Table 1 Trend and shift of indicated TC metric and index and when the influence of the PDO is reduced from their respective timeseries.

From: Increasing activity of tropical cyclones in East Asia during the mature boreal autumn linked to long-term climate variability

TC metrics

Period 1

Period 2

Difference (p-value)

Effect size

Sen’s slope (p-value)

Power Dissipation Index (PDI)

Original

0.16

0.22

0.06 (0.000)

−1.14

0.003 (0.009)

PDO_reduced

−0.02

0.01

0.030 (0.075)

−0.61

0.002 (0.067)

TC frequency

Percentage contribution to PDI: 56.3%

Original

3.8

5.2

1.40 (0.000)

−1.22

0.067 (0.000)

PDO_reduced

−0.20

0.18

0.39 (0.212)

−0.57

0.034 (0.075)

TC intensity

Percentage contribution to PDI: 14.1%

Original

4.27

4.35

0.08 (0.498)

−0.23

0.009 (0.013)

PDO_reduced

−0.05

0.05

0.10 (0.498)

−0.31

0.010 (0.103)

TC duration

Percentage contribution to PDI: 29.6%

Original

1.00

1.01

0.01 (0.829)

−0.08

0.000 (0.950)

PDO_reduced

0.00

0.00

0.004 (0.946)

−0.02

0.000 (0.824)

TC damages

Original

2.12

3.71

1.59 (0.048)

−0.67

0.090 (0.001)

WNP subtropical high zonal index

Original

−0.35

0.31

0.66 (0.001)

−1.03

0.030 (0.169)

East Asian subtropical jetstream index

Original

24.7

23.4

−1.35 (0.000)

−1.36

−0.056 (0.047)

  1. P-value that is less than 0.05 is shown in bold.