4.7 Article

Black carbon over a high altitude Central Himalayan Glacier: Variability, transport, and radiative impacts

Journal

ENVIRONMENTAL RESEARCH
Volume 204, Issue -, Pages -

Publisher

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.envres.2021.112017

Keywords

Central Himalayan glacier; BC transport; Sources; Radiative forcing

Funding

  1. MoES, Govt.

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The study found that black carbon concentrations in the glacier region of Central Himalaya decrease during monsoon months, related to limited long-range transport and rapid wet scavenging processes. The high BC concentrations in June, September, and October are mainly attributed to air transport from the polluted Indo-Gangetic Plain region, wildfires, and vehicular emissions in the valley region.
Ambient equivalent black carbon (BC) measurements spanning from June to October have been carried out over an adjoining location of Satopanth and Bhagirath-Kharak Glaciers (3858m, amsl) of Central Himalaya during the year 2019. Hourly BC varied from 12 ng m- 3 to 439 ng m- 3 during the entire period of observation. Monthly averaged BC values showed the highest concentration during June (230.96 +/- 85.46 ng m- 3) and the lowest in August (118.02 +/- 71.63 ng m- 3). The decrease in BC during monsoon months is attributed to limited long-range transport and rapid wet scavenging processes. Transport model studies indicate a higher retention time of tracer in Uttarakhand, Punjab, Haryana, and adjacent polluted valley regions with increased biomass burning (BB) incidences. The high rate of BC influx during June, September, and October was attributed to transport from the polluted Indo-Gangetic Plain (IGP) region, wildfires, and vehicular emissions in the valley region. Higher equivalent brown carbon (BrC) influx is linked to BB, especially wood-burning, during intense forest fires at slopes of mountains. Data obtained from limited BC observations during the 2011-19 period showed no significant BC influx change during post-monsoon. The strong correlation between BC mass and BB affirms the dominant role of BB in contributing BC to the Glacier region. Increased TOA forcing induced by surface darkening and BC atmospheric radiative heating indicate an additional warming and possible changes of the natural snow cycle over the glacier depending on the characteristics and extent of debris cover.

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