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. 2020 Mar 12;18(3):159. doi: 10.3390/md18030159

Table 2.

Recorded data of the rate of dissipation of turbulent kinetic energy (ε, ms−3) at the three sites. Data are expressed as mean ± standard deviation and [maximum–minimum]. Results of the analysis of two-way ANOVA showing the effects of site and depth (5–50 m) and their interactions on ε; df—degrees of freedom; MS—mean squares.

Epsilon, ε (m2 s−3) Coast Jet Gyre
Depth averaged
(5–200 m)
1.06 10−6 ± 2.07 10−6
[1.63 10−9–7.44 10−6]
3.25 10−6–6.05 10−6
[8.24 10−10 ± 2.18 10−5]
1.71 10−8 ± 3.43 10−8
[1.32 10−9–1.22 10−7]
Daily averaged
(5 m)
3.16 10−6 ± 2.6 10−6 1.21 10−5 ± 5.8 10−6 -
Daily averaged
(25 m)
1.12 10−8 ± 1.25 10−8 1.84 10−6 ± 3.65 10−6 6.032 10−9 ± 6.54 10−9
Source of variation df MS F p
site 2 6.37 10−11 4.835 0.017
Depth 1 3.33 10−10 25.27 0.00039
Site × depth 1 2.89 10−10 21.99 0.000091