Estimated range of black carbon dry deposition and the related snow albedo reduction over Himalayan glaciers during dry pre-monsoon periods

Teppei J. Yasunari, Qian Tan, K. M. Lau, Paolo Bonasoni, Angela Marinoni, Paolo Laj, Martin Ménégoz, Toshihiko Takemura, Mian Chin

    Research output: Contribution to journalArticle

    31 Citations (Scopus)

    Abstract

    One of the major factors attributed to the accelerated melting of Himalayan glaciers is the snow darkening effect of atmospheric black carbon (BC). The BC is the result of incomplete fossil fuel combustion from sources such as open biomass burning and wood burning cooking stoves. One of the key challenges in determining the darkening effect is the estimation uncertainty of BC deposition (BCD) rate on surface snow cover. Here we analyze the variation of BC dry deposition in seven different estimates based on different dry deposition methods which include different atmospheric forcings (observations and global model outputs) and different spatial resolutions. The seven simulations are used to estimate the uncertainty range of BC dry deposition over the southern Himalayas during pre-monsoon period (March-May) in 2006. Our results show BC dry deposition rates in a wide range of 270-4700μgm-2 during the period. Two global models generate higher BC dry deposition rates due to modeled stronger surface wind and simplification of complicated sub-grid surface conditions in this region. Using ice surface roughness and observation-based meteorological data, we estimate a better range of BC dry deposition rate of 900-1300μgm-2. Under dry and highly polluted conditions, aged snow and sulfate-coated BC are expected to possibly reduce visible albedo by 4.2-5.1%. Our results suggest that for estimating aerosol-induced snow darkening effects of Himalaya snowpacks using global and regional models, realistic physical representation of ice or snow surface roughness and surface wind speed are critical in reducing uncertainties on the estimate of BC deposition over snow surface.

    Original languageEnglish
    Pages (from-to)259-267
    Number of pages9
    JournalAtmospheric Environment
    Volume78
    DOIs
    Publication statusPublished - Oct 1 2013

    Fingerprint

    dry deposition
    black carbon
    albedo
    glacier
    monsoon
    snow
    surface roughness
    surface wind
    ice
    atmospheric forcing
    snowpack
    biomass burning
    snow cover
    fossil fuel
    spatial resolution
    melting
    combustion
    wind velocity
    aerosol
    sulfate

    All Science Journal Classification (ASJC) codes

    • Environmental Science(all)
    • Atmospheric Science

    Cite this

    Estimated range of black carbon dry deposition and the related snow albedo reduction over Himalayan glaciers during dry pre-monsoon periods. / Yasunari, Teppei J.; Tan, Qian; Lau, K. M.; Bonasoni, Paolo; Marinoni, Angela; Laj, Paolo; Ménégoz, Martin; Takemura, Toshihiko; Chin, Mian.

    In: Atmospheric Environment, Vol. 78, 01.10.2013, p. 259-267.

    Research output: Contribution to journalArticle

    Yasunari, Teppei J. ; Tan, Qian ; Lau, K. M. ; Bonasoni, Paolo ; Marinoni, Angela ; Laj, Paolo ; Ménégoz, Martin ; Takemura, Toshihiko ; Chin, Mian. / Estimated range of black carbon dry deposition and the related snow albedo reduction over Himalayan glaciers during dry pre-monsoon periods. In: Atmospheric Environment. 2013 ; Vol. 78. pp. 259-267.
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    AU - Lau, K. M.

    AU - Bonasoni, Paolo

    AU - Marinoni, Angela

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