Completed catalogue assessment
- Eligibility decision
- Include · Include
- Assessment date
- 28 September 2026
- Decision reason
- Original source identity and relevant content established; exact unsupported metadata replaced and evidential limits recorded.
- Metadata corrections
- {"canonical_title":"Glacier changes in Langtang Catchment, Central Nepalese Himalaya from the Little Ice Age (∼1815 CE) to 2023 CE","title_original":"Glacier changes in Langtang Catchment, Central Nepalese Himalaya from the Little Ice Age (∼1815 CE) to 2023 CE","publication_date":"2026-06-08","last_updated":"","access_url":"https://researchportal.northumbria.ac.uk/files/235093140/1-s2.0-S0921818126002766-main.pdf","temporal_start":"approximately 1815","temporal_end":"2023","production_method":"Reconstructs regional glacier outlines and area changes from mapped geomorphological evidence and multitemporal imagery, with historical climate context.","validation_status":"peer_reviewed_study","uncertainty_summary":"Mapped area-loss uncertainty accompanies the outlines. The source does not establish the previously asserted new lichenometric and cosmogenic cross-validation. Abstract and table percentages differ slightly; approximately 41% is an appropriately qualified summary.","limitations":"Regional historical baseline predating the 2026 event. It does not independently demonstrate source-zone debuttressing, permafrost degradation, or the cause of the later failure.","bbox_wgs84":"","reviewed_on":"2026-09-28","current_status":"eligibility_assessed"}
Identity and coverage
- Catalogue identifier
- res-1413cde3-9223-5000-97f2-1c18deae0117
- Persistent identifier
- 10.1016/j.gloplacha.2026.105555
- Resource version
- 1
- Publication date
- 8 June 2026
- Last updated
- Not stated
- Metadata reviewed
- 28 September 2026
- Language
- English
- Geographic coverage
- Langtang River Basin, Central Nepal Himalaya
- Bounding box (WGS 84)
- Not stated
- Temporal coverage
- approximately 1815 to 1 January 2023; Historical Baseline
- Themes
- Glaciology, Climate Warming, Decadal Deglaciation, Thermal Debuttressing, High Mountain Asia, Cryosphere
Method and provenance
- Production method
- Reconstructs regional glacier outlines and area changes from mapped geomorphological evidence and multitemporal imagery, with historical climate context.
- Provenance
- Published in Global and Planetary Change (Vol. 264, Article 105555) by an international research team.
- Validation
- Peer Reviewed Study
- Uncertainty
- Mapped area-loss uncertainty accompanies the outlines. The source does not establish the previously asserted new lichenometric and cosmogenic cross-validation. Abstract and table percentages differ slightly; approximately 41% is an appropriately qualified summary.
- Limitations
- Regional historical baseline predating the 2026 event. It does not independently demonstrate source-zone debuttressing, permafrost degradation, or the cause of the later failure.
Access and reuse
- Access
- Direct Open; open access route
- Licence
- CC-BY-4.0; licence evidence
- Redistribution
- Permitted Under Stated Licence
- Catalogue status
- Included
- Provider page
- Open authoritative resource page
Assets
1 assetGlacier changes in Langtang Catchment, Central Nepalese Himalaya from the Little Ice Age (∼1815 CE) to 2023 CE
Asset bounding box not stated. Parent resource coverage: Langtang River Basin, Central Nepal Himalaya