SWW

Southern Annular Mode

Today, glaciers in Patagonia and Antarctica are receding. In both cases, this has been attributed to changes in the Southern Westerly Winds and the Southern Annular Mode (SAM). The Southern Westerly Winds are an important wind belt that encircles the globe in the southern mid-latitudes1,2, with its core between 50-55°S1. The Southern Annular Mode describes […]

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The westerly winds and the Patagonian Ice Sheet

The moisture-bearing Southern Westerly Winds The Patagonian Ice Sheet, which formed during the Last Glacial Maximum (LGM) around 21,000 years ago, was strongly influenced by the Southern Westerly Winds. These winds blow around the Southern Hemisphere in the mid-latitudes (see map below) and deliver snow and rain to the western coast of southern South America[1],

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Patagonian Ice Sheet

This page summarises some of our recent research on the dynamics of Patagonian outlet glaciers during the Last Glacial Maximum and following deglaciation. Pages on glacial landforms are especially relevant to the Geography A-Level curriculum. Here, you can watch a seminar I gave about the Patagonian Ice Sheet: Further reading: QFuego-Patagonia: a website that includes

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Glaciers and Climate

This section of the website highlights how glaciers interact with climate, and how changing climate is changing glaciers around the world today. Globally, glaciers are receding and shrinking in response to atmospheric warming. The signal is remarkably consistent across different continents and mountain ranges. Glaciers are a critical water resource in many mountain regions of

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Patagonian Ice Sheet thinning during a changing climate

J.Boex, C. Fogwill, S. Harrison, N.F. Glasser, A. Hein, C. Schnabel and S. Xu.  Rapid thinning of the Late Pleistocene Patagonian Ice Sheet followed migration of the Southern Westerlies. Scientific Reports 3: 2118, p. 1-6 Download the PDF The Patagonian Ice Sheet This recent open-access paper in the new journal Science Communications, which is part

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