Mauna Loa Observatory

The Mauna Loa Observatory (MLO) is an atmospheric baseline station on Mauna Loa, on the island of Hawaii, located in the U.S. state of Hawaii.

The Observatory on Mauna Loa
Satellite image of the summit of Mauna Loa overlaid with 100-meter contour lines.

The observatory
Two domes house solar sensors.
The Keeling Curve: Atmospheric CO2 concentrations as measured at Mauna Loa Observatory

Since 1958, initially under the direction of Charles Keeling, followed by his son Ralph and later Elmer Robinson, Mauna Loa Observatory (MLO) has been monitoring and collecting data relating to atmospheric change, and is known especially for the continuous monitoring of atmospheric carbon dioxide (CO2), which is sometimes referred to as the Keeling Curve. The observatory is under the Earth System Research Laboratory which is part of the National Oceanic and Atmospheric Administration (NOAA). According to the NOAA, Mauna Loa is the world's oldest continuous CO2 monitoring station, and the world's primary benchmark site for measurement of the gas. [1]

The latest observation of CO2 concentrations from MLO can be found at web sites along with data from other sites[2] and trends at Mauna Loa.[3] The MLO levels can be compared with other sites in the global monitoring network.

MLO has activities at five locations on the Big Island. The primary observing site is located at the 3,397 metres (11,145 ft) level on Mauna Loa's north slope (19°32′10″N 155°34′34″W) about 5 kilometres (3 mi) north of the summit Mokuaweoweo. The Mauna Loa Solar Observatory shares this site. The administration and some data processing are done in the Hilo, Hawaii office. Kulani Mauka is a rain collection site. Cape Kumukahi is a flask sample site located on the easternmost point of Hawaii. At the Hilo airport, weekly balloon-borne instruments are prepared and launched to measure ozone from the surface to usually over 30 km (19 mi).[4] The observatory site is also a temporary home to a cosmic microwave background observatory called AMiBA.[5]

Mauna Loa was originally chosen as a monitoring site because, located far from any continent, the air was sampled and is a good average for the central Pacific. Being high, it is above the inversion layer where most of the local effects are present and there was already a rough road to the summit built by the military. The contamination from local volcanic sources is sometimes detected at the observatory, and is then removed from the background data.[6]

See also

References
  1. "Carbon Dioxide at NOAA's Mauna Loa Observatory reaches new milestone: Tops 400 ppm". National Oceanic and Atmospheric Administration. May 10, 2013. Retrieved June 12, 2014.
  2. "Carbon Cycle-Greenhouse Gases Observatory Measurements". National Oceanographic and Atmospheric Administration. Archived from the original on February 8, 2007. Retrieved July 4, 2009.
  3. "Trends in Atmospheric Carbon Dioxide - Mauna Loa". Retrieved July 4, 2009.
  4. "Ozonesonde". NOAA Ozone Layer web site. Retrieved July 4, 2009.
  5. "Mauna Loa Solar Observatory". mlso.hao.ucar.edu. Retrieved July 4, 2009.
  6. Steven Ryan (1995). "Quiescent Outgassing of Mauna Loa Volcano 1958-1994". Mauna Loa Revealed: Structure, Composition, History, and Hazards Geophysical Monograph 92, American Geophysical Union. Archived from the original on January 14, 1998. Retrieved July 4, 2009.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.