Glaciers of the Antarctic
Motion and change define a glacier's life. Glacial ice advances, then retreats. Glaciers grow and shrink in response to changing climate. Typically glacier movement and shape shifting occur over long periods of time (hundreds to thousands of years), but within historic memory such transformations in fewer than 100 years are not unknown.
Not all glaciers move slowly. For example, surging glaciers experience dramatic increases in flow rate, sometimes traveling as much as ten to one hundred times faster than the normal rate of movement.
By their movement, glaciers mark change and for this reason - among others - scientists, notably Dr. Fritz Koener, study glaciers. By monitoring glaciers over time and around the world, researchers construct valuable records of glacial activity and their response to climate variation.
By comparing contemporary observations with historical and environmental records, such as agricultural records, pre-historic temperature or climate profiles, glaciologists acquire and provide an enhanced understanding of global processes and change.
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Dr. Roy
'Fritz' Koerner
'Shut that door and keep those bloody Birders
out!'
Canada's leading
glaciologist and recipient of two Polar Medals for his work in both Antarctica
and the Arctic.
He is a senior member of the National Glacialogy Program at the Geological Survey of Canada In 1968-69, Fritz was a member of the remarkable British Trans-Arctic Expedition. A four-party group that crossed the Arctic Ocean sea ice from Barrow, Alaska to Svalbard, Spitzbergen via the North Pole. Perhaps one of the greatest polar expeditions of all time!
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