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Progress in Earth and Planetary Science
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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 DH (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
  1. Time series smoothed by a 35-month running mean filter were used for the calculations
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