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International Polar Year


The International Polar Years (IPY) are collaborative, international efforts with intensive research foci on the polar regions. Karl Weyprecht, an Austro-Hungarian naval officer, motivated the endeavor in 1875, but died before it first occurred in 1882–1883. Fifty years later (1932–1933) a second IPY took place. The International Geophysical Year was inspired by the IPY and was organized 75 years after the first IPY (1957–58). The fourth, and most recent, IPY covered two full annual cycles from March 2007 to March 2009.

The First International Polar Year was proposed by an Austro-Hungarian naval officer, Karl Weyprecht, in 1875 and organized by Georg Neumayer, director of the German Maritime Observatory. Rather than settling for traditional individual and national efforts, they pushed for a coordinated scientific approach to researching Arctic phenomena. Observers made coordinated geophysical measurements at multiple locations in the Arctic during the same year enabling multiple views of same phenomena, allowing broader interpretation of the available data and a validation of the results obtained.

It took seven years to organize the first IPY which had twelve participating nations: the Austro-Hungarian Empire, Denmark, Finland, France, Germany, Netherlands, Norway, Russia, Sweden, United Kingdom, Canada, and United States.

The aforementioned countries operated 12 stations in the Arctic and two in the sub-Antarctic. Six additional meteorological stations were organized by Neumayer at Moravian mission stations on the east coast of Labrador. Observations focused on meteorology, geomagnetism, auroral phenomena, ocean currents, tides, structure and the motion of ice and atmospheric electricity. More than 40 meteorological observatories around the world expanded the IPY programs of observations for this period. Data and images from the first IPY have very recently been made available for browsing and downloading on the internet. These records of the first IPY offer a rare glimpse of the circumpolar Arctic environment as it existed in the past and hold the potential to improve our understanding of historical climate variability and environmental change in the Arctic.


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