JRI

Glacier response to climate change

Climate change on the Antarctic Peninsula | Glacier fluctuations on James Ross Island | Glacier modelling experiments | Summary and conclusions | Further reading | Modelled glacier response to centennial temperature and precipitation trends on the Antarctic Peninsula This article is a summary of the following paper: Davies, B.J., Golledge, N.R., Glasser, N.F., Carrivick, J.L., […]

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Ice stream initiation on the northern Antarctic Peninsula

Please see the following work: Glasser, N.F., B.J. Davies, J.L. Carrivick, A. Ròdes, M.J. Hambrey, J.L. Smellie and E. Domack (2014). Ice-stream initiation, duration and thinning on James Ross Island, northern Antarctic Peninsula. Quaternary Science Reviews 86, 78-88. Download the Glasser et al. 2014 Preprint. The following is a shorter, simpler version of the paper.

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Subpolar landsystems of James Ross Island

This page is a shortened and simplified version of the paper by Davies et al. 2013, published by the Geological Society of London. It discusses a semi-arid subpolar landsystem and its paraglacial modification on James Ross Island, northeast Antarctic Peninsula. Glacial landsystems | | Methods | Sediment-landform assemblages | Processes of landscape evolution | Glacial-paraglacial-periglacial

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Periglacial environments

Introduction to periglacial environments | James Ross Island | Patriot Hills, Ellsworth Mountains | Vestfold Hills, East Antarctica | Terra Nova Bay, Northern Victoria Land | References | Comments | Introduction  to periglacial environments Periglacial, Paraglacial and Permafrost Periglacial environments are those that are in a cold climate, typically near glacierised regions. Permafrost environments are

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Antarctic terrestrial landforms

Glacial Landforms There is a huge variety of glacial landforms recognised in the geological record. However, they are difficult to see in Antarctica, because they are usually buried beneath ice. On a few small islands around the Antarctic Peninsula, however, you can see evidence of past glaciations through glacier sediments and landforms. The contrast between

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