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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 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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