River Winds and Transport of Forest Volatiles in the Amazonian Riparian Ecoregion

被引:8
|
作者
Ye, Jianhuai [1 ,2 ]
Batista, Carla E. [3 ,4 ]
Zhao, Tianning [1 ]
Campos, Jesus [5 ]
Ma, Yongjing [6 ]
Guimaraes, Patricia [3 ,4 ]
Ribeiro, Igor O. [3 ]
Medeiros, Adan S. S. [3 ]
Stewart, Matthew P. [1 ]
de Arellano, Jordi Vila-Guerau [7 ]
Guenther, Alex B. [5 ]
de Souza, Rodrigo Augusto Ferreira [3 ,4 ]
Martin, Scot T. [1 ,8 ]
机构
[1] Harvard Univ, Sch Engn & Appl Sci, Cambridge, MA 02138 USA
[2] Southern Univ Sci & Technol, Sch Environm Sci & Engn, Shenzhen 518055, Guangdong, Peoples R China
[3] Amazonas State Univ, Sch Technol, BR-69065020 Manaus, Amazonas, Brazil
[4] Natl Inst Amazonian Res, Postgrad Program Climate & Environm, BR-69060001 Manaus, Amazonas, Brazil
[5] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
[6] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
[7] Wageningen Univ, Meteorol & Air Qual Sect, NL-6708 PB Wageningen, Netherlands
[8] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
基金
美国国家科学基金会; 加拿大自然科学与工程研究理事会;
关键词
volatile organic compounds; river wind; riparian ecoregion; Amazon tropical forest; unmanned aerial vehicle; LOCAL BOUNDARY-LAYER; RAIN-FOREST; ORGANIC-COMPOUNDS; EMISSIONS; BREEZE; ISOPRENE; AEROSOLS; DROUGHT; SEASON; BASIN;
D O I
10.1021/acs.est.1c08460
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Volatile organic compounds (VOCs) emitted from forests are important chemical components that affect ecosystem functioning, atmospheric chemistry, and regional climate. Temperature differences between a forest and an adjacent river can induce winds that influence VOC fate and transport. Quantitative observations and scientific understanding, however, remain lacking. Herein, daytime VOC datasets were collected from the surface up to 500 m over the "Rio Negro" river in Amazonia. During time periods of river winds, isoprene, alpha-pinene, and beta-pinene concentrations increased by 50, 60, and 80% over the river, respectively. The concentrations at 500 m were up to 80% greater compared to those at 100 m because of the transport path of river winds. By comparison, the concentration of methacrolein, a VOC oxidation product, did not depend on river winds or height. The differing observations for primary emissions and oxidation products can be explained by the coupling of timescales among emission, reaction, and transport. This behavior was captured in large-eddy simulations with a coupled chemistry model. The observed and simulated roles of river winds in VOC fate and transport highlight the need for improved representation of these processes in regional models of air quality and chemistry-climate coupling.
引用
收藏
页码:12667 / 12677
页数:11
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