A study on the variations of optical and physical properties of aerosols over a tropical semi-arid station during grassland fire

被引:13
作者
Kumar, K. Raghavendra [1 ]
Narasimhulu, K. [1 ]
Balakrishnaiah, G. B. [1 ]
Reddy, B. Suresh Kumar [1 ]
Gopal, K. Rama [1 ]
Reddy, R. R. [1 ]
Satheesh, S. K. [2 ]
Moorthy, K. Krishna [3 ]
Babu, S. Suresh [3 ]
机构
[1] Sri Krishnadevaraya Univ, Dept Phys, Aerosol & Atmospher Res Lab, Anantapur 515055, Andhra Pradesh, India
[2] Indian Inst Sci, Ctr Atmospher & Ocean Sci, Bangalore 560012, Karnataka, India
[3] Vikram Sarabhai Space Ctr, Space Phys Lab, Trivandrum 695022, Kerala, India
关键词
Aerosol optical depth; Black carbon mass concentration; Size distribution; Accumulation mode particles; BLACK CARBON MEASUREMENTS; BIOMASS BURNING AEROSOLS; REAL-TIME MEASUREMENT; SEASONAL-VARIATIONS; BOUNDARY-LAYER; TRACE GASES; IMPACT; SMOKE; RADIATION; EMISSIONS;
D O I
10.1016/j.atmosres.2009.08.012
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The present paper records the results of a case study on the impact of an extensive grassland fire on the physical and optical properties of aerosols at a semi-arid station in southern India for the first time from ground based measurements using a MICROTOPS-II sunphotometer, an aethalometer and a quartz crystal microbalance impactor (QCM). Observations revealed a substantial increase in aerosol optical depth (AOD) at all wavelengths during burning days compared to normal days. High AOD values observed at shorter wavelengths suggest the dominance of accumulation mode particle loading over the study area. Daily mean aerosol size spectra shows, most of the time, power-law distribution. To characterize AOD, the Angstrom parameters (i.e., alpha and beta) were used. Wavelength exponent (1.38) and turbidity coefficient (0.21) are high during burning days compared to normal days, thereby suggesting an increase in accumulation mode particle loading. Aerosol size distribution suggested dominance of accumulation mode particle loading during burning days compared to normal days. A significant positive correlation was observed between AOD at 500 mn and water vapour and negative correlation between AOD at 500 nm and wind speed for burning and non-burning days. Diurnal variations of black carbon (BC) aerosol mass concentrations increased by a factor of similar to 2 in the morning and afternoon hours during burning period compared to normal days. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:77 / 87
页数:11
相关论文
共 59 条
[1]   Field validation of a semi-continuous method for aerosol black carbon (aethalometer) and temporal patterns of summertime hourly black carbon measurements in southwestern PA [J].
Allen, GA ;
Lawrence, J ;
Koutrakis, P .
ATMOSPHERIC ENVIRONMENT, 1999, 33 (05) :817-823
[2]   Atmospheric aerosols: Biogeochemical sources and role in atmospheric chemistry [J].
Andreae, MO ;
Crutzen, PJ .
SCIENCE, 1997, 276 (5315) :1052-1058
[3]   Biogeochemical cycling of carbon, water, energy, trace gases, and aerosols in Amazonia: The LBA-EUSTACH experiments [J].
Andreae, MO ;
Artaxo, P ;
Brandao, C ;
Carswell, FE ;
Ciccioli, P ;
da Costa, AL ;
Culf, AD ;
Esteves, JL ;
Gash, JHC ;
Grace, J ;
Kabat, P ;
Lelieveld, J ;
Malhi, Y ;
Manzi, AO ;
Meixner, FX ;
Nobre, AD ;
Nobre, C ;
Ruivo, MDLP ;
Silva-Dias, MA ;
Stefani, P ;
Valentini, R ;
von Jouanne, J ;
Waterloo, MJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D20) :33-1
[4]   Emission of trace gases and aerosols from biomass burning [J].
Andreae, MO ;
Merlet, P .
GLOBAL BIOGEOCHEMICAL CYCLES, 2001, 15 (04) :955-966
[5]   BIOMASS-BURNING EMISSIONS AND ASSOCIATED HAZE LAYERS OVER AMAZONIA [J].
ANDREAE, MO ;
BROWELL, EV ;
GARSTANG, M ;
GREGORY, GL ;
HARRISS, RC ;
HILL, GF ;
JACOB, DJ ;
PEREIRA, MC ;
SACHSE, GW ;
SETZER, AW ;
DIAS, PLS ;
TALBOT, RW ;
TORRES, AL ;
WOFSY, SC .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1988, 93 (D2) :1509-1527
[6]  
[Anonymous], 2007, AEROSOL AIR QUAL RES, DOI DOI 10.4209/AAQR.2007.01.0004
[7]   A case study on biomass burning aerosols: effects on aerosol optical properties and surface radiation levels [J].
Arola, A. ;
Lindfors, A. ;
Natunen, A. ;
Lehtinen, K. E. J. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2007, 7 (16) :4257-4266
[8]   Physical and chemical properties of aerosols in the wet and dry seasons in Rondonia, Amazonia -: art. no. 8081 [J].
Artaxo, P ;
Martins, JV ;
Yamasoe, MA ;
Procópio, AS ;
Pauliquevis, TM ;
Andreae, MO ;
Guyon, P ;
Gatti, LV ;
Leal, AMC .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D20) :LBA49-1
[9]   Large-scale aerosol source apportionment in Amazonia [J].
Artaxo, P ;
Fernandes, ET ;
Martins, JV ;
Yamasoe, MA ;
Hobbs, PV ;
Maenhaut, W ;
Longo, KM ;
Castanho, A .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D24) :31837-31847
[10]   Aerosol radiative forcing due to enhanced black carbon at an urban site in India [J].
Babu, SS ;
Satheesh, SK ;
Moorthy, KK .
GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (18)