All Tables
- Table 1:
Frequencies
,
periods
,
maximum power
,
significance levels p, and latitudes
(where power exceeds the given significance level) for the labeled regions in Figs. 3a and 3b, respectively. The error
is half the frequency resolution. The time intervals (last column) were determined using the
significance contours of Morlet wavelets with nondimensional frequency 6 or 9 (cf. Sect. 2.2). A time interval in an otherwise empty row belongs to the periodicity above. Rows in brackets indicate periodicities that are evident in the wavelet power spectra (with 99.9% significance) but not in Figs. 3a and 3b. The frequencies for
and
were computed with a five times higher frequency resolution. The original values calculated with the standard frequency resolution are
(
)
and
(
).
- Table 2:
Frequencies
,
periods
,
maximum power
,
significance levels p, and latitudes
(where the power exceeds the given significance level) for the labeled regions in Figs. 5a and 5b. Asterisks indicate that the
level was also reached. The error
is half the frequency resolution. The time intervals (last column) were determined using the
significance contours of Morlet wavelets with nondimensional frequency 12 (cf. Sect. 2.2). The time interval for the peak at
in region
could not be determined unambiguously.
- Table 3:
Frequencies
,
periods
,
maximum Power
,
significance levels p, latitudes
(where the power exceeds the given significance level) and cycles (when the corresponding oscillations occurred) for the labeled regions in Figs. 7a and 7b. The error
is half the frequency resolution.
- Table 7:
Frequency estimates for r-modes (Eqs. (3) and (4)) and equatorially trapped Rossby waves (Eq. (5)), calculated with
.
- Table 4:
Frequencies
,
periods
,
maximum power
,
significance levels p, and latitudes
(where the power exceeds the given significance level) for the labeled regions in Figs. 8a-8d (cycle 21). The columns on the left give the values for the net magnetic flux, the columns on the right the values for the total magnetic flux. The error
is half the frequency resolution. The time intervals were determined using the
significance contours of Morlet wavelets with nondimensional frequency 18 (cf. Sect. 2.2).
- Table 5:
Same as Table 4 for Figs. 9a-9d (cycle 22). The error is
.
- Table 6:
Same as Table 4 for Figs. 10a-10d (cycle 23). The error is
.