Ning et al. (2025) Atmospheric Freezing Level Height Changes
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: International Journal of Climatology
- Year: 2025
- Date: 2025-10-07
- Authors: Liang Ning, Raymond S. Bradley, Henry F. Díaz, Douglas R. Hardy, Chuanxi Xu
- DOI: 10.1002/joc.70133
Research Groups
[Not explicitly stated in the abstract]
Short Summary
This study updates global freezing level height (FLH) changes to 2023 using observations and models, revealing significant FLH increases, particularly in extra-tropical and high northern latitudes, which are linked to accelerated glacier mass loss driven by tropical sea surface temperature variability.
Objective
- To update global freezing level height (FLH) changes to 2023 using observations and model simulations.
- To investigate the spatial patterns and drivers of FLH variations globally.
- To assess the impact of observed FLH changes on glacier mass balance, particularly in Arctic and high mountain regions.
Study Configuration
- Spatial Scale: Global, with specific focus on Tropics, extra-Tropics, high latitudes in the Northern Hemisphere, Arctic, and high mountain stations.
- Temporal Scale: Historical analysis updated to 2023, including trends over "recent decades," and future projections for "last several decades of the 21st century."
Methodology and Data
- Models used: Unspecified climate models for simulations.
- Data sources: Observational data, glacier mass balance records, and data related to tropical sea surface temperature variability.
Main Results
- Global freezing level height (FLH) changes are updated to 2023, showing positive trends.
- Relatively smaller positive FLH trends and changes are observed over the Tropics.
- Higher FLH changes are found over the extra-Tropics, with maximum FLH rises occurring over high latitudes in the Northern Hemisphere.
- Temporal FLH variations are largely driven by the variability of tropical sea surface temperature.
- Observed FLH changes over Arctic and high mountain stations have led to significant glacier mass losses.
- Glacier mass losses have accelerated in recent decades.
- Model simulations project maximum increases in tropical middle to high troposphere temperature over the last several decades of the 21st century.
Contributions
- Provides an up-to-date assessment of global freezing level height changes to 2023.
- Offers a detailed spatial analysis of FLH trends, differentiating between tropical and extra-tropical regions and highlighting high northern latitude increases.
- Identifies tropical sea surface temperature variability as a primary driver for temporal FLH variations.
- Establishes a direct link between observed FLH changes and significant, accelerated glacier mass loss in critical cryospheric regions.
- Incorporates future projections of tropical tropospheric temperature increases, suggesting continued warming impacts.
Funding
[Not explicitly stated in the abstract]
Citation
@article{Ning2025Atmospheric,
author = {Ning, Liang and Bradley, Raymond S. and Díaz, Henry F. and Hardy, Douglas R. and Xu, Chuanxi},
title = {Atmospheric Freezing Level Height Changes},
journal = {International Journal of Climatology},
year = {2025},
doi = {10.1002/joc.70133},
url = {https://doi.org/10.1002/joc.70133}
}
Original Source: https://doi.org/10.1002/joc.70133