Table 3 Results of the Mann–Whitney-Wilcoxon test between different CMIP projects (95% confidence level).

From: Hydrological droughts in the southern Andes (40–45°S) from an ensemble experiment using CMIP5 and CMIP6 models

Comparison

CMIP5 vs. CMIP6

Variable

Precipitation

Temperature

Streamflow

DJF

p < 0.001

p < 0.01

p < 0.001

MAM

p < 0.05

p < 0.05

p < 0.05

JJA

p < 0.1

NSC

p < 0.1

SON

NSC

NSC

NSC

Volume (m3)

 

NSC

Length (months)

p < 0.01

Events per decade

NSC

  1. The p-values indicate when there are significant differences between groups.
  2. NSC non-significant change.
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