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Mauna Loa Observatory

Atmospheric research station on island of Hawaii

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  • 4 chapters

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History

MLO was founded on June 28, 1956, as part of the US Weather Bureau. It was established on the northern flank of Mauna Loa at 3,394 meters (11,134 ft) after 1951–1954 efforts were unable to maintain a summit observatory at 4,100 meters (13,453 ft).

MLO was developed specifically to monitor solar, atmospheric, and meteorological parameters in the free atmosphere. The establishment of a solar constant, routine weather observations, the determination of ozone, and monitoring atmospheric circulation were early priorities. Continuous carbon dioxide measurements began in March of 1958 directed by Charles David Keeling from the Scripps Institute of Oceanography. The data set, referred to as the Keeling Curve, is the foundational study in the composition and behavior of greenhouse gases in the atmosphere. Other early research at the observatory included measurements of cosmic radiation, the atmosphere of Mars, atomic fallout, snow crystals, the solar corona, meteors, cosmic rays, and radio transmission. The International Geophysical Year enabled many of the early projects at the observatory to secure support and funding.

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