Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning
<p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmosp...
Ausführliche Beschreibung
Autor*in: |
S. Rodrigues [verfasserIn] G. Cirino [verfasserIn] D. Moreira [verfasserIn] A. Pozzer [verfasserIn] R. Palácios [verfasserIn] S.-C. Lee [verfasserIn] B. Imbiriba [verfasserIn] J. Nogueira [verfasserIn] M. I. Vitorino [verfasserIn] G. Vourlitis [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2024 |
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Übergeordnetes Werk: |
In: Biogeosciences - Copernicus Publications, 2004, 21(2024), Seite 843-868 |
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Übergeordnetes Werk: |
volume:21 ; year:2024 ; pages:843-868 |
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Link aufrufen |
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DOI / URN: |
10.5194/bg-21-843-2024 |
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Katalog-ID: |
DOAJ101406134 |
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520 | |a <p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< | ||
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10.5194/bg-21-843-2024 doi (DE-627)DOAJ101406134 (DE-599)DOAJc59309e02bdb41008f8876c0993f54c9 DE-627 ger DE-627 rakwb eng QH540-549.5 QH501-531 QE1-996.5 S. Rodrigues verfasserin aut Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< Ecology Life Geology G. Cirino verfasserin aut G. Cirino verfasserin aut G. Cirino verfasserin aut D. Moreira verfasserin aut A. Pozzer verfasserin aut A. Pozzer verfasserin aut R. Palácios verfasserin aut R. Palácios verfasserin aut S.-C. Lee verfasserin aut B. Imbiriba verfasserin aut J. Nogueira verfasserin aut M. I. Vitorino verfasserin aut M. I. Vitorino verfasserin aut G. Vourlitis verfasserin aut In Biogeosciences Copernicus Publications, 2004 21(2024), Seite 843-868 (DE-627)392963957 (DE-600)2158181-2 17264189 nnns volume:21 year:2024 pages:843-868 https://doi.org/10.5194/bg-21-843-2024 kostenfrei https://doaj.org/article/c59309e02bdb41008f8876c0993f54c9 kostenfrei https://bg.copernicus.org/articles/21/843/2024/bg-21-843-2024.pdf kostenfrei https://doaj.org/toc/1726-4170 Journal toc kostenfrei https://doaj.org/toc/1726-4189 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 21 2024 843-868 |
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10.5194/bg-21-843-2024 doi (DE-627)DOAJ101406134 (DE-599)DOAJc59309e02bdb41008f8876c0993f54c9 DE-627 ger DE-627 rakwb eng QH540-549.5 QH501-531 QE1-996.5 S. Rodrigues verfasserin aut Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< Ecology Life Geology G. Cirino verfasserin aut G. Cirino verfasserin aut G. Cirino verfasserin aut D. Moreira verfasserin aut A. Pozzer verfasserin aut A. Pozzer verfasserin aut R. Palácios verfasserin aut R. Palácios verfasserin aut S.-C. Lee verfasserin aut B. Imbiriba verfasserin aut J. Nogueira verfasserin aut M. I. Vitorino verfasserin aut M. I. Vitorino verfasserin aut G. Vourlitis verfasserin aut In Biogeosciences Copernicus Publications, 2004 21(2024), Seite 843-868 (DE-627)392963957 (DE-600)2158181-2 17264189 nnns volume:21 year:2024 pages:843-868 https://doi.org/10.5194/bg-21-843-2024 kostenfrei https://doaj.org/article/c59309e02bdb41008f8876c0993f54c9 kostenfrei https://bg.copernicus.org/articles/21/843/2024/bg-21-843-2024.pdf kostenfrei https://doaj.org/toc/1726-4170 Journal toc kostenfrei https://doaj.org/toc/1726-4189 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 21 2024 843-868 |
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10.5194/bg-21-843-2024 doi (DE-627)DOAJ101406134 (DE-599)DOAJc59309e02bdb41008f8876c0993f54c9 DE-627 ger DE-627 rakwb eng QH540-549.5 QH501-531 QE1-996.5 S. Rodrigues verfasserin aut Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< Ecology Life Geology G. Cirino verfasserin aut G. Cirino verfasserin aut G. Cirino verfasserin aut D. Moreira verfasserin aut A. Pozzer verfasserin aut A. Pozzer verfasserin aut R. Palácios verfasserin aut R. Palácios verfasserin aut S.-C. Lee verfasserin aut B. Imbiriba verfasserin aut J. Nogueira verfasserin aut M. I. Vitorino verfasserin aut M. I. Vitorino verfasserin aut G. Vourlitis verfasserin aut In Biogeosciences Copernicus Publications, 2004 21(2024), Seite 843-868 (DE-627)392963957 (DE-600)2158181-2 17264189 nnns volume:21 year:2024 pages:843-868 https://doi.org/10.5194/bg-21-843-2024 kostenfrei https://doaj.org/article/c59309e02bdb41008f8876c0993f54c9 kostenfrei https://bg.copernicus.org/articles/21/843/2024/bg-21-843-2024.pdf kostenfrei https://doaj.org/toc/1726-4170 Journal toc kostenfrei https://doaj.org/toc/1726-4189 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 21 2024 843-868 |
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10.5194/bg-21-843-2024 doi (DE-627)DOAJ101406134 (DE-599)DOAJc59309e02bdb41008f8876c0993f54c9 DE-627 ger DE-627 rakwb eng QH540-549.5 QH501-531 QE1-996.5 S. Rodrigues verfasserin aut Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< Ecology Life Geology G. Cirino verfasserin aut G. Cirino verfasserin aut G. Cirino verfasserin aut D. Moreira verfasserin aut A. Pozzer verfasserin aut A. Pozzer verfasserin aut R. Palácios verfasserin aut R. Palácios verfasserin aut S.-C. Lee verfasserin aut B. Imbiriba verfasserin aut J. Nogueira verfasserin aut M. I. Vitorino verfasserin aut M. I. Vitorino verfasserin aut G. Vourlitis verfasserin aut In Biogeosciences Copernicus Publications, 2004 21(2024), Seite 843-868 (DE-627)392963957 (DE-600)2158181-2 17264189 nnns volume:21 year:2024 pages:843-868 https://doi.org/10.5194/bg-21-843-2024 kostenfrei https://doaj.org/article/c59309e02bdb41008f8876c0993f54c9 kostenfrei https://bg.copernicus.org/articles/21/843/2024/bg-21-843-2024.pdf kostenfrei https://doaj.org/toc/1726-4170 Journal toc kostenfrei https://doaj.org/toc/1726-4189 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 21 2024 843-868 |
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S. Rodrigues misc QH540-549.5 misc QH501-531 misc QE1-996.5 misc Ecology misc Life misc Geology Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning |
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Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning |
abstract |
<p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< |
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<p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< |
abstract_unstemmed |
<p<Carbon cycling in the Amazon fundamentally depends on the functioning of ecosystems and atmospheric dynamics, which are highly intricate. Few studies have hitherto investigated or measured the radiative effects of aerosols on the Amazon and Cerrado. This study examines the effects of atmospheric aerosols on solar radiation and their effects on net ecosystem exchange (NEE) in an area of semideciduous tropical forest in the north of Mato Grosso. Our results show that for a relative irradiance (<span class="inline-formula"<<i<f</i<</span<) 1.10–0.67, a decrease in incident solar radiation is associated with a reduction in the NEE. However, an average increase of 25 %–110 % in NEE was observed when pollution levels and aerosol optical depth (AOD) were above <span class="inline-formula"<≈ 1.25</span< and <span class="inline-formula"<<i<f</i<</span< <span class="inline-formula"<<</span< 0.5. The increase NEE was attributed to the increase of up to 60 % in the diffuse fraction of photosynthetically active radiation. The change in AOD and <span class="inline-formula"<<i<f</i<</span< was mainly attributable to biomass burning organic aerosols from fires. Important influences on vapor pressure deficit (VPD) as well as air temperature (<span class="inline-formula"<<i<T</i<<sub<air</sub<</span<) and canopy (LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<), induced by the interaction between solar radiation and high aerosol load in the observation area, were also noticed. On average, a cooling of about 3–4 <span class="inline-formula"<<sup<∘</sup<</span<C was observed for <span class="inline-formula"<<i<T</i<<sub<air</sub<</span< and LC<span class="inline-formula"<<sub<<i<T</i<</sub<</span<, and a decrease of up to 2–3 hPa was observed for VPD. Given the long-distance transport of aerosols emitted by burning biomass, significant changes in atmospheric optical properties and irradiance will impact the CO<span class="inline-formula"<<sub<2</sub<</span< flux of semideciduous forests distributed in the region.</p< |
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Enhanced net CO<sub<2</sub< exchange of a semideciduous forest in the southern Amazon due to diffuse radiation from biomass burning |
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