Harris et al. (2026) Weather News
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: Weather
- Year: 2026
- Date: 2026-01-01
- Authors: Dan Harris, Zoe Hutin
- DOI: 10.1002/wea.70026
Research Groups
- Ochwat et al. (2025) - primary authors of the new research.
- Swansea University (mentioned as a source for the research).
Short Summary
New research reveals the Hektoria Glacier on the eastern Antarctic Peninsula experienced a record-fast retreat of 25 km in 14 months (January 2022 – March 2023), driven primarily by rapid ice-plain calving due to its underlying bed shape, rather than atmospheric or oceanic conditions.
Objective
- To identify the primary drivers behind the rapid retreat of the Hektoria Glacier.
Study Configuration
- Spatial Scale: Hektoria Glacier, eastern Antarctic Peninsula, British Antarctic Territory (area approximately 298 km²).
- Temporal Scale: Glacier retreat observed between January 2022 and March 2023 (14 months). Research published in November 2025.
Methodology and Data
- Models used: Not explicitly stated. The research focuses on observational analysis of physical processes.
- Data sources:
- Observational records of glacier retreat (e.g., satellite imagery, ground measurements).
- Seismic tremors recorded during the collapse event.
- Analysis of the glacier's underlying bedrock topography (ice-plain geometry).
Main Results
- The Hektoria Glacier retreated by 25 km between January 2022 and March 2023, including a rapid loss of 8 km in just two months, marking one of the fastest observed glacier retreats on record.
- The primary driver for this retreat was rapid ice-plain calving, a destabilization and collapse mechanism triggered by the glacier's underlying bed shape.
- This finding contradicts previous assumptions that atmospheric or oceanic conditions were the main drivers.
- Seismic tremors confirmed that the glacier was grounded, indicating a loss of land ice rather than merely floating ice disintegration.
- The resulting freshwater influx into the Southern Ocean could disrupt local salinity and mixing, potentially allowing warmer deep water to reach remaining ice and accelerate further melt.
Contributions
- Provides a novel understanding of the Hektoria Glacier's rapid retreat, attributing it to ice-plain calving driven by bed shape, thereby challenging prior hypotheses focused on atmospheric/oceanic factors.
- Highlights the critical role of subglacial topography in glacier stability and retreat dynamics, particularly for glaciers with vulnerable ice-plain geometries.
- Emphasizes the potential for significant future implications for global sea-level rise, ocean currents, and climate feedbacks from similar collapses of larger glaciers.
Funding
- Not specified in the provided text.
Citation
@article{Harris2026Weather,
author = {Harris, Dan and Hutin, Zoe},
title = {Weather News},
journal = {Weather},
year = {2026},
doi = {10.1002/wea.70026},
url = {https://doi.org/10.1002/wea.70026}
}
Original Source: https://doi.org/10.1002/wea.70026