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Where was the ice at the Global Last Glacial Maximum?
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Classroom Contents
The Evolution of the Patagonian Ice Sheet from 35 ka to the Present Day
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- 1 Intro
- 2 Where was the ice at the Global Last Glacial Maximum?
- 3 Glaciers and climate change in Patagonia
- 4 Rationale: reconstructing the last Patagonian Ice Sheet
- 5 Setting the scene: Patagonian Climate
- 6 The Southern Westerly Winds
- 7 Last Glaciation
- 8 Geomorphology 4 key landsystems identified
- 9 Geomorphology: Upland mountain glacier landsystem
- 10 Geomorphology: Lowland land-terminating glacial landsystem
- 11 Land-terminating lowland landsystem: Monte San Lorenzo
- 12 Geomorphology: Glaciomarine landsystem
- 13 Project aims: PATICE
- 14 Methods: Geomorphology
- 15 Palaeo ice-sheet reconstruction
- 16 Timing of key advances
- 17 Annual rates of recession
- 18 Palaeoclimatic controls on ice advance and recession in the Holocene: the SAM "Pacemaker"
- 19 Insights into Antarctica
- 20 Summary and conclusions
