The relationship between Brown haze, atmospheric boundary layer structure, and air pollution in an urban area of complex coastal terrain

被引:13
作者
Marley, Hannah G. [1 ]
Dirks, Kim N. [2 ]
Neverman, Andrew J. [3 ]
McKendry, Ian [4 ]
Salmond, Jennifer A. [1 ]
机构
[1] Univ Auckland, Sch Environm, Fac Sci, 23 Symonds St, Auckland 1010, New Zealand
[2] Univ Auckland, Dept Civil & Environm Engn, Fac Engn, 1 Grafton Rd, Auckland 1010, New Zealand
[3] Massey Univ, Manaaki Whenua Landcare Res, Riddet Rd, Palmerston North 4417, New Zealand
[4] Univ British Columbia, Fac Arts, Dept Geog, 1984 West Mall, Vancouver, BC V6T 1Z2, Canada
关键词
Air pollution; Atmospheric boundary layer; Brown haze; Ceilometer; Morning transition; Residual layer; RESIDUAL-LAYER; IMPACT; EVOLUTION; TRANSPORT; AEROSOLS; AUCKLAND; EPISODES; OZONE; IDENTIFICATION; CIRCULATION;
D O I
10.1016/j.apr.2021.101057
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Brown haze, observed over some cities during the winter months, has been found to be associated with poor surface air quality and negative health outcomes. While the link between the atmospheric boundary layer (ABL) structure and surface air quality is well-established, the degree to which boundary layer structure influences local brown haze formation is unknown. Using continuous ceilometer data from seven winters, we investigate the influence of the ABL structure in relation to surface air pollution and brown haze formation over an urban area of complex coastal terrain in the Southern Hemisphere city of Auckland, New Zealand. When days with severe brown haze are compared with those when brown haze is expected but not observed (based on favorable meteorology and high surface air pollution levels), the presence of severe brown haze is found to coincide with a significantly shallower boundary layer during both the daytime convective phase (similar to 48% lower) and the earlymorning nocturnal phase (similar to 28% lower). Severe brown haze is also found to be associated with significantly reduced morning transition growth rates (70 m h(-1)) compared to days on which brown haze is expected but not observed (170 m h(-1)). Our results also suggest the entrainment of pollutants stored in the residual layer may contribute to the severity of the haze. This study illustrates the complex interactions between the ABL structure, air pollution, and the presence of brown haze, and demonstrates the utility of a ceilometer instrument in understanding and predicting the occurrence of brown haze events.
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页数:11
相关论文
共 56 条
[1]   The transport of atmospheric NOx and HNO3 over Cape Town [J].
Abiodun, B. J. ;
Ojumu, A. M. ;
Jenner, S. ;
Ojumu, T. V. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2014, 14 (02) :559-575
[2]   Observations of the morning transition of the convective boundary layer [J].
Angevine, WM ;
Baltink, HK ;
Bosveld, FC .
BOUNDARY-LAYER METEOROLOGY, 2001, 101 (02) :209-227
[3]  
[Anonymous], 2018, Burden of disease from ambient air pollution for 2016, DOI DOI 10.1029/2005JD006314
[4]  
[Anonymous], 2005, CHARACTERISATION CAP
[5]   Boundary Layer Evolution and its Influence on Ground-Level Ozone Concentrations [J].
Athanassiadis, Georgios A. ;
Rao, S. Trivikrama ;
Ku, Jia-Yeong ;
Clark, Richard D. .
ENVIRONMENTAL FLUID MECHANICS, 2002, 2 (04) :339-357
[6]  
Auckland Council, 2016, AIR QUAL REP CARD AU
[7]  
Bell A, 1981, ECOS CSIRO ENV RES, V30, P12
[8]  
Chappell PR., 2013, NIWA Science and Technology Series, V60
[9]   Assessment of the impact of the meteorological meso-scale circulation on air quality in arid subtropical region [J].
Charabi, Yassine ;
Al-Bulooshi, Ali ;
Al-Yahyai, Sultan .
ENVIRONMENTAL MONITORING AND ASSESSMENT, 2013, 185 (03) :2329-2342
[10]   Assessing the impact of atmospheric stability on locally and remotely sourced aerosols at Richmond, Australia, using Radon-222 [J].
Crawford, Jagoda ;
Chambers, Scott ;
Cohen, David ;
Williams, Alastair ;
Griffiths, Alan ;
Stelcer, Eduard .
ATMOSPHERIC ENVIRONMENT, 2016, 127 :107-117