From: A statistical analysis of Pc1–2 waves at a near-cusp station in Antarctica
C | A 1 | ω 1 | φ 1 | A 2 | ω 2 | φ 2 | A 3 | ω 3 | φ 3 | A 4 | ω 4 | φ 4 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Summer | |||||||||||||
a 0 | − 12.21 | 3.15 | 0.26 | 2.33 | 0.32 | 0.49 | 3.35 | 22.16 | 0.93 | 1.07 | 22.10 | 0.93 | 4.18 |
a 1 | 0.55 | 0.32 | 0.25 | − 0.63 | 10.34 | 0.94 | − 2.60 | 0.06 | 0.57 | − 2.58 | 10.33 | 0.94 | 0.53 |
a 2 | 0.18 | 0.22 | 0.27 | − 2.76 | 0.05 | 0.51 | − 2.40 | 0.04 | 3.38 | − 1.31 | 0.03 | 1.24 | − 1.35 |
Equinox | |||||||||||||
a 0 | − 13.17 | 1.59 | 0.24 | 2.46 | 0.54 | 0.60 | 0.16 | 2.52 | 0.96 | 0.13 | 2.48 | 0.99 | 2.93 |
a 1 | 0.59 | 0.17 | 0.24 | − 0.19 | 0.16 | 0.54 | − 2.64 | 2.98 | 0.99 | − 3.51 | 2.99 | 0.99 | − 0.41 |
a 2 | 0.26 | 0.26 | 0.26 | 2.86 | 0.09 | 0.53 | 2.86 | 5.20 | 1.19 | − 4.15 | 5.20 | 1.19 | − 1.02 |
Winter | |||||||||||||
a 0 | − 14.91 | 0.54 | 0.26 | 2.58 | 0.43 | 0.59 | − 0.34 | 5.21 | 0.97 | − 5.77 | 5.18 | 0.98 | 3.58 |
a 1 | 0.80 | 0.14 | 0.56 | − 3.13 | 0.08 | 0.27 | 0.03 | 0.52 | 0.92 | 0.46 | 0.51 | 0.91 | − 2.50 |
a 2 | 0.18 | 0.23 | 0.26 | 2.35 | 0.03 | 0.81 | 0.69 | 0.03 | 1.90 | 0.95 | 0.02 | 0.45 | 2.36 |