Smith et al. (2025) Strongly Heterogeneous Surface‐Water Warming Trends in High Mountain Asia
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: Geophysical Research Letters
- Year: 2025
- Date: 2025-11-23
- Authors: Taylor Smith, Bodo Bookhagen
- DOI: 10.1029/2025gl119418
Research Groups
Not available from the abstract.
Short Summary
This study examines long-term (1994–2023) and high-resolution (30 m) changes in water-surface temperature across High Mountain Asia, revealing a significant increase in temperatures, particularly in snow-covered regions, with an acceleration in the last decade and surface water warming faster than land.
Objective
- To examine long-term (1994–2023) and high-resolution (30 m) changes in water-surface temperature over a large and topographically diverse region encompassing the world's highest mountains.
Study Configuration
- Spatial Scale: Large and topographically diverse region encompassing the world's highest mountains, with a resolution of 30 meters.
- Temporal Scale: Long-term, from 1994 to 2023.
Methodology and Data
- Models used: Not specified in the abstract.
- Data sources: Not explicitly specified in the abstract, but implies high-resolution surface temperature measurements.
Main Results
- Water-surface temperatures have significantly increased across the vast majority of the study area, with rates up to 0.3 °C and an average increase of 0.1 °C.
- The warming is particularly pronounced in snow-covered regions.
- A notable acceleration in water-surface temperature increase has been observed over the past decade.
- Surface water is warming faster than nearby land areas.
- Changes in the cryosphere are posited to induce strong spatial heterogeneities in surface-water warming, leading to both drastic increases and localized decreases in surface-water temperature.
Contributions
- Provides a long-term (1994–2023) and high-resolution (30 m) analysis of water-surface temperature changes in High Mountain Asia.
- Quantifies the significant increase in water-surface temperatures and identifies an acceleration in warming over the last decade.
- Highlights that surface water is warming faster than adjacent land areas.
- Proposes a mechanism (cryosphere changes) for the observed spatial heterogeneity in surface-water warming.
Funding
Not available from the abstract.
Citation
@article{Smith2025Strongly,
author = {Smith, Taylor and Bookhagen, Bodo},
title = {Strongly Heterogeneous Surface‐Water Warming Trends in High Mountain Asia},
journal = {Geophysical Research Letters},
year = {2025},
doi = {10.1029/2025gl119418},
url = {https://doi.org/10.1029/2025gl119418}
}
Original Source: https://doi.org/10.1029/2025gl119418