Composition and mixing states of brown haze particle over the Himalayas along two transboundary south-north transects

被引:24
作者
Dong, Zhiwen [1 ]
Kang, Shichang [1 ,2 ]
Guo, Junming [1 ]
Zhang, Qianggong [2 ,3 ]
Wang, Xuejia [1 ]
Qin, Dahe [1 ]
机构
[1] Chinese Acad Sci, State Key Lab Cryosphere Sci, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Peoples R China
[2] CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
[3] Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
基金
中国国家自然科学基金;
关键词
Brown haze; TEM-EDX; Mixing states; Himalayas; Tibetan Plateau; TIBETAN PLATEAU; BLACK CARBON; NORTHWESTERN HIMALAYA; BACKGROUND AEROSOL; OPTICAL-PROPERTIES; INDIAN HIMALAYA; ALPINE GLACIERS; ICE CORE; DUST; CLIMATE;
D O I
10.1016/j.atmosenv.2017.02.029
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Pollutants that are usually transported from southern Asia to the Tibetan Plateau deposit on the Plateau surface, change snow albedo and thereby surface radiative flux. This results numerous climatic implications like as erratic monsoon, perturbation in hydrological cycle, etc. However, the accurate estimation of these climatic implications is not well understood, because the atmospheric pollution is a heterogeneous mixture of various particle types. Therefore, this part of climate research requires a detailed investigation of physical and chemical properties of atmospheric pollutants. This study aimed to examine the physical and chemical properties of atmospheric pollutants across the Himalayan regions along two transboundary south-north transects. The information of individual-particles was obtained using microscopy-based techniques that comprises transmission electron microscope (TEM) and Energy-dispersive X-ray spectrometer (EDX). Study capture the signatures of various types of atmospheric species such as black carbon (BC), mineral dust, fly ash, organic matter, sulfate, nitrite, ammonium, and NaCI. Microscopy-based techniques confirm that these particles were generally in mixing state, for example salt-coated particles accounting for 25-56% of the total particles in sampled locations. Our analysis shows that urban and rural locations are characterized with atmospheric particles which sourced from anthropogenic activities, whereas remote locations with those released from natural crustal. However, the relative contributions of anthropogenic particles were higher than that of particles released from natural crustal. The presence of such particles over remote locations of Himalayan region provides an evidence of prevailing atmospheric transport processes, which further need to be well understood. It is expected that this work would be helpful in understanding the regional atmospheric conditions and the transboundary transport process of haze particles. As these informations are of great importance in modeling studies, which further lead to improve understanding of haze particles climate effects. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:24 / 35
页数:12
相关论文
共 68 条
[1]   Internally mixed soot, sulfates, and organic matter in aerosol particles from Mexico City [J].
Adachi, K. ;
Buseck, P. R. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2008, 8 (21) :6469-6481
[2]   Shapes of soot aerosol particles and implications for their effects on climate [J].
Adachi, Kouji ;
Chung, Serena H. ;
Buseck, Peter R. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2010, 115
[3]   High microbial activity on glaciers: importance to the global carbon cycle [J].
Anesio, Alexandre M. ;
Hodson, Andrew J. ;
Fritz, Andreas ;
Psenner, Roland ;
Sattler, Birgit .
GLOBAL CHANGE BIOLOGY, 2009, 15 (04) :955-960
[4]  
[Anonymous], ADV WATER RESOUR
[5]  
[Anonymous], CLIMATE CHANGE ENV
[6]   Atmospheric Brown Clouds in the Himalayas: first two years of continuous observations at the Nepal Climate Observatory-Pyramid (5079 m) [J].
Bonasoni, P. ;
Laj, P. ;
Marinoni, A. ;
Sprenger, M. ;
Angelini, F. ;
Arduini, J. ;
Bonafe, U. ;
Calzolari, F. ;
Colombo, T. ;
Decesari, S. ;
Di Biagio, C. ;
di Sarra, A. G. ;
Evangelisti, F. ;
Duchi, R. ;
Facchini, M. C. ;
Fuzzi, S. ;
Gobbi, G. P. ;
Maione, M. ;
Panday, A. ;
Roccato, F. ;
Sellegri, K. ;
Venzac, H. ;
Verza, G. P. ;
Villani, P. ;
Vuillermoz, E. ;
Cristofanelli, P. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2010, 10 (15) :7515-7531
[7]   Emissions from the laboratory combustion of wildland fuels:: Particle morphology and size [J].
Chakrabarty, RK ;
Moosmüller, H ;
Garro, MA ;
Arnott, WP ;
Walker, J ;
Susott, RA ;
Babbitt, RE ;
Wold, CE ;
Lincoln, EN ;
Hao, WM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D7)
[8]   Yak dung combustion aerosols in the Tibetan Plateau: Chemical characteristics and influence on the local atmospheric environment [J].
Chen, Pengfei ;
Kang, Shichang ;
Bai, Jiankun ;
Sillanpaa, Mika ;
Li, Chaoliu .
ATMOSPHERIC RESEARCH, 2015, 156 :58-66
[9]   Carbonaceous aerosols on the south edge of the Tibetan Plateau: concentrations, seasonality and sources [J].
Cong, Z. ;
Kang, S. ;
Kawamura, K. ;
Liu, B. ;
Wan, X. ;
Wang, Z. ;
Gao, S. ;
Fu, P. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2015, 15 (03) :1573-1584
[10]   Dust and Biological Aerosols from the Sahara and Asia Influence Precipitation in the Western U.S. [J].
Creamean, Jessie M. ;
Suski, Kaitlyn J. ;
Rosenfeld, Daniel ;
Cazorla, Alberto ;
DeMott, Paul J. ;
Sullivan, Ryan C. ;
White, Allen B. ;
Ralph, F. Martin ;
Minnis, Patrick ;
Comstock, Jennifer M. ;
Tomlinson, Jason M. ;
Prather, Kimberly A. .
SCIENCE, 2013, 339 (6127) :1572-1578