The soil in parts of Himachal and Uttarakhand is almost sinking and causing devastation in the geologically sensitive regions
An interaction between a western disturbance and the
trough also led to extremely heavy rainfall in the region and caused widespread
damage in July. On August 18 and 19, the trough temporarily moved southward
before moving to the north of its normal position again. Whenever it shifts
north, rainfall is concentrated over the Himalayan states and northeast India
while the rest of the plains remain largely dry.
Continuous rainfall soaks the topsoil, leading to flash
floods, heavy erosion, and collapse of structures. The soil in parts of
Himachal and Uttarakhand is almost sinking and causing devastation in the
geologically sensitive regions. Continued rainfall can saturate already
withered topsoil and lead to small and large landslides and destruction
particularly when infrastructure is not scientifically planned.
Wadia Institute of Himalayan Geology (Dehradun) director
Kalachand Sain called for the need to understand why this is happening. “The
monsoon trough is very active over the Himalayas. There is often also a
confluence or interaction with westerly disturbances which accentuates
rainfall. Due to climate change, some high-altitude regions are recording
significant rises in temperatures and hence a rise in the water-vapour holding
capacity. There is a lot of moisture available.”
Sain said in the Himalayan slope regions, the top part of the soil is environmentally weathered in most parts. “Very warm temperatures followed by cold temperatures—a cycle of thawing and freezing—is further degrading the topsoil. ...there is a lot of anthropogenic activity which can further put these regions at risk such as hill cutting, slope instability, heavy load, etc. in areas where load bearing capacity is not assessed. "Sain called for sensitising people about the risks in this terrain in current climatic conditions. “For short-term economic gain, lives can be lost if norms are not followed.”
Sain said all kinds of anthropogenic activities cannot be
allowed in the Himalayan region. “This should be clear to people. Second, we
can develop a landslide vulnerability map to identify zones at the highest
risk...land use maps should be prepared for them. Land use can allow only those
structures which are safe.”
Sain underlined the Himalayas are a very young mountain
range and a lot of subsurface and surface activities were going on there.
“There is erosion going on due to heavy rainfall events and snowfall. There is
exhumation of rocks and plate tectonics. It is geo-dynamically extremely active
due to these ongoing processes.”
He said the Himalayas are geologically very active and
add to the risk. Sain cited the downstream impact on the national Capital when
continuous rainfall led to devastating floods, landslides, and mudslides in
Himachal Pradesh followed by Uttarakhand in July.
Pushpendra Johari, senior vice-president (sustainability)
at RMSI, a global disaster risk management firm, said there has been excessive
rainfall but this is not the first time that the Himalayan states are getting
it. He added the use of dynamite and other invasive construction activities
have also impacted the topsoil. “There is no subsidence in these states on a
large scale. So, every time there is heavy rain, multiple landslides are
triggered. This is the case in Shimla, too, where the number of constructions
is extremely high. Slope stabilization has been completely ignored by road
construction projects.”
Johari said slopes have not been stabilized. “It should be made mandatory for project proponents and construction companies to stabilize slopes and ensure green cover before leaving a finished project. Secondly, the foundations of buildings and homes have to be deeper. We are seeing the topsoil just washing away with the building structure in Himachal Pradesh.”
Climate scientist and former earth sciences ministry
secretary M Rajeevan called on policymakers to make use of good science and
prediction capability. He added the monsoon is confined to the foothills of the
Himalayas due to its weak phase. “In the hilly region, monsoon rains are very
heavy. This is bound to happen. We should be prepared for both extremely heavy
precipitation as well as a prolonged dry spell. Mitigation efforts should be
strengthened.”
The standard precipitation index, which reflects soil
moisture and rainfall conditions for a particular location, for Mandi, Shimla,
Sirmaur, and Solan in Himachal and Uttarakhand’s Haridwar, Dehradun, and
Chamoli are “very wet” in August as per India Meteorological Department. It can
also help identify districts facing intense rainfall.
Environmentalist Ravi Chopra, who headed the Supreme
Court-appointed committee on Char Dham roads’ projects, in July highlighted the
significant impact of roads, railways, and transmission lines on Himalayan
ecology during a meeting on the Forest Conservation (Amendment) Bill
“We have seen how the government ensured that the Char
Dham project bypassed the environment impact assessment. ...an adverse impact
could have been avoided had the project been scrutinized. For example, a lot of
landslides took place in the Tankapur to Pithoragarh stretch. There were 102
sensitive zones and 45 landslides had already taken place in 2019. A geological
investigation and EIA [Environmental Impact Assessment] may have helped avoid
this. The muck went into the river. When muck goes into rivers, the river level rises, and it can cause devastating floods.”
The environmental impact appraisal was bypassed for the
880-km Char Dham project. In an affidavit, the Union government told the
National Green Tribunal in 2018 that only new national highways and expansion
of highways longer than 100 km need prior environmental clearance under 206 EIA
notification. The Char Dham project was divided into several small stretches
separated by 16 bypasses.
The impact of climate change on the temperature in
Himachal Pradesh and Uttarakhand is also significant with over 1°C warming
compared to the long-term average. Himachal Pradesh’s average annual mean land
surface air temperature during 2022 was 1.2 °C warmer than its long-period
average for the period 1981-2010.
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Credit: HINDUSTAN TIMES
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