Fieldnotes

Dendrochronological fieldwork in the Eastern Himalayas to understand changes to water resources and natural hazards in the context of climate change – Nazimul Islam

In the Himalayas, glacier-fed rivers are an important source of freshwater for millions of people downstream. The cryosphere being very sensitive to rising temperatures, climate-change induced seasonal snow and glacier melt may have tremendous impact on streamflow in such basins. Its impact may be combined with anthropogenic interventions (e.g. hydropower) and changes in land use. Not only are water resources likely to be significantly affected but also natural hazards, notably glacial lake outburst floods (GLOFs) and landslide lake outburst floods (LLOFs). As a result, it is crucial to understand how snow and glacier melt during both the high and low-flow (monsoon and non-monsoon) seasons influences river discharge and its variation.

This project focuses on a little-known part of the Eastern Himalayas in the state of Sikkim, and on quantifying how climate change is simultaneously impacting both water-related risks and water-related resources in the Himalayas, and crucially how far downstream. It is doing so by combining stable isotope and anatomical analysis of tree rings, starting close to the glaciers that are the source of the Teesta River and continuing over a large distance downstream.

Sampling positions (SPs) in the Eastern Himalayas: Our field-campaign for data collection started from the proximity to the Zemu Glacier (largest glacier in the eastern Himalaya) to the downstream along the Zemu River. © Nazimul Islam, all rights reserved

Fieldwork in the Eastern (Sikkim) Himalaya

With the support of the Swiss Polar Institute, two fieldtrips were successfully completed in 2022. The first, during the pre-monsoon period in April and May involved coring trees along the Teesta River and one of its tributaries, starting at the Zemu Glacier, the largest in the Eastern Himalaya. Samples were collected from two tree species, the Bhutan fir (Abies densa) and the Himalayan larch (Larix graffithiana). Sampling considered both trees close to the river and those more distal. The work was completed in a highly inaccessible area of the Himalaya, during a difficult trek, due to missing footpaths and bridges.

Difficulties to reach the sampling sites in a highly inaccessible region: In most cases, there were no footbridges to cross the river. © Nazimul Islam, all rights reserved
Coring trees for collecting samples near the river: Tree-rings are collected from the living trees using an increment borer. © Nazimul Islam, all rights reserved
Observing site conditions with my supervisor: An interesting site where floods and landslides might have left some imprints on the trees. © Nazimul Islam, all rights reserved
Collecting additional information of the trees: Beside collecting tree-rings, we also recorded some additional information such as the site conditions where the tree is growing, its canopy status, size, etc. © Nazimul Islam, all rights reserved

The second visit, in November 2022, considered a tributary of the Teesta River slightly further east, where landslide dam outbreak floods and related natural hazards were suspected. Access was easier. The same tree species as in the first visit were cored to reconstruct flood and landslide histories.

Both field visits suggest that our planned sampling strategy will yield the datasets that our project needs. The cores show distinctive patterns of growth and of changes in tree ring width that could relate to disturbances from landslides and/or flooding. Century-long (>100 years) time series from the old trees will allow longer chronologies to be developed thus allowing analyses into the pre-instrumental period.

Tree-rings after the sample processing: The tree-rings and their growth patterns are clearly visible after processing the raw data we collected from the field. © Nazimul Islam, all rights reserved

Future prospects of more dendrochronological research for hazards monitoring

Fig. 1 – Evidence of forest fires in trees.
© Nazimul Islam, all rights reserved
Fig. 2 – Evidence of landslide. © Nazimul Islam, all rights reserved
Fig. 3 – Evidence of rockfall/avalanche.
© Nazimul Islam, all rights reserved

In many occasions we found evidences of forest fire in the trees (Fig. 1). However, no such damaged trees were cored during the fieldtrips because our research goals are different, but looking at these trees, it gives ample opportunity to extend our research goals further and reconstruct forest fire events in the Himalayas.

On our way back to sampling position (SP) 2 from SP-1 we have encountered a massive landslide event (Fig. 2). However, this was not the only place where we spotted such chunk of snow, ice and debris slide down and blocked the river course.

Rockfall/avalanche paths (Fig. 3) were seen very often in our study area and as the local sources informed that these paths become active during the monsoon period (June-September) every year. These events damaged the trees externally (in the bark) and internally (in the rings, and cells) on their paths. Therefore, dating those damaged trees can help dendrochronologists to reconstruct these events in the past.

We are extremely thankful to the Swiss Polar Institute (SPI) for providing us the financial support under the scheme of Polar Access Fund 2022 to successfully conduct two proposed fieldworks in the Eastern part of the Himalayas.

Nazimul Islam is a doctoral researcher at the University of Lausanne. His fieldtrips took place in April-May and in November 2022 with the financial support from a Polar Access Fund grant.

Header photograph: Tree-rings after the sample processing. © Nazimul Islam, all rights reserved