Enacting new policies can achieve benefits over the projected 23% reduction in Black Carbon as a result of ongoing efforts.
Black Carbon (BC) deposits produced by human activity which accelerate the pace of glacier and snow melt in the Himalayan region can be sharply reduced through new, currently feasible policies by an additional 50% from current levels, new research by World Bank (WB) specialists has said.
The research report from the WB covers the Himalaya, Karakoram, and Hindu Kush (HKHK) mountain ranges, where, it says, glaciers are melting faster than the global average ice mass. The rate of retreat of HKHK glaciers is estimated to be 0.3 metres per year in the west to 1.0 metre per year in the east. BC adds to the impact of climate change.
Full implementation of current policies to mitigate BC can achieve a 23% reduction by 2040 but enacting new policies and incorporating them through regional cooperation among countries can achieve enhanced benefits, the WB said in its research report titled “Glaciers of the Himalayas, Climate Change, Black Carbon and Regional Resilience” released on Thursday.
“BC is a short-lived pollutant that is the second-largest contributor to warming the planet behind carbon dioxide (CO.2). Unlike other greenhouse gas emissions, BC is quickly washed out and can be eliminated from the atmosphere if emissions stop,” the publication says. Unlike historical carbon emissions it is also a localised source with greater local impact.
Cutting black carbon
Some of the ongoing policy measures to cut BC emissions are enhancing fuel efficiency standards for vehicles, phasing out diesel vehicles and promoting electric vehicles, accelerating the use of liquefied petroleum gas for cooking and through clean cookstove programs, as well as upgrading brick kiln technologies, says the publication, edited by Muthukumara Mani, lead economist, South Asia Region, World Bank. However, with all existing measures, water from glacier melt is still projected to increase in absolute volume by 2040, with impacts on downstream activities and communities.
At a virtual panel discussion on the release of the report, Hartwig Schafer, vice-president, South Asia Region, World Bank Group, said regional integration and collaboration was one way to address the question of melting glaciers. The research done by the team brought new perspective to reduction of black carbon emissions in the region.
Deposits of BC act in two ways hastening the pace of glacier melt: by decreasing surface reflectance of sunlight and by raising air temperature, the researchers point out.
“Specifically, in the Himalayas, reducing black carbon emissions from cookstoves, diesel engines, and open burning would have the greatest impact and could significantly reduce radiative forcing and help to maintain a greater portion of Himalayan glacier systems. More detailed modelling at a higher spatial resolution is needed to expand on the work already completed,” it says, calling upon regional governments to review policies on water management, with an emphasis on basin-based regulation and use of price signals for efficiency, careful planning and use of hydropower to reflect changes in water flows and availability, and increasing the efficiency of brick kilns through proven technologies. There must also be greater knowledge sharing in the region.
The WB publication says “Industry (primarily brick kilns) and residential burning of solid fuel together account for 45–66% of regional anthropogenic [man-made] BC deposition, followed by on-road diesel fuels (7–18%) and open burning (less than 3% in all seasons)” in the region.
There are almost 55,000 glaciers in the HKHK mountains, and they store more freshwater “than any other region outside the North and South Poles.” The glaciers contain estimated ice reserves of 163 cubic kilometres, of which almost 80% feeds the Indus, Ganges, and Brahmaputra, the report says.
Glacier melt produces flash floods, landslides, soil erosion, and glacial lake outburst floods (GLOF), and in the short run, the higher volumes of melt water could replace receding groundwater downstream. But in the long run, decreased water availability would aggravate water shortage.
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