An overview of the studies on black carbon and mineral dust deposition in snow and ice cores in East Asia

详细信息    查看全文

• 作者：Xin Wang ; Baiqing Xu ; Jing Ming
• 关键词：black carbon ; mineral dust ; ice core ; seasonal snow ; radiative forcing ; Tibetan Plateau
• 刊名：Journal of Meteorological Research
• 出版年：2014
• 出版时间：June 2014
• 年：2014
• 卷：28
• 期：3
• 页码：354-370
• 全文大小：846 KB
• 参考文献：Alfaro, S. C., S. Lafon, J. L. Rajot, et al., 2004: Iron oxides and light absorption by pure desert dust: An experimental study. J. Geophys. Res., 109(D8), doi: 10.1029/2003jd004374.
  Aoki, T., K. Kuchiki, M. Niwano, et al., 2011: Physically based snow albedo model for calculating broadband albedos and the solar heating profile in snowpack for general circulation models. J. Geophys. Res., 116(D11), doi: 10.1029/2010jd015507.
  Baumgardner, D., G. Kok, and G. Raga, 2004: Warming of the Arctic lower stratosphere by light absorbing particles. Geophys. Res. Lett., 31, doi: 10.1029/2003gl018883.
  Bi, J. R., J. P. Huang, Q. A. Fu, et al., 2011: Toward characterization of the aerosol optical properties over Loess Plateau of northwestern China. J. Quant. Spectrosc. Ra., 112, 346-60, doi: 10.1016/J.Jqsrt.2010.09.006.
  Bond, T. C., M. Bussemer, B. Wehner, et al., 1999: Light absorption by primary particle emissions from a lignite burning plant. Environ. Sci. Technol., 33, 3887-891, doi: 10.1021/Es9810538.
  - D. G. Streets, K. F. Yarber, et al., 2004: A technology-based global inventory of black and organic carbon emissions from combustion. J. Geophys. Res., 109(D14), doi: 10.1029/2003jd003697.
  - and R. W. Bergstrom, 2006: Light absorption by carbonaceous particles: An investigative review. Aerosol Sci. Technol., 40, 27-7, doi: 10.1080/02786820500421521.
  - E. Bhardwaj, R. Dong, et al., 2007: Historical emissions of black and organic carbon aerosol from energy-related combustion, 1850-000. Global Biogeochem. CY., 21, doi: 10.1029/2006gb002840.
  - S. J. Doherty, D. W. Fahey, et al., 2013: Bounding the role of black carbon in the climate system: A scientific assessment. J. Geophys. Res., 118, 5380-552, doi: 10.1002/jgrd.50171.
  Cachier, H., M. P. Bremond, and P. Buat-Ménard, 1989: Determination of atmospheric soot carbon with a simple thermal method. Tellus B, 41, 379-90.
  - and M. H. Pertuisot, 1994: Particulate carbon in Arctic ice. Analusis, 22, M34–M37.
  Cao, J. J., S. C. Lee, J. C. Chow, et al., 2007: Spatial and seasonal distributions of carbonaceous aerosols over China. J. Geophys. Res., 112(D22), doi: 10.1029/2006jd008205.
  Charlson, R. J., S. E. Schwartz, J. M. Hales, et al., 1992: Climate forcing by anthropogenic aerosols. Science, 255, 423-30, doi: 10.1126/science.255.5043.423.
  Che, H. Z., X. Y. Zhang, S. Alfraro, et al., 2009: Aerosol optical properties and its radiative forcing over Yulin, China in 2001 and 2002. Adv. Atmos. Sci., 26, 564-76, doi: 10.1007/S00376-009-0564-4.
  - Y. Q. Wang, J. Y. Sun, et al., 2013: Variation of aerosol optical properties over the Taklimakan desert in China. Aerosol Air Qual. Res., 13, 777-85, doi: 10.4209/Aaqr.2012.07.0200.
  Chen, S. Y., J. P. Huang, C. Zhao, et al., 2013: Modeling the transport and radiative forcing of Taklimakan dust over the Tibetan Plateau: A case study in the summer of 2006. J. Geophys. Res., 118, 797-12, doi: 10.1002/Jgrd.50122.
  Chen, Y., and T. C. Bond, 2010: Light absorption by organic carbon from wood combustion. Atmos. Chem. Phys., 10, 1773-787.
  Chylek, P., V. Ramaswamy, and V. Srivastava, 1983: Albedo of soot-contaminated snow. J. Geophys. Res., 88, 10837-0843, doi: 10.1029/Jc088ic15p10837.
  - V. Srivastava, L. Cahenzli, et al., 1987: Aerosol and graphitic carbon content of snow. J. Geophys. Res., 92(D8), 9801-809, doi: 10.1029/Jd092id08p09801.
  Claquin, T., C. Roelandt, K. Kohfeld, et al., 2003: Radiative forcing of climate by ice-age atmospheric dust. Climate Dyn., 20, 193-02.
  Clarke, A. D., 1982: Integrating sandwich: A new method of measurement of the light-absorption coefficient for atmospheric particles. Appl. Opt., 21, 3011-020.
  - and K. J. Noone, 1985: Soot in the Arctic snowpack: A cause for perturbations in radiative transfer. Atmos. Environ., 19, 2045-053, doi: 10.1016/0004-6981(85)90113-1.
  - K. J. Noone, J. Heintzenberg, et al., 1987: Aerosol light absorption measurement techniques: Analysis and intercomparisons. Atmos. Environ., 21, 1455-465.
  - Y. Shinozuka, V. N. Kapustin, et al., 2004: Size distributions and mixtures of dust and black carbon aerosol in Asian outflow: Physiochemistry and optical properties. J. Geophys. Res., 109(D15), doi: 10.1029/2003jd004378.
  Conway, H., A. Gades, and C. F. Raymond, 1996: Albedo of dirty snow during conditions of melt. Water Resour. Res., 32, 1713-718, doi: 10.1029/96wr00712.
  Covert, D. S., and J. Heintzenberg, 1993: Size distributions and chemical properties of aerosol at Ny lesund, Svalbard. Atmos. Environ., 27, 2989-997, doi: 10.1016/0960-1686(93)90331-R.
  Derimian, Y., A. Karnieli, Y. J. Kaufman, et al., 2008: The role of iron and black carbon in aerosol light absorption. Atmos. Chem. Phys., 8, 3623-637.
  Ding, Y. J., S. Y. Liu, J. Li, et al., 2006: The retreat of glaciers in response to recent climate warming in western China. Ann. Glaciol., 43, 97-05, doi: 10.3189/172756406781812005.
  Doherty, S. J
• 作者单位：Xin Wang (1)
  Baiqing Xu (2)
  Jing Ming (3)
  
  1. Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou, 730000, China
  2. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China
  3. National Climate Center, China Meteorological Administration, Beijing, 100081, China
  
• 刊物类别：Atmospheric Sciences; Meteorology; Geophysics and Environmental Physics; Atmospheric Protection/Air
• 刊物主题：Atmospheric Sciences; Meteorology; Geophysics and Environmental Physics; Atmospheric Protection/Air Quality Control/Air Pollution;
• 出版者：The Chinese Meteorological Society
• ISSN：2198-0934

文摘

Black carbon (BC) is the most effective insoluble light-absorbing particulate (ILAP), which can strongly absorb solar radiation at visible wavelengths. Once BC is deposited in snow via dry or wet process, even a small amount of BC could significantly decrease snow albedo, enhance absorption of solar radiation, accelerate snow melting, and cause climate feedback. BC is considered the second most important component next to CO₂ in terms of global warming. Similarly, mineral dust (MD) is another type of ILAP. So far, little attention has been paid to quantitative measurements of BC and MD deposition on snow surface in the midlatitudes of East Asia, especially over northern China. In this paper, we focus on reviewing several experiments performed for collecting and measuring scavenging BC and MD in the high Asian glaciers over the mount-range (such as the Himalayas) and in seasonal snow over northern China. Results from the surveyed literature indicate that the absorption of ILAP in seasonal snow is dominated by MD in the Qilian Mount’s and by local soil dust in the Inner Mongolian region close to dust sources. The detection of BC in snow and ice cores using modern techniques has a large bias and uncert’ty when the snow sample is mixed with MD. Evidence also indicates that the reduction of snow albedo by BC and MD perturbations can significantly increase the net surface solar radiation, cause surface air temperature to rise, reduce snow accumulation, and accelerate snow melting. Key words black carbon mineral dust ice core seasonal snow radiative forcing Tibetan Plateau