SPI-PAMIR

Started
January 1, 2022
Status
In Progress
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Abstract

Among the most iconic mountain ranges of the Third Pole are the Pamir Mountains, a keystone connecting the Central Asian (e.g. Tien Shan) and Himalayan mountain chains (e.g. Karakoram, Kunlun and Hindu Kush). The Pamir Mountains in Tajikistan supply water to an arid region stretching to the Aral Sea, and buffer seasonal water shortage with snow, glacier and permafrost thaw. The Pamirs’ cryosphere is thus of key importance, particularly given the ongoing challenges with water management, agriculture and energy production. Still, the response of the Pamir cryosphere and its ecosystems to climate change remains poorly understood, and the anomalous state of its glaciers exhibiting both health and decay, as well as the extent of thawing permafrost contributing additional water availability, remains an unsolved puzzle.

Permafrost is ground that remains continuously at or below 0°C for at least two consecutive years. In the collaboration between the PAMIR project and the SDSC, we will model permafrost probability for the Pamir region. The aim is to develop a machine learning surrogate of a computationally costly ground thermal model that can be applied to create maps of permafrost presence for the entire Pamir region.

People

Collaborators

SDSC Team:
Luke Gregor
Michele Volpi

PI | Partners:

Swiss Polar Institute, PAMIR project:

  • Prof. Martin Hölzle
  • Prof. Francesca Pellicciotti

More info

description

Motivation

Permafrost modelling is a challenging task that integrates decades of hourly climatic conditions. The current state of the art approach, a land surface model with elements of radiative transfer, is computationally costly at large scales. Various techniques have been developed to reduce the computational cost of the approach to make it feasible to run on a large compute cluster (Fiddes and Gruber, 2012). Machine learning offers a way to further reduce this computational cost.

Proposed Approach / Solution

The SDSC will aid the PAMIR project by creating baseline maps of permafrost and state variables for the Pamir mountain range (Figure 1) with a simple implementation of the CryoGrid model (Westermann et al., 2022). Smaller regions will be mapped with a pseudo-spatial implementation of CryoGrid (Fiddes et al., 2015) using local data to determine valid ranges for parameters (Mathys et al., 2024). These outputs will serve as training data for a machine learning surrogate. The surrogate will then be used to predict permafrost at high resolution (~ 100 m) for the entire region.

Impact

Permafrost could play an important part of the water cycle in the Pamir region, which is the reservoir for the arid downstream regions (Figure 2). Being able to map the presence and changing state of permafrost (increasing or decreasing) will help to understand the vulnerability of this region to climate change.

Figure 1: The Pamir Mountains are located in Tajikistan. The sites for the PAMIR project are indicated by circles. Access to the region is limited due to inaccessibility and in some cases political instability.

Figure 2: Conceptual summary of the complex systems we target in the PAMIR Flagship Initiative, the measurement locations and the linkages between the six proposed clusters. Figure from PAMIR proposal document.

Gallery

Annexe

Cover image source: Jason Klimatsas

Additional resources

Bibliography

  1. Westermann, S., Ingeman-Nielsen, T., Scheer, J., Aalstad, K., Aga, J., Chaudhary, N., Etzelmüller, B., Filhol, S., Kääb, A., Renette, C., Schmidt, L. S., Schuler, T. V., Zweigel, R. B., Martin, L., Morard, S., Ben-Asher, M., Angelopoulos, M., Boike, J., Groenke, B., … Langer, M. (2023). The CryoGrid community model (version 1.0) – a multi-physics toolbox for climate-driven simulations in the terrestrial cryosphere. Geoscientific Model Development, 16(9), 2607–2647. https://doi.org/10.5194/gmd-16-2607-2023
  2. Mathys, T., Azimshoev, M., Bektursunov, Z., Hauck, C., Hilbich, C., Duishonakunov, M., Kayumov, A., Kassatkin, N., Kapitsa, V., Martin, L. C. P., Mollaret, C., Navruzshoev, H., Pohl, E., Saks, T., Silmonov, I., Musaev, T., Usubaliev, R., & Hoelzle, M. (2024). Quantifying permafrost ground ice contents in the tien shan and pamir (central asia): A petrophysical joint inversion approach using the geometric mean model. EGUsphere, 2024, 1–52. https://doi.org/10.5194/egusphere-2024-2795
  3. Fiddes, J., & Gruber, S. (2012). TopoSUB: A tool for efficient large area numerical modelling in complex topography at sub-grid scales. Geoscientific Model Development, 5(5), 1245–1257. https://doi.org/10.5194/gmd-5-1245-2012
  4. Fiddes, J., Endrizzi, S., & Gruber, S. (2015). Large-area land surface simulations in heterogeneous terrain driven by global data sets: Application to mountain permafrost. The Cryosphere, 9(1), 411–426. https://doi.org/10.5194/tc-9-411-2015

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