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对流、化学作用及森林砍伐对亚马孙地区生物源挥发性有机化合物的影响。

Impacts of convection, chemistry, and forest clearing on biogenic volatile organic compounds over the Amazon.

作者信息

Tripathi Nidhi, Krumm Bianca E, Edtbauer Achim, Ringsdorf Akima, Wang Nijing, Kohl Matthias, Vella Ryan, Machado Luiz A T, Pozzer Andrea, Lelieveld Jos, Williams Jonathan

机构信息

Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany.

Institute for Atmospheric Physics, Johannes Gutenberg University Mainz, Mainz, Germany.

出版信息

Nat Commun. 2025 May 20;16(1):4692. doi: 10.1038/s41467-025-59953-2.

DOI:10.1038/s41467-025-59953-2
PMID:40394002
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC12092753/
Abstract

The Amazon rainforest is the largest source of biogenic volatile organic compounds (BVOCs) to the atmosphere. To understand the distribution and chemistry of BVOCs, airborne and ground-based measurements of BVOCs are conducted over the Amazon rainforest in the CAFE-Brazil campaign (December 2022-January 2023), including diel (24-hour) profiles between 0.3-14 km for isoprene, its oxidation products, and total monoterpenes. Although daytime deep convective transport of BVOCs is rendered ineffective by photochemical loss, nocturnal deep-convection exports considerable BVOC quantities to high altitudes, extending the chemical influence of the rainforest to the upper troposphere, and priming it for rapid organic photochemistry and particle formation at dawn. After contrasting pristine and deforested areas, a BVOC sensitivity analysis is performed using a chemistry-climate model. Here we show that reducing BVOC emissions, decreased upper tropospheric ozone, increased lower tropospheric hydroxyl radicals, shortened the methane lifetime, with the net effect of enhancing climate warming through ozone and aerosols.

摘要

亚马逊雨林是大气中生物源挥发性有机化合物(BVOCs)的最大来源。为了解BVOCs的分布和化学性质,在“巴西咖啡”(CAFE-Brazil)活动(2022年12月至2023年1月)期间,对亚马逊雨林进行了BVOCs的机载和地面测量,包括异戊二烯、其氧化产物和总单萜在0.3 - 14千米之间的日变化(24小时)剖面。尽管白天BVOCs的深对流输送因光化学损失而失效,但夜间深对流将大量BVOCs输送到高海拔地区,将雨林的化学影响扩展到对流层上部,并使其在黎明时易于发生快速的有机光化学和颗粒物形成。在对比原始区域和森林砍伐区域后,使用化学气候模型进行了BVOCs敏感性分析。我们在此表明,减少BVOCs排放会降低对流层上部臭氧、增加对流层下部羟基自由基、缩短甲烷寿命,其净效应是通过臭氧和气溶胶增强气候变暖。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/6733088ab72f/41467_2025_59953_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/8a01a196d152/41467_2025_59953_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/249b59d7b002/41467_2025_59953_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/c0174ab46761/41467_2025_59953_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/df330d971ecb/41467_2025_59953_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/6733088ab72f/41467_2025_59953_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/8a01a196d152/41467_2025_59953_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/249b59d7b002/41467_2025_59953_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/c0174ab46761/41467_2025_59953_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/df330d971ecb/41467_2025_59953_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3092/12092753/6733088ab72f/41467_2025_59953_Fig5_HTML.jpg

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本文引用的文献

1
Isoprene nitrates drive new particle formation in Amazon's upper troposphere.异戊二烯硝酸盐促使亚马逊对流层上层形成新颗粒。
Nature. 2024 Dec;636(8041):124-130. doi: 10.1038/s41586-024-08192-4. Epub 2024 Dec 4.
2
Chemistry-albedo feedbacks offset up to a third of forestation's CO removal benefits.化学-反照率反馈抵消了高达三分之一的造林固碳效益。
Science. 2024 Feb 23;383(6685):860-864. doi: 10.1126/science.adg6196. Epub 2024 Feb 22.
3
Oxidized organic molecules in the tropical free troposphere over Amazonia.亚马孙地区热带对流层上层中的氧化有机分子。
Natl Sci Rev. 2023 May 15;11(1):nwad138. doi: 10.1093/nsr/nwad138. eCollection 2024 Jan.
4
Inferring the diurnal variability of OH radical concentrations over the Amazon from BVOC measurements.通过生物源挥发性有机化合物(BVOC)测量推断亚马逊地区OH自由基浓度的日变化。
Sci Rep. 2023 Sep 9;13(1):14900. doi: 10.1038/s41598-023-41748-4.
5
Effects of drought and recovery on soil volatile organic compound fluxes in an experimental rainforest.干旱及恢复对实验雨林中土壤挥发性有机化合物通量的影响
Nat Commun. 2023 Aug 21;14(1):5064. doi: 10.1038/s41467-023-40661-8.
6
Chemistry-driven changes strongly influence climate forcing from vegetation emissions.化学驱动的变化强烈影响植被排放对气候的强迫作用。
Nat Commun. 2022 Nov 23;13(1):7202. doi: 10.1038/s41467-022-34944-9.
7
Major Regional-Scale Production of O and Secondary Organic Aerosol in Remote Amazon Regions from the Dynamics and Photochemistry of Urban and Forest Emissions.从城市和森林排放的动力学和光化学角度看,主要的区域尺度的 O 和次生有机气溶胶在偏远亚马逊地区的产生。
Environ Sci Technol. 2022 Jul 19;56(14):9924-9935. doi: 10.1021/acs.est.2c01358. Epub 2022 Jul 8.
8
Nocturnal survival of isoprene linked to formation of upper tropospheric organic aerosol.异戊二烯的夜间存活与对流层上层有机气溶胶的形成有关。
Science. 2022 Feb 4;375(6580):562-566. doi: 10.1126/science.abg4506. Epub 2022 Feb 3.
9
Understanding the properties of methyl vinyl ketone and methacrolein at the air-water interface: Adsorption, heterogeneous reaction and environmental impact analysis.理解甲基乙烯基酮和甲基丙烯醛在气-水界面上的性质:吸附、非均相反应和环境影响分析。
Chemosphere. 2021 Nov;283:131183. doi: 10.1016/j.chemosphere.2021.131183. Epub 2021 Jun 14.
10
Deforestation reduces rainfall and agricultural revenues in the Brazilian Amazon.森林砍伐减少了巴西亚马逊地区的降雨量和农业收入。
Nat Commun. 2021 May 10;12(1):2591. doi: 10.1038/s41467-021-22840-7.