Extraordinary rains of September end 2024 (in the Darjeeling - Sikkim Himalaya).

Until the 23rd, the month of September 2024 for us in the Darjeeling-Sikkim Himalaya turned out to be very dry and inordinately hot, prompting a member of the SaveTheHill's What'sApp group 'Hazard Alerts' to write:

'What does it mean, no rain in Kalimpong, Sikkim or Darjeeling?? Paddy fields are drying, springs and streams have dried already, this year "MUL PHUTENA", meaning ground aquifers were not recharged completely. This situation warns of the chaotic food insurgency especially to those who wait for food from farmers. Poor farmers look at the sky, it looks blue, no cloud, and he screams for his hardships and crop failure. I'm a farmer, what option do I have now??'

Another member post this cartoon about the prevailing hot weather:

Then on 24Sep2024, another LOW pressure area, in a series of bumper to bumper lows which had formed in the Bay after 17July2024, developed as shown below:

IMD issued a number of press releases about the weather systems causing the heavy rain and likely weather which would ensue:

Based on IMD and other inputs, STH posted satellite imagery and weather updates continuously during the period in our WhatsApp groups 'Hazard Alerts, Hazard Alerts 2, Hazard Alerts 3' - we also used other social media handles to publicize the heavy rainfall warnings.

Rainfall data

On 29Sep2024, IMD gave us a GREEN (ie no warning after 3 days of RED warning and 1 day of orange warning in the above period) and we had a dry day after 5 days of non-stop rain.

The average monthly rainfall for September in Sub-Himalayan W Bengal and Sikkim is 388.1mm - the 5 day rainfall of Sept2024 end, as seen above came close to or in the case of many towns, exceeded the monthly average and thus we swung from a total deficiency of rain in the first three weeks of September to a gross excess of rain, all of the large volume of water coming at the end of the monsoons when the mountains are almost saturated with water. As such the impact of this unusual heavy rains was huge in the region.

IMPACT

Firstly and most importantly, there were no fatalities even though we did have many landslides and near misses.
Road Communications: NH10
The already poor state of road communications especially in the Teesta valley suffered further set backs.

Landslide on NH10 near Teesta bridge on 27Sep2024 (27 03 40.2 N 88 25 35.3 E)

Large landslide on NH10 near Melli (27.08388889N 88.45098611E)

Other places in the Teesta Valley

Flooded Darjeeling - Kalimpong road near Teesta bridge, 28Sep2024. The debris and sand deposits by the GLOF of Oct2023 had raised the level of the Teesta river by as much as 4-5m so heavy rain
always results in the river flooding this road.

Teesta Low Dam Project III at 27Mile and the flooded Bangay bazar bridge
(26°59´38.20´´N 88°26´32.83´´E)

Flood affected areas of Teesta bazar. As mentioned earlier, the GLOF of Oct2023 has pushed the riverbed levels up by 4-5m and as such the river runs perilously close to many densely populated areas - Melli, SIngtam and Rangpo to name a few. Heavy rain in the valley invariably results in flooding of these areas.

Melli town and stadium ( 27°05´23.03´´N 88°27´28.01´´). The stadium which was entirely covered by debris and sand by the GLOF in Oct2023 had been painstakingly cleaned by the town but it has been rendered unusable by the repeated flooding of the river.

The GTA Covid Hospital (27°04´48.63´´N 88°25´50.37´´E) lying derelict on the banks of the Rangeet river since the GLOF of Oct2023. Parts of the one lane road leading up to the hospital from Teesta Bazar has been under the river for a year now and the recent rains have inundated even more areas of the road.

Other parts of the Kalimpong and Darjeeling districts

Major landslide in the vicinity of Kalimpong town at the by-pass road, 7th mile (27 04 13.9 N 88 26 56.8 E). In Sep 2024, Kalimpong received less rain than Darjeeling and Kurseong and as such we never had as many landslides.This large landslide took place on 28Sep at around3.30pm.

Subsidence due to mountain stream erosion (jhora) in a densely populated area of Kalimpong municipality (27 03 47.0 N 88 27 45.8 E). The subsidence (seen here covered by plastic sheets to prevent water ingress) occurred during daytime on 28Sep2024 when the stream was gorged with runoff from upstream paved surfaces. My concern here is that this whole area is located above a landslide prone zone on which we have done a story in 2010.

Landslide in the Darjeeling Municipal area at Hooker Road, on 26Sep2024

Landslide at Lower Bhaktey bustee in Darjeeling

Sikkim received much less rainfall in late Sep2024 resulting in much less devastation and landslides.

I am sure there were many more unreported landslides and instances of flooding caused by the unusual heavy rains and we will keep updating this blog on the reports, when received. We will also be surveying the affected areas in due course of time.

My thanks to all HA members whose images and reports I have used liberally here and elsewhere - all with the intention of recording the event for posterity.

Documentation of parts of the above report was supported by Royal Enfield, as part of their Social Mission Initiative


Praful Rao
SaveTheHills
savethehills@gmail.com
9475033744

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