Akzharkynova et al. (2026) Climate-Driven Cryospheric Changes and Their Impacts on Glacier Runoff Dynamics in the Northern Tien Shan
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: Atmosphere
- Year: 2026
- Date: 2026-01-03
- Authors: Aigul N. Akzharkynova, Berik Iskakov, Gulnara Iskaliyeva, Nurmakhambet Sydyk, Rustam G. Abdrakhimov, Alima Amangeldi, Aibek Merekeyev, A. Chigrinets
- DOI: 10.3390/atmos17010063
Research Groups
[Information not provided in the paper text.]
Short Summary
This study quantifies long-term changes in glacier area, firn-line elevation, and glacier runoff in the Northern Tien Shan from 1955 to 2021, revealing a significant decline in glacier area and meltwater contribution to annual discharge due to climate warming, despite an increase in total runoff.
Objective
- To quantify long-term changes in glacier area, firn-line elevation, and glacier runoff in the Northern Tien Shan from 1955 to 2021 to assess the impact of ongoing climate warming on water resources.
Study Configuration
- Spatial Scale: Northern Tien Shan (Ile River basin, supplying Almaty, Kazakhstan).
- Temporal Scale: 1955 to 2021.
Methodology and Data
- Models used: Empirical and semi-empirical runoff estimation methods.
- Data sources: Multi-decadal meteorological observations, hydrological records, multi-temporal Landsat-7/8 and Sentinel-2 imagery, Digital Elevation Models (DEMs).
Main Results
- Glacier area in the Northern Tien Shan declined by more than 45% to 60% since 1955.
- Firn-line altitude rose from approximately 3400 meters to 3700 meters.
- Mean summer air temperature at Mynzhylky station increased by 0.88 °C, indicating persistent warming at glacierized elevations.
- The contribution of glacier meltwater to annual discharge decreased from approximately 32% during 1955–1990 to approximately 25% during 1991–2021.
- Total and vegetation-period runoff increased due to modified seasonal hydrological conditions.
Contributions
- Provides a comprehensive long-term (1955–2021) quantification of glacier degradation and its impact on runoff in the Northern Tien Shan, a critical water source for Almaty.
- Demonstrates the direct link between climate warming, glacier retreat, and altered hydrological regimes in a vital glaciated region.
- Highlights the urgent need to integrate glacier degradation into water-resource management and long-term water-security assessments for the region.
Funding
[Information not provided in the paper text.]
Citation
@article{Akzharkynova2026ClimateDriven,
author = {Akzharkynova, Aigul N. and Iskakov, Berik and Iskaliyeva, Gulnara and Sydyk, Nurmakhambet and Abdrakhimov, Rustam G. and Amangeldi, Alima and Merekeyev, Aibek and Chigrinets, A.},
title = {Climate-Driven Cryospheric Changes and Their Impacts on Glacier Runoff Dynamics in the Northern Tien Shan},
journal = {Atmosphere},
year = {2026},
doi = {10.3390/atmos17010063},
url = {https://doi.org/10.3390/atmos17010063}
}
Original Source: https://doi.org/10.3390/atmos17010063