PulseExploreJournal ClubDebatesTrendingResearchersJournals
Instagram
HomeExploreJournal ClubTrending
Synapse
⌘+K
Synapse
March 28, 2026Annals of Glaciology0 citationsOpen Access

A 70-year chronicle of the evolution of Echaurren Norte Glacier, Central Andes of Chile

JMJames McPheeDCDaniela CarriónFUFelipe Ugalde

Key Points

  • This analysis aims to document the long-term changes in the Echaurren Norte Glacier and its mass balance.
  • Analyzed satellite imagery from 1955 to 2023
  • Monitored mass balance and glacier area reduction
  • Examined changes in debris cover and glacier structure
  • ~65% reduction in glacier area observed
  • No clean ice remained visible on the surface
  • Transformation into three debris-covered units with a total area of 0.18 km

Abstract

The Echaurren Norte Glacier mass balance time series is the longest in the Southern Hemisphere, thus it is -together with the Zongo Glacier in Bolivia-a reference glacier by the World Glacier Monitoring Service (WGMS).The Echaurren Norte Glacier constitutes a reference case of glacier degradation and transition in the Central Andes of Chile, exemplifying the full spectrum of contemporary glacier evolution processes: frontal retreat, surface thinning, progressive debris cover and fragmentation.An analysis of satellite imagery from 1955 to 2023 reveals a ~65% reduction in glacier area, accompanied by an expansion of supraglacial debris.Today, no clean ice is visible at the surface, and the glacier persists as three fully debris-covered units with a combined area of only 0.18 km.These transformations indicate a shift from an active mountain glacier toward a debris-covered glacieret, characterized by negligible ice flow

Ask AI
Helpful
Bookmark
Share
View Full Paper

Cite This Study

McPhee et al. (2026) studied this question.

synapsesocial.com/papers/69c770888bbfbc51511e0a31https://doi.org/10.1017/aog.2026.10050
Ask AI
Helpful
Bookmark
Share
View Full Paper