Temporal variability and radiative impact of black carbon aerosol over tropical urban station Hyderabad

被引:68
|
作者
Dumka, U. C. [1 ,2 ]
Manchanda, R. K. [1 ]
Sinha, P. R. [1 ]
Sreenivasan, S. [1 ]
Moorthy, K. Krishna [3 ]
Babu, S. Suresh [3 ]
机构
[1] Tata Inst Fundamental Res, Balloon Facil, Hyderabad 500062, Andhra Pradesh, India
[2] Aryabhatta Res Inst Observat Sci ARIES, Naini Tal 263129, India
[3] Vikram Sarabhai Space Ctr, Space Phys Lab, Trivandrum 695022, Kerala, India
关键词
Black carbon; Air mass back-trajectory; CWT; Radiative forcing; Hyderabad; VISIBLE-LIGHT ABSORPTION; SOURCE APPORTIONMENT; SPECTRAL DEPENDENCE; PARTICULATE MATTER; SEASONAL-VARIATION; OPTICAL-PROPERTIES; COASTAL STATION; SOUTH-ASIA; CLIMATE; INDIA;
D O I
10.1016/j.jastp.2013.08.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Time variability of black carbon (BC) aerosols over different timescales (daily, weekly and annual) is studied over a tropical urban location Hyderabad in India using seven channel portable Aethalometer. The results for the 2-year period (January 2009-December 2010) show a daily-mean BC variability from similar to 1.00 +/- 0.12 mu g m(-3) to 12.50 +/- 3.06 mu g m(-3), with a remarkable annual pattern of winter high and monsoon low. The BC values maximize during winter (December-January), similar to 6.67 +/- 0.22 mu g m(-3), and drop during summer (June-August), similar to 2.36 +/- 0.09 mu g m(-3), which establishes a large seasonal variation. Furthermore, the BC mass concentration exhibits a well-defined diurnal variation, with a morning peak and early afternoon minimum. The magnitude of the diurnal variations is seasonal dependent, which maximizes during the winter months. Air mass back trajectories indicated several different transport pathways, while the concentration weighted trajectory (CWT) analysis reveals that the most important potential sources for BC aerosols are the Indo-Gangetic plain (IGP), central India and some hot spots in Pakistan, Arabian Peninsula and Persian Gulf. The absorbing Angstrom exponent (alpha(abs)) estimated from the spectral values of absorption coefficient (sigma(abs)) ranges from 0.9 to 1.1 indicating high BC/OC ratio typical of fossil fuel origin. The annual average BC mass fraction to composite aerosols is found to be (10 +/- 3) % contributing to the atmospheric forcing by (55 +/- 10) %. The BC radiative forcing at the atmosphere shows strong seasonal dependency with higher values in winter (33.49 +/- 7.01) and spring (31.78 +/- 12.89) and moderate in autumn (18.94 +/- 6.71) and summer (13.15 +/- 1.66). The BC radiative forcing at the top of the atmosphere (TOA) is positive in all months, suggesting an overall heating of the regional climate over Hyderabad. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:81 / 90
页数:10
相关论文
共 50 条
  • [31] High light absorption and radiative forcing contributions of primary brown carbon and black carbon to urban aerosol
    Zhu, Chong-Shu
    Qu, Yao
    Zhou, Yue
    Huang, Hong
    Liu, Hui-Kun
    Yang, Lu
    Wang, Qi-Yuan
    Hansen, Anthony D. A.
    Cao, Jun-Ji
    GONDWANA RESEARCH, 2021, 90 : 159 - 164
  • [32] Impact of direct radiative forcing of black carbon aerosols on tropical convective precipitation
    Wang, Chien
    GEOPHYSICAL RESEARCH LETTERS, 2007, 34 (05)
  • [33] Aerosol radiative effects over an urban location and a remote site in western India: Seasonal variability
    Ramachandran, S.
    Kedia, Sumita
    ATMOSPHERIC ENVIRONMENT, 2011, 45 (39) : 7415 - 7422
  • [34] Black carbon aerosols over tropical urban environment - a case study
    Latha, KM
    Badarinath, KV
    ATMOSPHERIC RESEARCH, 2003, 69 (1-2) : 125 - 133
  • [35] Vertical profiles of aerosol black carbon in the atmospheric boundary layer over a tropical coastal station: Perturbations during an annular solar eclipse
    Babu, S. Suresh
    Sreekanth, V.
    Moorthy, K. Krishna
    Mohan, Mannil
    Kirankumar, N. V. P.
    Subrahamanyam, D. Bala
    Gogoi, Mukunda M.
    Kompalli, Sobhan Kumar
    Beegum, Naseema
    Chaubey, Jai Prakash
    Kumar, V. H. Arun
    Manchandab, Ravi K.
    ATMOSPHERIC RESEARCH, 2011, 99 (3-4) : 471 - 478
  • [36] Black carbon in contrasting environments in India: Temporal variability, source apportionment and radiative forcing
    Romshoo, Baseerat
    Bhat, Mudasir Ahmad
    Habib, Gazalla
    ATMOSPHERIC ENVIRONMENT, 2023, 302
  • [37] Direct radiative forcing from black carbon aerosols over urban environment
    Badarinath, K. V. S.
    Latha, K. Madhavi
    ATMOSPHERIC REMOTE SENSING: EARTH'S SURFACE, TROPOSPHERE, STRATOSPHERE AND MESOSPHERE - II, 2006, 37 (12): : 2183 - 2188
  • [38] Aerosol mixing over an urban region: radiative effects
    Srivastava, Rohit
    Ramachandran, S.
    Rajesh, T. A.
    QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2016, 142 (697) : 1732 - 1744
  • [39] Influence of accidental fire on black carbon aerosol concentrations over an urban environment
    Latha, KM
    Badarinath, KVS
    INTERNATIONAL JOURNAL OF ENVIRONMENT AND POLLUTION, 2005, 23 (04) : 473 - 479
  • [40] Temporal variability in aerosol characteristics and its radiative properties over Patiala, northwestern part of India: Impact of agricultural biomass burning emissions
    Sharma, D.
    Srivastava, A. K.
    Ram, K.
    Singh, A.
    Singh, D.
    ENVIRONMENTAL POLLUTION, 2017, 231 : 1030 - 1041