Overview
Syllabus
Intro
Where was the ice at the Global Last Glacial Maximum?
Glaciers and climate change in Patagonia
Rationale: reconstructing the last Patagonian Ice Sheet
Setting the scene: Patagonian Climate
The Southern Westerly Winds
Last Glaciation
Geomorphology 4 key landsystems identified
Geomorphology: Upland mountain glacier landsystem
Geomorphology: Lowland land-terminating glacial landsystem
Land-terminating lowland landsystem: Monte San Lorenzo
Geomorphology: Glaciomarine landsystem
Project aims: PATICE
Methods: Geomorphology
Palaeo ice-sheet reconstruction
Timing of key advances
Annual rates of recession
Palaeoclimatic controls on ice advance and recession in the Holocene: the SAM "Pacemaker"
Insights into Antarctica
Summary and conclusions
Taught by
Seds Online