Due to its unique location, dedicated and highly trained staff, and excellent power and communications infrastructure, the Barrow Atmospheric Baseline Observatory is host to numerous cooperative research projects from around the world. This facility is staffed year round by 2 engineers/scientists to complete routine inspections and maintenance of the instruments. Because of its proximity to these bodies of water and theįact that the prevailing winds are off the Beaufort Sea, BRW is perhaps best characterizedĪs having an Arctic maritime climate affected by variations of weather and sea ice conditions The concentration of atmospheric carbon dioxide at Mauna Loa Observatory, Hawaii is reported for eight years (19641971) of a long term program to document. Keeling, who also runs a parallel program at SIO to measure changes in atmospheric O 2 and Ar abundances ( Scripps O. It is currently being continued by Ralph F. The Scripps CO 2 program was initiated in 1956 by Charles David Keeling and operated under his direction until his passing in 2005. There are large lagoons and a number of lakes in the vicinity, and the Arctic Ocean is less CO 2 Concentration at Mauna Loa Observatory, Hawaii. It is about 8 km northeast of the village of Utqiaġvik (formerly Barrow) Alaska, and has a prevailing east-northeast windĪlthough the measurements at BRW are made over open tundra, Hundreds of lava flows were erupted during this time, but they did not cover the volcano evenly. The Barrow Atmospheric Baseline Observatory (BRW), established in 1973, is located on the northern most point of the United States. (Public domain.) Detailed geologic mapping and dating of lava flows above sea level have shown that about 90 percent of Mauna Loa's surface is covered with flows erupted within the past 4,000 years.
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