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The Lateral Eddy Viscosity Derived from the Decay of Oceanic Mesoscale Eddies

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Figure

Figure 1. (a) Two long-term eddy tracks in the ocean. (b) Time series of the amplitude blue lines indicate the linear decay periods, and the amplitude decaying rates are re-gressed from the lines
Figure 2. The power laws for eddy parameties in the ACC based on Li dataset, where the vertical axis is eddy number (in logarithm scale): (a) The number of eddies vs their am-plitude; (b) The number of eddies vs their area; (c) The number of eddies vs thei
Figure 3. The same as in Figure 2 but for global oceans. There are critical values (A02 = 38 cm, S02 = 36 × 103 km2 and T02 = 78 days) separating the e-folding decay laws into two segments
Table 1. The isopycnal eddy parameters in different periods for two long-lived eddies
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