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Table 4 Absolute values of differences in amplitude of semiannual prograde and semiannual retrograde oscillation between GAO and HAM from CMIP6 (only the five models with the smallest differences are shown)

From: Preliminary study on hydrological angular momentum determined from CMIP6 historical simulations

Semiannual prograde amplitude

Semiannual retrograde amplitude

Model

Difference (mas)

Model

Difference (mas)

GISS-E2-1-G_historical_r10i1p1f2

0.47

MRI-ESM2-0_historical_r2i1p1f1

0.69

BCC-CSM2-MR_historical_r3i1p1f1

0.59

MRI-ESM2-0_historical_r1i2p1f1

0.88

BCC-CSM2-MR_historical_r2i1p1f1

0.61

MRI-ESM2-0_historical_r4i1p1f1

1.06

GISS-E2-1-G_historical_r7i1p1f2

0.68

MRI-ESM2-0_historical_r5i1p1f1

1.21

BCC-CSM2-MR_historical_r1i1p1f1

0.77

MRI-ESM2-0_historical_r1i1p1f1

1.24

GRACE

1.13

GRACE

1.63

LSDM

2.08

LSDM

2.15

MEAN

1.68

MEAN

1.82

  1. The results obtained from GRACE, LSDM, and MEAN model are also shown