Glacial geomorphology of the former Patagonian Ice Sheet (44–46 °S)

Autor: Emma-Louise Cooper, Varyl R. Thorndycraft, Bethan J. Davies, Adrian P. Palmer, Juan-Luis García

Publikováno v: Journal of Maps, Vol 17, Iss 2, Pp 661-681 (2021)

We map the glacial geomorphology of the former Patagonian Ice Sheet between 44°S and 46°S. Building on previous work, our map covers a ∼50,000 km2 region of west-central Patagonia. The study area includes the eastward-flowing Río Pico, Río Cace

Externí odkaz: https://doaj.org/article/b7a55a217f89497cb93549a4743bda01

Rapid glacier recession at Monte San Lorenzo (Patagonia) in response to abrupt Southern Hemisphere warming 13.0–12.0 ka BP

Autor: Julian R. V. Martin, Varyl R. Thorndycraft, Bethan J. Davies, Ángel Rodés

Publikováno v: Journal of Quaternary Science. 38:160-173

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::56ed21e73a324c3d293b7b885f7fdd93
https://doi.org/10.1002/jqs.3463

Glacier dynamics during a phase of Late Quaternary warming in Patagonia reconstructed from sediment-landform associations

Autor: Bethan J. Davies, Varyl R. Thorndycraft, Julian R.V. Martin

Publikováno v: Geomorphology. 337:111-133

The geomorphological record in glaciated landscapes can provide important information for the study of the response of glaciers to rapid climate change. This study presents a new reconstruction of the glacial history of the northern Monte San Lorenzo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b60e4fe655307e26b1dee983da9d6c37
https://doi.org/10.1016/j.geomorph.2019.03.007

Declining discharge of glacier outburst floods through the Holocene in central Patagonia

Autor: Varyl R. Thorndycraft, Alejandro Dussaillant, Carlos Sancho, María José Machado, Gerardo Benito, Alicia Medialdea

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
instname
Digital.CSIC: Repositorio Institucional del CSIC
Consejo Superior de Investigaciones Científicas (CSIC)

Glacier outburstfloods are a major hazard in glacierized catchments. Global analyses have shownreduced frequency of glacierfloods over recent decades but there is limited longer-term data on eventmagnitude and frequency. Here, we present a Holocene p

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::304c278248df2444beb687c51fa4a304
http://hdl.handle.net/10261/243488

The Glacial Geomorphology of central-Patagonia (44 – 46°S): glacier dynamics within and beyond the austral Andes

Autor: Juan-Luis García, Bethan J. Davies, Adrian Palmer, Emma-Louise Cooper, Varyl R. Thorndycraft

The former Patagonian Ice Sheet (PIS, 38 – 56°S) was one of the largest ice masses to develop in the Southern Hemisphere. Its formation was uniquely influenced by the Southern Westerly Winds (SWWs) colliding with the Andean Cordillera, generating

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c8e269455fd573311c65e04f4e2dbf21
https://doi.org/10.5194/egusphere-egu21-13184