APIS

Antarctic Peninsula has strong sensitivity to surface warming

The Antarctic Peninsula is warming very rapidly, about six times the global average[1-3]. There has been a 95% increase in positive degree day sums since 1948[4]. Glaciers in the region are accelerating, in response to frontal thinning and recession[5]. In addition, ice shelves are collapsing[6], glacier fronts are retreating[7]. The causes for much of these

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Antarctica

The Antarctic continent | The Antarctic Ice Sheets | Ice streams, subglacial lakes and ice shelves in Antarctica | Wildlife of Antarctica | Exploration of Antarctica | References | Comments | The Antarctic continent Antarctica: the enigmatic, romantic, remote white continent. Antarctica lies at the bottom of the world and all waters south of 60°S

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Antarctic Peninsula Ice Sheet

Introduction | Oceanography and climate | Modern Glaciology | Geological history | References | Comments | Introduction This section largely taken from Davies et al., 2012 (Quaternary Science Reviews)[1]. The Antarctic Peninsula Ice Sheet (sometimes written as APIS) is widely regarded as sensitive to climate change due to its small size and northerly location, and

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Antarctic Peninsula Ice Sheet evolution

Pre-Quaternary Antarctic Peninsula Ice Sheet evolution | Quaternary glaciation of the Antarctic Peninsula | Last Glacial Maximum | Antarctic Peninsula Ice streams | References | Comments | This section is largely taken from Davies et al. 2012 (Quaternary Science Reviews)[1], and summarises Antarctic Peninsula Ice Sheet evolution throughout the Cenozoic, Last Glacial Maximum and into

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