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Orange line in extent image (left) and gray line in time series (right) indicate 1981 to 2010 average extent for the day shown.
The AEC will host a Broadband Summit on July 13-14, 2016 in the Arctic community of Barrow, Alaska.
Join AEC Chair Tara Sweeney as she and other Arctic leaders explore transnational broadband strategy for the Arctic.
The final agenda for the Arctic Broadband Summit is released: Arctic Broadband Summit FINAL Agenda At a time of increasing focus on the Arctic, reliable high-speed communications technologies are becoming increasingly vital.
Expanding broadband access and adoption is crucial for indigenous and local people living and doing business in some of the most remote areas on Earth.
Additionally, as broadband usage continues to skyrocket across the globe, communities without broadband access will become even more isolated from the world.
Many of these proxies reveal cyclical patterns that provide a basis for astronomical tuning.
Recent advances in dating technology, calibration and age modelling allow for measuring smaller quantities of material and to more precisely date previously undatable material (i.e.
foraminifera for C, and single-grain luminescence). However, for much of the Pleistocene there are still limits to the resolution of most dating methods.
Consequently improving the accuracy and precision (analytical and geological uncertainty) of dating methods through technological advances and better understanding of processes are important tasks for the future.
Without effective and reliable connectivity, these communities will be deprived of economic, social, civic, and political engagement needed to survive in the 21 century.
Arctic topics will include the challenges of connectivity, the government’s role in, and commitment to, broadband development, and private investment opportunities.
To better understand Pleistocene climatic changes in the Arctic, integrated palaeoenvironmental and palaeoclimatic signals from a variety of marine and terrestrial geological records as well as geochronologic age control are required, not least for correlation to extra-Arctic records.