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Xu Ming,Chen Ge,Peng Lin. Temporal and spatial properties of short-life oceanic eddies[J]. Haiyang Xuebao,2019, 41(9):94–104,doi:10.3969/j.issn.0253−4193.2019.09.009
Citation: Xu Ming,Chen Ge,Peng Lin. Temporal and spatial properties of short-life oceanic eddies[J]. Haiyang Xuebao,2019, 41(9):94–104,doi:10.3969/j.issn. 0253−4193.2019.09.009

Temporal and spatial properties of short-life oceanic eddies

doi: 10.3969/j.issn.0253-4193.2019.09.009
  • Received Date: 2019-01-31
  • Rev Recd Date: 2019-05-19
  • Available Online: 2021-04-21
  • Publish Date: 2019-09-25
  • Mesoscale eddies are widely distributed in the ocean and play a significant role in the mixing and transporting of momentum and nutrients. Statistics suggest that more than 80% eddies’ lifetime are less than 1 month, belonging to the defined “short-life eddies” in this paper. This design adopt statistics and comparison, commit to having a earlier reasearch of global scale, short-life eddies. Results show that short-life eddies have a close correlation with ocean current. The most productive places for short-life eddies are those where warm and cold currents or two currents with opposite directions meet, and except in tropical areas of 30°S–30°N, the short-life eddies in other areas have a slight preference for cyclonic. Seasons with low temperature are favorable for short-life eddies in low latitudes, while seasons with high temperature are favorable in high latitudes. Short-life eddies tend to propagate westward in most of areas, however, they notable propagate eastward in eastward currents areas. Meridional deflection is quite messy, but with a tiny preference for equatorward and poleward deflections of cyclones and anticyclones, respectively. The distribution of average displacement and propagation velocity have similar regulation.
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