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Table 7.

Mode identifications in the form (n, ℓ, m) for best and alternate configurations.

No. True seismic
σF = 0.01 σF = 0.05 σF = 0.05 σF = 0.05 σF = 0.05 σF = 0.1 σF = 0.1
# Best Alternate (2017/18) (even) (even, 2017/18) (even) (even, 2017/18)
F1 (3, 1, 0) (3, 2, 1) (2, 2, −2) (1, 3, −3) (2, 3, 1) (3, 2, 2) (3, 1, −1) (2, 3, −3) (2, 3, −3)
F2 (3, 2, −1) (4, 2, 2) (4, 3, 3) (3, 3, 3) (3, 3, 3) (3, 2, 0) (4, 2, 2) (4, 2, 2) (4, 2, 2)
F3 (3, 3, −1) (4, 3, 3) (4, 1, 1) (3, 1, −1) (3, 1, −1) (3, 3, 1) (3, 3, −1) (3, 3, −1) (3, 3, −1)
F4 (5, 1, 1) (4, 2, −1) (4, 1, −1) (3, 3, 0) (3, 3, 0) (4, 1, −1) (5, 0, 0) (4, 2, −2) (4, 2, −2)
Fc (4, 2, −2) (5, 2, 2) (5, 3, 3) (3, 3, −1) (3, 3, −1) (4, 2, 0) (5, 2, 2) (5, 2, 2) (5, 2, 2)
F5 (4, 3, −1) (5, 3, 3) (5, 2, 2) (4, 3, 3) (4, 3, 3) (4, 3, 1) (4, 3, −1) (5, 3, 3) (5, 3, 3)
F6 (5, 3, 2) (5, 1, 0) (4, 3, 0) (4, 1, −1) (4, 1, −1) (5, 0, 0) (5, 1, −1) (5, 1, −1) (5, 1, −1)
F7 (5, 2, 1) (5, 2, 1) (4, 2, −2) (3, 3, −3) (4, 3, 2) (4, 2, −2) (4, 3, −3) (4, 3, −3) (4, 3, −3)
F8 (5, 3, 1) (4, 3, −3) (4, 3, −1) (4, 2, 0) (4, 2, 0) (5, 1, 1) (5, 2, 0) (5, 2, 0) (5, 2, 0)
F9 (6, 3, 3) (5, 3, 1) (5, 3, 2) (4, 3, 1) (4, 3, 1) (4, 3, −1) (5, 3, 1) (5, 3, 1) (5, 3, 1)
F11 (6, 1, 1) (5, 2, −2) (5, 1, −1) (4, 2, −2) (4, 2, −2) (5, 1, −1) (6, 1, 1) (6, 1, 1) (6, 1, 1)
F12 (5, 3, 0) (5, 3, 0) (5, 1, 0) (5, 1, 1) (4, 3, 0) (4, 3, −3) (6, 2, 2) (6, 2, 2) (6, 2, 2)
F13 (6, 3, 1) (6, 2, 1) (5, 3, 0) (5, 1, 0) (4, 3, −2) (6, 0, 0) (5,3,−3) (6, 1, −1) (5,3,−3)
F14 (6, 2, 0) (5, 3, −3) (6, 0, 0) (4, 3, −2) (5, 1, −1) (5, 2, −2) (6,1,−1) (5, 3, −3) (6,1,−1)
F15 (6, 2, 1) (6, 2, 0) (5, 3, −1) (5, 2, 1) (5, 2, 1) (6, 1, 1) (6, 2, 0) (6, 2, 0) (6, 2, 0)

Notes. The boldfaced mode identifications in Cols. 8 and 10 correspond to modes for which the theoretical frequencies are in the inverse order compared to observations (i.e., the two modes are swapped), likely as a result of favoring normalized amplitudes over frequencies.

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