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Volume 21 Issue 2
Apr 2010
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Article Contents
Ningning Zhang, Yuanqing He, Wilfred H Theakstone, Hongxi Pang. Chemical Composition of Aerosol and Fresh Snow and Tourism Influences at Baishui Glacier No. 1 from Mt. Yulong, Southeastern Tibetan Plateau. Journal of Earth Science, 2010, 21(2): 199-209. doi: 10.1007/s12583-010-0018-z
Citation: Ningning Zhang, Yuanqing He, Wilfred H Theakstone, Hongxi Pang. Chemical Composition of Aerosol and Fresh Snow and Tourism Influences at Baishui Glacier No. 1 from Mt. Yulong, Southeastern Tibetan Plateau. Journal of Earth Science, 2010, 21(2): 199-209. doi: 10.1007/s12583-010-0018-z

Chemical Composition of Aerosol and Fresh Snow and Tourism Influences at Baishui Glacier No. 1 from Mt. Yulong, Southeastern Tibetan Plateau

doi: 10.1007/s12583-010-0018-z
Funds:

the National Natural Science Foundation of China 40801028

the National Natural Science Foundation of China 40971019

the National Basic Research Program of China 2007CB411501

the West Light Foundation of Chinese Academy of Sciences O828A11001

the Funds from the State Key Laboratory of Cryospheric Sciences and the Lijiang City Government 

More Information
  • Corresponding author: Zhang Ningning, 236923zh@163.com
  • Received Date: 30 Oct 2009
  • Accepted Date: 10 Jan 2010
  • Publish Date: 01 Apr 2010
  • Aerosol and snow samples were collected at ablation zone of Baishui (白水) Glacier No. 1, Mt. Yulong (玉龙), from May to June, 2006. The concentrations of Cl-, NO3-, SO42-, Na+, K+, Mg2+, and Ca2+ were determined by ion chromatograph both in aerosol and snow samples. The average total aerosol loading is 25.45 neq·scm-1, NO3- and Na+ are the dominant soluble ions in the aerosol, accounting for 39% and 21% of average total aerosol loading, respectively. Monsoon circulation reduces the concentration of most ions, indicating that wet scavenging is effective for aerosol particles. In snow samples, SO42- and Ca2+ are the dominant anion and cation, respectively. A lower Na+/Cl- ratio was found in fresh snow samples compared to the higher ratio that was found in aerosol samples. Analyzing the difference in SO42- and NO3- in air and fresh snow indicated that the aerosol was influenced by local circulation, but the components in fresh snow samples were from long-distance transport. Enrichment of NO3- in aerosol samples is attributed to motor exhaust emissions from tourism by calculating the SO42- /NO3- ratio in aerosol and fresh snow samples. The temporal variation and correlation coefficients between soluble species in aerosol samples suggest that Cl-, Na+ and K+ come from sea-salt aerosol, and SO42-, Mg2+ and Ca2+ are from continental crust sources.

     

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  • Al-Khashman, O. A., 2005. Study of Chemical Composition in Wet Atmospheric Precipitation in Eshidiya Area, Jordan. Atmospheric Environment, 39: 6175-6183 doi: 10.1016/j.atmosenv.2005.06.056
    Balerna, A., Bernieri, E., Pecci, M., et al., 2003. Chemical and Radio-chemical Composition of Fresh Snow Samples from Northern Slope of Himalayas (Cho Oyu Range, Tibet). Atmospheric Environment, 37(12): 1573-1581 doi: 10.1016/S1352-2310(03)00009-8
    He, Y. Q., Yao, T. D., Cheng, G. D., et al., 2001. Climatic Records in a Firn Core from an Alpine Temperate Glacier on Mt. Yulong, Southeastern Part of the Tibetan Plateau. Episodes, 24(1): 13-18
    He, Y. Q., Yao, T. D., Theakstone, W. H., et al., 2002. Recent Climate Significance of Chemical Signals in a Shallow Firn Core from an Alpine Glacier in the South-Asia Monsoon Region. Journal of Asian Earth Science, 20(3): 289-296 doi: 10.1016/S1367-9120(01)00038-4
    Hitchcock, R. D., Spiller, L. L., Wilson, E. W., 1980. Sulphuric Acid Aerosols and HCl Release in Coastal Atmospheres: Evidence of Rapid Formation of Sulphuric Acid Particulates. Atmospheric Environment, 14: 165-182 doi: 10.1016/0004-6981(80)90275-9
    Hou, S. G., Qin, D. H., Zhang, D. Q., et al., 2002. Comparison of Two Ice Core Chemical Records Recovered from the Qomolangma (Mount Everest) Region, Himalaya. Annals of Glaciology, 99(35): 266-272
    Kang, S. C., Mayewski, P. A., Qin, D. H., et al., 2002. Glaciochemical Records from a Mt. Everest Ice Core, Relationship to Atmospheric Circulation over Asia. Atmospheric Environment, 36(21): 3351-3361
    Kang, S. C., Mayewski, P. A., Qin, D. H., et al., 2004. Seasonal Differences in Snow Chemistry from the Vicinity of Mt. Everest, Central Himalayas. Atmospheric Environment, 38(18): 2819-2829 doi: 10.1016/j.atmosenv.2004.02.043
    Kang, S. C., Qin, D. H., Mayewski, P. A., et al., 2001. Climatic and Environmental Records from the Far East Rongbuk Ice Core, Mt. Qomolangma (Mt. Everest). Episodes, 24(3): 176-181 doi: 10.18814/epiiugs/2001/v24i3/004
    Kang, S. C., Wake, C. P., Qin, D. H., et al., 2000. Monsoon and Dust Signals Recorded in the Dasuopu Glacier, Tibetan Plateau. Journal of Glaciology, 40(153): 222-226
    Marenco, F., Bonasoni, P., Calzolari, F., et al., 2006. Characterization of Atmospheric Aerosols at Monte Cimone, Italy, during Summer 2004: Source Apportionment and Transport Mechanisms. Journal of Geophysical Research, 111: D24202. doi: 10.1029/2006JD007145
    Marinoni, A., Polesello, S., Smiraglia, C., et al., 2001. Chemical Composition of Freshsnow Samples from the Southern Slope of Mt. Everest Region (Khumbu-Himal Region, Nepal). Atmospheric Environment, 35: 3183-3190
    Mayewski, P. A., Lyons, W. B., Ahmad, N., 1983. Chemical Composition of a High Altitude Fresh Snowfall in the Ladakh Himalayas. Geophys. Res. Lett. , 10(1): 105-108 doi: 10.1029/GL010i001p00105
    Mayewski, P. A., Berry, L. W., Spencer, M. J., et al., 1986. Snow Chemistry from Xixabangma Peak, Tibet. Journal of Glaciology, 32(112): 542-543 doi: 10.1017/S0022143000012296
    Migliavacca, D., Teixeira, E. C., Wiegand, F., et al., 2005. Atmospheric Precipitation and Chemical Composition of an Urban Site, Guaiba Hydrographic Basin, Brazil. Atmospheric Environment, 39: 1829-1844 doi: 10.1016/j.atmosenv.2004.12.005
    Ming, J., Zhang, D. Q., Kang, S. C., et al., 2007. Aerosol and Fresh Snow Chemistry in the East Rongbuk Glacier on the Northern Slope of Mt. Qomolangma (Everest). J. Geophys. Res. , 112: D15307 doi: 10.1029/2007JD008618
    Ohta, S., Okita, T., 1990. A Chemical Characterization of Atmospheric Aerosol in Sapporo. Atmospheric Environment, 24A: 815-822
    Pang, H. X., He, Y. Q., Theakstone, W. H., et al., 2007. Soluble Ionic and Oxygen Isotopic Compositions of a Shallow Firn Profile, Baishui Glacier No. 1, Southeastern Tibetan Plateau. Annals of Glaciology, 46: 325-330
    Ramachandran, S., 2005. PM2.5 Mass Concentrations in Comparison with Aerosol Optical Depths over the Arabian Sea and Indian Ocean during Winter Monsoon. Atmospheric Environment, 39: 1879-1890 doi: 10.1016/j.atmosenv.2004.12.003
    Sheng, W. K., Yao, T. D., Li, Y., et al., 1999. Variation of Ca2+ Concentration within the Guliya Ice Core and Its Climatic Signifecance. Journal of Glaciology and Geocryology, 21(1): 19-21 (in Chinese with English Abstract)
    Shrestha, A. B., Wake, C. P., Dibb, E. J., 1997. Chemical Composition of Aerosol and Snow in the High Himalaya during the Summer Monsoon Season. Atmospheric Environment, 31: 2815-2826 doi: 10.1016/S1352-2310(97)00047-2
    Shrestha, A. B., Wake, C. P., Dibb, E. J., et al., 2000. Seasonal Variations in Aerosol Concentrations and Compositions in the Nepal Himalaya. Atmospheric Environment, 34: 3349-3363 doi: 10.1016/S1352-2310(99)00366-0
    Shrestha, A. B., Wake, C. P., Dibb, E. J., 2002. Aerosol and Precipitation Chemistry at a Remote Himalayan Site in Nepal. Aerosol Science and Technology, 36: 441-456 doi: 10.1080/027868202753571269
    Sun, J. Y., 2002. Study on Chemistry of Aerosol and Snow/Ice from Cryosphere-Cases Studies at the Antarctic, the Arctic and Western China: [Dissertation]. Cold and Arid Regions Enviromental and Engineering Research Institute, Chinese Academy of Sciences (CAS), Lanzhou. 50-75 (in Chinese with English Abstract)
    Thompson, L. G., Yao, Y. D., Mosley-Thompson, E. D., et al., 2000. A High-Resolution Millennial Record of the South Asian Monsoon from Himalayan Ice Cores. Science, 289(5486): 1916-1919 doi: 10.1126/science.289.5486.1916
    Thompson, L.G., Yao, T. D., Davis, M. E., et al., 1997. Tropical Climate Instability: The Last Glacial Cycle from a Qinghai-Tibetan Ice Core. Science, 276: 1821-1825 doi: 10.1126/science.276.5320.1821
    Valsecchi, S., Smiraglia, C., Tartari, G., et al., 1999. Chemical Composition of Monsoon Deposition in the Everest Region. Science of the Total Environment, 226: 187-199 doi: 10.1016/S0048-9697(98)00393-3
    Wake, P. C., Dibb, E. J., Mayewski, P. A., et al., 1994. The Chemical Composition of Aerosols over the Eastern Himalayas and Tibetan Plateau during Low Dust Periods. Atmospheric Environment, 28(4): 301-306
    Yao, T. D., Duan, K. Q., Xu, B. Q., et al., 2002. Temperature and Methane Changes over the Past 1 000 Years Recorded in Dasuopu Glacier (Central Himalaya) Ice Core. Annals of Glaciology, 35: 379-383 doi: 10.3189/172756402781816997
    Zhao, Z. P., Li, Z. Q., 2004. Determination of Soluble Ions in Atmospheric Aerosol by Ion Chromatography. Modern Scientific Instruments, 5: 46-49 (in Chinese with English Abstract)
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