Showing posts with label dikchu. Show all posts
Showing posts with label dikchu. Show all posts

Monday, December 30, 2024

A post GLOF look at parts of Teesta Valley (Part - 2)

More than a year has passed since the devastating GLOF disaster of October 4, 2023, that swept through the Teesta Valley. We have extensively documented the catastrophe and its aftermath in this blog. Following the GLOF, the 2024 monsoon season brought further destruction, exacerbating the damage to already weakened structures, roads, and the environment.

In the photos below, we aim to capture the changes that have unfolded during this time. With another monsoon fast approaching, our repeated calls for mitigation efforts during this dry, non-monsoon period have largely gone unheeded except for the transfer of maintenance of sections of NH10 in West Bengal from the state PWD to NHIDCL, a step forward, which is widely regarded as too little, too late.

Sikkim

Sangakalang

Both these bridges on the river bed and a larger bridge which spanned the river were swept away during the monsoons of 2024.

Dzongu
Fidang

Dikchu town

NHPC Stage V dam (Dikchu)

Sikkim and West Bengal

Tar khola NHPC Power house
All drone images by Praveen Chhetri, Junkeri Studios, 9733185815

Praful Rao,
SaveTheHills
savethehills@gmail.com
9475033744


Wednesday, October 4, 2023

GLOF in North Sikkim triggers flashfloods down stream

We have had incessant rain in our region for the past 24hrs or so and as always STH has tracked the cloud movements and put updates in our WhatsApp group 'HAZARD ALERTS 1 & 2' with a view to provide some rudimentary early warning to the community.

Perhaps it is this incessant rainfall, due to a circulation over Jharkhand, which triggered the GLOF in South Lhonak glacier in North Sikkim. A very technical study has been done and is available here
The abstract from the article is reproduced below:

The Teesta basin in Sikkim Himalaya hosts numerous glacial lakes in the high altitude glacierized region, including one of the largest and the fastest-growing South Lhonak Lake. While these lakes are mainly located in remote and unsettled mountain valleys, far-reaching glacial lake outburst floods (GLOFs) may claim lives and damage assets up to tens of kilometers downstream. Therefore, evaluating GLOF hazard associated with current and potential future glacier-retreat-driven changes is of high importance. In this work, we assess the future GLOF hazard of the South Lhonak Lake by integrating glacier and hydrodynamic modeling to calculate the lake's future volume and hydraulic GLOF characteristics and impacts along the valley. We identify the increased susceptibility of the lake to potential avalanche impacts as the lake grows in the future. Here we model six avalanche scenarios of varying magnitudes to evaluate the impact-wave generated in the lake and overtopping flow at the dam. Avalanche simulations indicate that the frontal moraine is susceptible to overtopping. The overtopping flow hydraulics is evaluated along the channel assuming no erosion of the moraine. Further, we consider three lake-breach scenarios to model GLOFs originating from the lake, flow propagation, and its downstream impacts. The uncertainty in the breach parameters including breach width and time of failure are calculated to estimate the upper and the lower hydraulic limits of potential future GLOF events. Further, the uncertainty in the flow hydraulics was evaluated using dynamic flood routing of six GLOFs that originate from the lake. Hydrodynamic GLOF modeling resulted in a predicted peak discharge of 4311 m3s−1, 8000 m3s−1, and 12,487 m3s−1 for breach depths of 20 m, 30 m, and 40 m respectively. The large-potential scenario suggests that maximum flow depth and flow velocity at Chungthang, a town proximally located to a major hydropower station built-in 2015, could reach up to 25–30 m and 6–9 m s−1, respectively. Mapping infrastructure exposed to GLOFs in the Teesta valley shows that many settlements and assets located along the river channel at Chungthang are potentially exposed to future GLOFs, indicating the need to conduct a full environmental impact assessment and potentially undertake GLOF risk mitigation measures.


I was up at 2.20am after being notified of the GLOF by a friend. I spoke to several people in Sikkim to verify the information but it was difficult to get thru and rather embarrassing to disturb a person at that time.
After becoming reasonably sure of the event, I alerted the NDMA control room at 3.33am with a request to verify the information from SSDMA. (Sikkim State Disaster Management Authority).
I was surprised at the speed at which the flood waters advanced. Luckily, most people in the low lying areas made it to higher ground, despite the non-stop rainfall and darkness. Approximate timeline of the flooding (based on information given to me this morning by a friend when the event was unfolding) is given below:

Casualties and damage:

Sikkim State Disaster Management Report
Gangtok, October 4 (IPR): The Glacial Lake Outburst Flood (GLOF) in portions of Lhonak Lake, Mangan District, which caused the rise of water levels with very high velocities downstream along the Teesta River Basin in the early hours of October 4, 2023, has caused severe damage in Mangan, Gangtok, Pakyong, and Namchi Districts.
The lake outburst in portions of Lhonak Lake in North Sikkim caused a rise in water levels with very high velocities near about 15m/sec, crossed the CWC Melli site measuring 227 m, near about 3m above Danger Level, at 0600 am.
According to the Central Water Commission (CWC), the flood occurred at midnight on October 3, 2023. Simultaneous flood forecasts for both India and Bangladesh were made at 0600 hrs and 1400 hrs. The river Teesta is flowing below the warning level at CWC Domohani FF Station. The water level at 0600 hrs is 84.83m and is expected to cross its warning level within 6 hours.
Similarly, around 1 a.m. on October 4, 2023, the major flooding of the Teesta River was reported from Chunthang. Likewise, by 2:30 pm, the flood had reached the lowlying areas of the remaining districts, causing serious destruction to public properties and public infrastructure. The communication network under Mangan District surrounding Chungthang and its pheriphery has been affected. Districts sprung into action and immediately initiated the evacuation of the people from the lowlying areas.
Further, the SDRF team from the State Home Guard and Civil Defence, Gangtok, and NDRF Pakyong has already been deployed in the affected areas.
As per  the report received from the SSDMA, the following damages have been reported from the districts:
(i) Mangan District: Chungthang cut off due to the Toong Bridge collapse. Phidang Bridge collapsed. Four pucca houses at Phidang were washed away. Two houses at Dikchu were washed away. Houses along the river line are in danger, and two GREF labourers are reported missing at Sangkhalang, as per information received from GREF sources and one person missing from Phidang.
The GREF Crusher Plant and Old Police Barrack have been washed away at Toong, and four people have been reported missing.
Forest Guest House and two units of government quarters at Sangkhalang has been swept away.
(ii) Gangtok: Four injured have been taken to Singtam Hospital. 25 people have been rescued by SDRF, more rescue is underway.
(iii) Namchi district: LD Kazi Bridge washed away. Indreni Bridge washed away. A relief camp was set up at Namphing Sai Mandir. As of now, 500 people have been kept in the relief camps, and permanent relief has been set up at  Pranami Mandir.
(iv) Pakyong district: Two minor injuries, one dead in West Bengal, and one person is under observation at Rangpo PHC. 23 army personnel have been missing and one person has been rescued at Bardang.

SSDMA

Fatalities/Missing
Known missing thus far are 23 army soldiers who were presumably swept away from their barracks at Bardang near Singtam by massive 15-20' waves of the Teesta river.
20 civilians are also reported missing.

Damages
Proper estimation of the damages in Sikkim and W Bengal may take some time. However, the major damage are as follows:

1. Sikkim Urja Dam at Chungtang, a 1200 MW Teesta Stage III Hydro Power plant was partly swept away by the GLOF resulting is huge release of water.


2. Indreni bridge at Singtam (30km from Gangtok) and another bridge at Baluatar were swept away. Several other bridges have also been washed away.

3. Control room of NHPC Stage V Dam at Dikchu has been damaged.

4. NH10 and communication lines all over Sikkim and Kalimpong district in W Bengal have been severely damaged at many places. Road towards Darjeeling from Kalimpong is severely damaged at Teesta bazar.

5. Three districts in Sikkim including Mangan (north Sikkim), Pakyong and Gangtok (east Sikkim) were severely affected. Mangan was the worst hit.

Will update this continuously over the next few days as more information is available

Incredible photos (includes drone imagery) by STH photo/videographer Praveen Chhetri of the GLOF devastation at Teesta bazaar (taken in the morning on 04Oct2023)

Why at Teesta Bazaar only and not in Sikkim?
Because there is no road access anywhere - National Highway10 (NH10) towards Siliguri is damaged and eroded, as is the highway to Gangtok. The road to Darjeeling from Teesta has been 'eaten away' by the floods this morning


As I write at 8.pm on 04Oct2023, it continues to rain in Kalimpong, Darjeeling, Kurseong and I am sure in many places in Sikkim for almost 36hrs now, at varying intensities.
Hope things get better tomorrow.

Praful Rao
Kalimpong district
Darjeeling - Sikkim Himalaya
savethehills@gmail.com
9475033744

Wednesday, March 29, 2023

SaveTheHills survey of landslides near Dikchu (East Sikkim) on 27Mar2023


 

LANDSLIDE 2

Following media reports on a major landslide occurrence at Sokpay, near DIKCHU on 26Mar2023, we made a quick visit to the region the next day. Our report:

Rainfall data for the month of MARCH of Mangan (District HQ of North Sikkim)
2021 - 249.9mm
2022 - 166.5mm
2023 - 272mm (upto 28Mar2023)
Dikchu is situated approx 2.5km (approx 21km by road) south of Mangan.

Location and Co-ordinates of the base (toe) of landslide
The landslide at Sokpay (Rakdong-Tintek block) is huge with the crown located at least 1500' above the toe. We could only survey the base (toe) of the landslide which is located very close to DIKCHU town because the landslide has cut off access to the higher reaches where several affected homesteads are located.
Co-ordinates and elevation: N27° 23.822' E88° 31.142'
Elevation: 2543ft (775m)

Brief history and date and time of occurrence
As per locals, the landslide at Sokpay took place between 3-4am on 26Mar2023.
However, they trace back the instability to 2016 when there was a landslide in the area and thereafter, smaller landslides taking place at regular (even yearly) intervals; with 'surveys' being conducted and talks of relocation also taking place but nothing being implemented.

Probable cause
This seems to be a mystery since there has been very little rainfall in this region since Oct2022. In Mar2023, Mangan and Gangtok region did receive 'excess' rainfall (see below)
But this amount and intensity of rainfall, in our experience does not trigger such a large landslide. Local people are quick to point out that it is NHPC's Stage V Dam on the Teesta river located at Dikchu as a cause and also the large power towers (pylons) at the top (crown) of the landslide as the probable trigger.
However, there is no study done to prove this.
Government officials are equally fast in saying the entire investigation is being done by the Department of Mines and Geology, Govt of Sikkim and that their report on the cause and remedial measures to be taken is awaited. They also point out that this area is landslide prone with many sinking zones - which even a cursory look at the region will prove as correct.
We also found no other evidence of large scale and recent human interference such as road/tunnel construction which could have triggered the landslide. Nor was there any erosion by a jhora or river in the close vicinity which could have caused erosion and triggered the  landslide which started from the hilltop.

Casualties and damage
There were no human lives lost even though the farmers lost cattle and pigs in the slide. 4 homes were totally damaged and 20 families have been shifted to temporary relief shelters by the government. Unlike the landslide in Pathing, both the media and government authorities seem to have mobilized immediately. The Government has implemented relief measures and also taken the help of the Power Companies to provide temporary rehabilitation to the affected families.
Road communications from DIKCHU to GANGTOK has snapped and the main road from DIKCHU to MANGAN may also be affected in case the landslide is reactivated during the oncoming monsoons.

 

 
 

LANDSLIDE 1

We discovered this landslide at Tumin Shelay, in the same area almost by accident. This huge landslide is more than a year old and seems to have been triggered by rain in an agricultural area. The farmers have lost almost 3 acres of paddy field there and around 3-5 families have been compelled to relocate. A local person guided us to the landslide which has affected the lives of the farming community in more ways than one - tourism which was coming up around a beautiful waterfall in the vicinity has died a premature death.
Like many landslides which occur in remote areas, this one never hit the headlines - in fact, I had never even heard about it, until we reached the place searching for the recent DIKCHU slide.

Location and Co-ordinates of landslide
Located at Tumin Shelay village.
Co- ordinates near the crown: N27° 19.492' E88° 30.134'
Elevation: 4082ft (1244m)


We will be uploading a short documentary, on our visit to these landslide sites. The documentary will include interviews, images and drone footages of the landslides.

Praful Rao
Kalimpong district
Darjeeling-Sikkim Himalaya
9475033744
savethehills@gmail.com











Friday, July 3, 2020

A pictoral record of the landslides of JUN 2020 in Darjeeling-Sikkim Himalaya


Shown above are the approx timelines when due to the more than normal rainfall in Jun2020, there were numerous landslides in the Darjeeling - Sikkim Himalayas and all occurred during periods of heavy rain. For example, in 6 days (17Jun-22Jun2020) Kalimpong received approx 78% of its monthly rainfall which is when all the landslides in Kalimpong took place.
More specifically:
a. Darjeeling and Kurseong area had landslides just as the SW monsoons entered the region on 12/13Jun 2020. Many of these landslides are documented here.
b. Kalimpong district which had almost no rain during this onset period, had intense rain on 17Jun which triggered a number of slides in the district.
c. Mangan (N Sikkim) and E Sikkim were the only places which had surplus rain over the winter months and continued to have very heavy rain towards June end and that triggered a number of landslides.
In order to maintain a record of the landslide events I am posting verified photos of some of them as submitted by HA members.

Kalimpong:
North Sikkim (Passingdang)
North Sikkim (District HQ: Mangan)27.4979° N, 88.5348° E

North Sikkim (Barfok)
27.509787°N, 88.437531°E
Debris Torrent as seen from across the Teesta from Mangan. No loss of lives, some houses evacuated.

Landslide at NHPC Stage V 510 MW Dam at Dikchu, East Sikkim



Landslip on Dhotrey- Maneybhanjang road (22Jun2020?)
Rimbick- Lodhoma landslide (28Jun2020)
at Chota Hatta, Kankeybong.

Breaches on NH55 (Siliguri to Darjeeling) near Pagla Jhora (Kurseong)
30Jun2020



My sincere thanks to all those who have volunteered their time and effort in 'HAZARDS ALERTS' (Whats App group)  and elsewhere to provide the information and photographs for the above record.

Praful Rao
Kalimpong district
Darjeeling Sikkim Himalaya