Progress in Earth and Planetary Science

Table 2 Dependence of the correlation coefficients between the observed and simulated SSH at station K2 on the eddy dissipation coefficients B (m²s⁻³) and D_H (m²s⁻¹)

From: Wind-driven decadal sea surface height and main pycnocline depth changes in the western subarctic North Pacific

D _H	B
	0	1×10⁻⁸	5×10⁻⁸	1×10⁻⁷	2×10⁻⁷
0	0.436	0.358	0.758	0.785	0.781
1	0.423	0.366	0.759	0.786	0.781
10	0.333	0.421	0.763	0.788	0.784
50	0.267	0.498	0.744	0.767	0.763
100	0.337	0.507	0.712	0.735	0.731

Time series smoothed by a 35-month running mean filter were used for the calculations

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