blow over vast expanses of intact tropical forest before reaching the measurement tower, thus representative of near-pristine conditions. However, during part of the year, the site is affected by regional transport of pollutants, most of it from long-range transported biomass burning emissions [Artaxo et al., 2013].
All measurements are taken under dry conditions (RH 30–40%) by use of an automatic diffusion dryer in the sampling line[]. An inlet with 50% aerodynamic cut-off of 7 um is used for sampling. Inlet lines run from the measurement level (39 m agl, about 10 m above the canopy height) to an air-conditioned container at ground level. These observations are taken at the TT34 tower. Housing for the researchers and a diesel generator that provide the power supply were located respectively 0.33 km and 0.72 km to the west of the sampling site (downwind). A detailed description of the ZF2 TT34 tower measurement site and surrounding area can be found in Martin et al [2010].
No biomass burning occurs in the reservation or close to the site. During the wet season, the prevailing trade winds blow over vast expanses of intact tropical forest before reaching the measurement tower, thus representative of near-pristine conditions. However, during part of the year, the site is affected by regional transport of pollutants, most of it from long-range transported biomass burning emissions [Artaxo et al., 2013].
All measurements are taken under dry conditions (RH 30–40%) by use of an automatic diffusion dryer in the sampling line[]. An inlet with 50% aerodynamic cut-off of 7 um is used for sampling. Inlet lines run from the measurement level (39 m agl, about 10 m above the canopy height) to an air-conditioned container at ground level. These observations are taken at the TT34 tower. Housing for the researchers and a diesel generator that provide the power supply were located respectively 0.33 km and 0.72 km to the west of the sampling site (downwind). A detailed description of the ZF2 TT34 tower measurement site and surrounding area can be found in Martin et al [2010].
Changed lines 11-13 from:
S. T. Martin, M. O. Andreae, D. Althausen, P. Artaxo, H. Baars, S. Borrmann, Q. Chen, D. K. Farmer, A. Guenther, S. S. Gunthe, J. L. Jimenez, T. Karl, K. Longo, A. Manzi, T. Pauliquevis, M. D. Petters, A. J. Prenni, U. P ̈oschl, L. V. Rizzo, J. Schneider, J. N. Smith, E. Swietlicki, J. Tota, J. Wang, A. Wiedensohler and S. R. Zorn, An overview of the Amazonian Aerosol Characterization Experiment 2008 (AMAZE-08), Atmos. Chem. Phys. Discuss., 2010, 10, 18139–18195.
to:
Paulo Artaxo, Luciana V. Rizzo, Joel F. Brito, Henrique M. J. Barbosa, Andrea Arana, Elisa T. Sena, Glauber G. Cirino, Wanderlei Bastos, Scot T. Martin and Meinrat O. Andrea: Atmospheric aerosols in Amazonia and land use change: from natural biogenic to biomass burning conditions. Faraday Discussions 165 (2013) doi: 10.1039/c3fd00052d
S. T. Martin, M. O. Andreae, D. Althausen, P. Artaxo, H. Baars, S. Borrmann, Q. Chen, D. K. Farmer, A. Guenther, S. S. Gunthe, J. L. Jimenez, T. Karl, K. Longo, A. Manzi, T. Pauliquevis, M. D. Petters, A. J. Prenni, U. P ̈oschl, L. V. Rizzo, J. Schneider, J. N. Smith, E. Swietlicki, J. Tota, J. Wang, A. Wiedensohler and S. R. Zorn, An overview of the Amazonian Aerosol Characterization Experiment 2008 (AMAZE-08), Atmos. Chem. Phys. Discuss., 2010, 10, 18139–18195.
S. T. Martin, M. O. Andreae, D. Althausen, P. Artaxo, H. Baars, S. Borrmann, Q. Chen, D. K. Farmer, A. Guenther, S. S. Gunthe, J. L. Jimenez, T. Karl, K. Longo, A. Manzi, T. Pauliquevis, M. D. Petters, A. J. Prenni, U. P ̈oschl, L. V. Rizzo, J. Schneider, J. N. Smith, E. Swietlicki, J. Tota, J. Wang, A. Wiedensohler and S. R. Zorn, An overview of the Amazonian Aerosol Characterization Experiment 2008 (AMAZE-08), Atmos. Chem. Phys. Discuss., 2010, 10, 18139–18195.
Added lines 1-20:
This site is representative of near-pristine conditions during the wet season.
This forest site is located 60 km northwest to Manaus urban area, at the ZF2 Ecological Station (2.59S, 60.21W, 110 m asl), within the INPA (Brazilian National Institute for Amazonian Research) Cuieiras forest reserve.
There, from the point of view of aerosol properties, the wet season corresponds to the period Jan–Jun, whereas the dry season corresponds to Jul– Dec [Rizzo et al., 2013].
No biomass burning occurs in the reservation or close to the site. Most of the time, the prevailing trade winds blow over vast expanses of intact tropical forest before reaching the measurement tower. However, the site is affected by regional transport of pollutants, most of it from long-range transported biomass burning emissions during part of the year.
Observations are taken at the TT34 tower
All measurements are taken under dry conditions (RH 30–40%) by use of an automatic diffusion dryer in the sampling line[]. An inlet with 50% aerodynamic cut-off of 7 um is used for sampling. Inlet lines run from the measurement level (39 m agl, about 10 m above the canopy height) to an air-conditioned container at ground level. Housing for the researchers and a diesel generator that provide the power supply were located respectively 0.33 km and 0.72 km to the west of the sampling site (downwind). A detailed description of the ZF2 TT34 tower measurement site and surrounding area can be found in Martin et al [2010].
!! References
L. V. Rizzo, P. Artaxo, T. Muller, A. Wiedensohler, M. Paix~ao, G. G. Cirino, A. Arana, E. Swietlicki, P. Roldin, E. O. Fors, K. T. Wiedemann, L. S. M. Leal and M. Kulmala, Long term measurements of aerosol optical properties at a primary forest site in Amazonia, Atmos. Chem. Phys., 2013, 13, 1–23
S. T. Martin, M. O. Andreae, D. Althausen, P. Artaxo, H. Baars, S. Borrmann, Q. Chen, D. K. Farmer, A. Guenther, S. S. Gunthe, J. L. Jimenez, T. Karl, K. Longo, A. Manzi, T. Pauliquevis, M. D. Petters, A. J. Prenni, U. P ̈oschl, L. V. Rizzo, J. Schneider, J. N. Smith, E. Swietlicki, J. Tota, J. Wang, A. Wiedensohler and S. R. Zorn, An overview of the Amazonian Aerosol Characterization Experiment 2008 (AMAZE-08), Atmos. Chem. Phys. Discuss., 2010, 10, 18139–18195.
This forest site is located 60 km northwest to Manaus urban area, at the ZF2 Ecological Station (2.59S, 60.21W, 110 m asl), within the INPA (Brazilian National Institute for Amazonian Research) Cuieiras forest reserve.
There, from the point of view of aerosol properties, the wet season corresponds to the period Jan–Jun, whereas the dry season corresponds to Jul– Dec [Rizzo et al., 2013].
No biomass burning occurs in the reservation or close to the site. Most of the time, the prevailing trade winds blow over vast expanses of intact tropical forest before reaching the measurement tower. However, the site is affected by regional transport of pollutants, most of it from long-range transported biomass burning emissions during part of the year.
Observations are taken at the TT34 tower
All measurements are taken under dry conditions (RH 30–40%) by use of an automatic diffusion dryer in the sampling line[]. An inlet with 50% aerodynamic cut-off of 7 um is used for sampling. Inlet lines run from the measurement level (39 m agl, about 10 m above the canopy height) to an air-conditioned container at ground level. Housing for the researchers and a diesel generator that provide the power supply were located respectively 0.33 km and 0.72 km to the west of the sampling site (downwind). A detailed description of the ZF2 TT34 tower measurement site and surrounding area can be found in Martin et al [2010].
!! References
L. V. Rizzo, P. Artaxo, T. Muller, A. Wiedensohler, M. Paix~ao, G. G. Cirino, A. Arana, E. Swietlicki, P. Roldin, E. O. Fors, K. T. Wiedemann, L. S. M. Leal and M. Kulmala, Long term measurements of aerosol optical properties at a primary forest site in Amazonia, Atmos. Chem. Phys., 2013, 13, 1–23
S. T. Martin, M. O. Andreae, D. Althausen, P. Artaxo, H. Baars, S. Borrmann, Q. Chen, D. K. Farmer, A. Guenther, S. S. Gunthe, J. L. Jimenez, T. Karl, K. Longo, A. Manzi, T. Pauliquevis, M. D. Petters, A. J. Prenni, U. P ̈oschl, L. V. Rizzo, J. Schneider, J. N. Smith, E. Swietlicki, J. Tota, J. Wang, A. Wiedensohler and S. R. Zorn, An overview of the Amazonian Aerosol Characterization Experiment 2008 (AMAZE-08), Atmos. Chem. Phys. Discuss., 2010, 10, 18139–18195.