Table 3 A two-sample KS test result for the spatial extent of CDHE before and after 1976 for each homogenous region.

From: Disentangling increasing compound extremes at regional scale during Indian summer monsoon

Cluster

JUN

JUL

AUG

SEP

\({Z}_{s}\)

\({\mathrm{p}}_{\mathrm{v}}\)

\({Z}_{s}\)

\({\mathrm{p}}_{\mathrm{v}}\)

\({Z}_{s}\)

\({\mathrm{p}}_{\mathrm{v}}\)

\({Z}_{s}\)

\({\mathrm{p}}_{\mathrm{v}}\)

Western India

0

0.20

0

1.00

0

1.00

0

0.73

North-western India

0

0.91

0

1.00

1

0.00

1

0.04

North-central India

0

0.26

0

0.97

1

0.00

1

0.03

Eastern India

0

0.72

1

0.01

0

0.15

0

0.15

South-central India

0

0.30

0

0.07

0

0.09

0

0.06

South-eastern coastline

0

0.29

1

0.01

0

0.23

1

0.02

Konkan Coast

0

1.00

0

0.07

0

0.43

0

0.38

North-eastern India

0

0.08

0

0.17

0

0.08

0

0.29

Rain-belt western Himalayan

0

0.06

1

0.02

0

1.00

0

0.17

Rain-shadow western Himalayan

0

0.19

0

1.00

0

1.00

0

0.40

  1. H is the hypothesis (i.e. two samples are from the same underlying continuous population; \({\mathrm{p}}_{\mathrm{v}}\) is the p-value corresponding to H; H = 0 (1) state hypothesis is not rejected (rejected) at the 5% significance level; Bold text represent significant values greater than 95% confidence level (p-value \(\le\) 0.05, see Text S2).