Polygon experiment

The POLYGON experiment was a pioneer experiment in oceanography conducted in the middle of the Atlantic Ocean during the 1970s.[1][2] The experiment, led by Leonid Brekhovskikh, was the first to establish the existence of so-called mesoscale eddies, eddies at the 100 km (60 mi) and 100-day scale, which triggered the "mesoscale revolution".[1] The existence of mesoscale eddies was predicted by Henry Stommel in the 1960s,[3] but there was no way to observe them with traditional sampling methods.[1]

  1. ^ a b c Munk & Day (2008)
  2. ^ 16°30′N 33°30′W / 16.500°N 33.500°W / 16.500; -33.500, see Brekhovskikh et al. (1971)
  3. ^ Mikhalevsky (2005)

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