Figure legend: Data management procedures for ARGO data.
For more information on Argo data management activities of the Physical Oceanography Division of NOAA’s Atlantic Oceanographic and Meteorological Laboratory go to:
http://www.aoml.noaa.gov/phod/argo/index.php
http://www.aoml.noaa.gov/phod/sardac/index.php
How has the distribution of XBT and Argo floats evolved with time?
XBT data were originally used in regional studies of intense ocean currents. Thus, late 1960 data are concentrated along the western boundaries of the ocean basins. With the start of the Tropical Ocean and Global Atmosphere and World Oceana Circulation Programs in the late 1980s data were routinely collected along repeated transects. The Argo array has grown from a 1990s start to a 3000-float array today.
How has the distribution of surface drifters evolved with time?
The surface drifter program started as part of the Tropical Ocean Global Atmosphere project, which focused on El Nino variability in the Pacific Ocean. Thus, early deployments (starting in 1979) were in the eastern equatorial Pacific region. As late as 1989, nearly all deployments were still conducted across the tropical Pacific basin, with very few in the tropical Indian Ocean (starting in 1985). The situation changed quickly over the next ten years, with the creation of the Global Drifter Program and emphasis on a truly global array of drifters at a nominal resolution of 5x5 degrees. Dense and regular deployments began in earnest in the North Atlantic in 1989, and throughout the Pacific and Southern oceans in the early 1990s. Deployments commenced in the South Atlantic in 1993, and sustained annual deployments in the Indian Ocean began in 1994. Finally, regular deployments in the Tropical Atlantic began in 1997. By 2000, there were over 600 drifters in all major ocean basins. In September 2005, the program reached its goal of 1250 drifters worldwide, and has subsequently maintained an array of approximately that size.
How have satellite observations evolved with time?
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