Estimation of radiative forcing and heating rate based on vertical observation of black carbon in Nanjing, China

被引:23
|
作者
Shi, Shuangshuang [1 ]
Zhu, Bin [1 ]
Lu, Wen [1 ]
Yan, Shuqi [1 ]
Fang, Chenwei [1 ]
Liu, Xiaohui [1 ]
Liu, Duanyang [2 ]
Liu, Chao [1 ]
机构
[1] Nanjing Univ Informat Sci & Technol, China Meteorol Adm,Minist Educ KLME,Key Lab Meteo, Key Lab Aerosol Cloud Precipitat,Joint Int Res La, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing 210044, Peoples R China
[2] China Meteorol Adm, Jiangsu Inst Meteorol Sci, Nanjing Joint Inst Atmospher Sci, Key Lab Transportat Meteorol, Nanjing 210008, Peoples R China
基金
中国国家自然科学基金;
关键词
Black carbon aerosols; Vertical profiles; Radiative forcing; Heating rate; ABSORPTION-COEFFICIENT; MICRO-AETHALOMETER; SIZE DISTRIBUTION; LOWER TROPOSPHERE; MIXING-LAYER; AEROSOLS; PROFILES; SUMMER; PARTICLES; POLLUTION;
D O I
10.1016/j.scitotenv.2020.144135
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Owing to a lack of vertical observations, the impacts of black carbon (BC) on radiative forcing (RF) have typically been analyzed using ground observations and assumed profiles. In this study, a UAV platform was used to measure high-resolution in-situ vertical profiles of BC, fine partides (PM2.5), and relevant meteorological parameters in the boundary layer (BL). Further, a series of calculations using actual vertical profiles of BC were conducted to determine its impact on RF and heating rate (HR). The results show that the vertical distributions of BC were strongly affected by atmospheric thermodynamics and transport. Moreover. Three main types of profiles were revealed: Type I, Type II, Type III, which correspond to homogenous profiles (HO), negative gradient profiles (NG), and positive gradient profiles (PG), respectively. Types I and II were related to the diurnal evolution of the BL, and Type III was caused by surrounding emissions from high stacks and regional transport. There were no obvious differences in RF calculated for HO profiles and corresponding surface BC concentrations, unlike for NG and PG profiles. RF values calculated using surface BC concentrations led to an overestimate of 13.2 W m(-2) (27.5%, surface) and 18.2 W m(-2) (33.4%, atmosphere) compared to those calculated using actual NG profiles, and an underestimate of approximately 15.4 W m(-2) (35.0%, surface) and 16.1 W m(-2) (29.9%, atmosphere) compared to those calculated using actual PG profiles. In addition, the vertical distributions of BC HR exhibited dear sensitivity to BC profile types. Daytime PG profiles resulted in a positive vertical gradient of HR, which may strengthen temperature inversion at high altitudes. These findings indicate that calculations that use BC surface concentrations and ignore the vertical distribution of BC will lead to substantial uncertainties in the effects of BC on RE and HR. (C) 2020 Elsevier B.V. All rights reserved.
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页数:11
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