In Pacific Air Forces initiated "Operation Clean Sweep", in which abandoned Cold War stations in Alaska were remediated and the land restored to its previous state. The site remediation of the radar and support station was carried out by the th Civil Engineering Squadron at Elmendorf, and remediation work was completed by The airport remains open to support the small settlement at Kaktovik and to provide contractor support access to the military radar site.
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Barter Island controlled nine manned stations, four of them being classified as "auxiliary" sites and five "intermediate" stations. The auxiliary stations were similar to the main site at Barter Island; the intermediate sites had less personnel at them.
The sites had one man module building for personnel who supported the radar, and an airstrip, although the length and capacity varied greatly, making frequent risky landings necessary at some sites. Each of the sites was staffed by civilian contract workers who had signed month contracts, although they were visited by Air Force military personnel frequently. The intermediate sites were closed in due to the advancements in radar technology.
From Wikipedia, the free encyclopedia. Source: Federal Aviation Administration .
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December Retrieved January 14, Arctic Circle. The upper sediment column of the coastal North Slope of Alaska can be described as continuous permafrost underlying a thin typically less than 1—2 m active layer that responds variably to seasonal thaw cycles. Assessing the temporal and spatial variability of the active layer and underlying permafrost is essential to better constrain how heightened erosion may impact material fluxes to the atmosphere and the coastal ocean, and how enhanced thaw cycles may impact the stability of the coastal bluffs.
In this study, multi-channel electrical resistivity tomography ERT was used to image shallow subsurface features of a coastal bluff west of Kaktovik, on Barter Island, northeast Alaska. A comparison of a suite of paired resistivity surveys conducted in early and late summer provided detailed information on how the active layer and permafrost are impacted during the short Arctic summer. Such results are useful in the development of coastal resilience models that tie together fluvial, terrestrial, climatic, geologic, and oceanographic forcings on shoreline stability.