Kathmandu, Aug. 5
The Melamchi disaster of June15 and
the subsequent days was the result of multiple man-made and climatic factors,
concluded a recent report of the International Centre for Integrated Mountain
Development (ICIMOD).
It attributed factors including weather
condition, snowmelt and erosion of glacial deposits, glacial lake outburst,
landslide and river damming, new landslide, riverbank erosion and debris
deposition to the disaster which killed five and swept away 20 people and
damaged property worth billions of rupees.
Experts also cited possible
earthquake impact behind the devastating floods that deposited debris in
Melamchi Bazaar and buried houses, fields and other properties.
“The Melamchi disaster of June 15 and the following days cannot be
attributed to a single factor. It was the result of multiple anthropogenic and
climatic factors and processes that occurred at various locations along the
Melamchi River,” read the report.
According to it, the Melamchi-Indrawati watershed receives high
precipitation, which increases, along with altitude, towards the north. This
disaster was initiated by intense precipitation in the upstream areas, which triggered
cascading hazards along the river corridors, causing loss of life and extreme
devastation to settlements, markets, roads and bridges, and local livelihoods.
Both the Melamchi and Indrawati basins started
receiving rainfall from June 9 as recorded in the automatic weather station of
the Department of Hydrology and Meteorology (DHM) at Sermathang, located at an
elevation of 2625 metres above sea level. On June 11, Sermathang recorded more
than 100 mm of daily rainfall. During the six-day interval, the station had,
therefore, received more than 200 mm of rainfall.
According to the DHM report on pre-monsoon rainfall
monitoring, the daily accumulated rainfall from March to May was 129 per cent
above normal, which shows that the watershed had experienced significant
precedent precipitation.
The automatic weather station (AWS) operated by
ICIMOD at Ganja La in the upper Yangri Khola shows that just four days before
the occurrence of the most significant mass flow events, air temperature had
risen significantly suggesting a transition to heavy snow melt, according to
the report.
It said that both pre-monsoon precipitation
events and the two cyclones, Yaas and Taukte, resulted in significant amounts
of snow in the headwater areas of the Melamchi watershed. Rapid snow melt and
high precipitation resulted in the erosion of glacial deposits in the
headwaters of Pemdang Khola, Yangri Khola and Larke Khola.
It is estimated that glacial deposit
erosion occurred over an area of approximately 70,000 m² in the headwaters of
Pemdang Khola, stated the report.
The new landslide, 550 metre wide at the bottom, at the east of
Melamchigaon on the left bank of the Melamchi River deposited about 670,000
cubic metre of debris on the river blocking its flow.
“This blockage would have got filled up
with debris flowing from the upstream area. Eventually, the river would have
overflowed the landslide by eroding and cutting the damming material and
breached out, causing the catastrophic flood that resulted in major damage to
the downstream areas,” read the report.
Stating that cascading hazards are becoming more common in Nepal and in
the Hindu Kush Himalaya, the report suggested that it demanded a more holistic
approach in hazard assessment and risk management.
The report prepared by 11 scientists
and researchers also suggested establishing early
warning system in the watershed with strong involvement from upstream and
downstream communities, supported by local and national government entities.
The study was based mainly on remote sensing information, and a rapid field assessment in the downstream part of the watershed should be augmented by aerial observation and detailed field investigation, particularly in the upstream high-altitude area of the watershed.
Published in The Rising Nepal daily on 6 August 2021.
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