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Progress in Earth and Planetary Science

Table 3 Damping rates of the SSH disturbances per year, i.e., exp(−rmn×1 year), with respect to the vertical and meridional modes for the case of B=1×10−7 m2s−3 and DH=10 m2s−1

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

Meridional modes

Vertical modes

    
 

n=0

n=1

n=2

n=3

n=4

m=1

0.999

0.377

0.028

0.000

0.000

m=2

0.995

0.376

0.028

0.000

0.000

m=3

0.988

0.373

0.028

0.000

0.000

m=4

0.980

0.370

0.028

0.000

0.000

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