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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Table 3 Changes in the intensity of simulated precipitation (mm·day−1) between CTRL04 and LOW04 for each quantile of topography, and corresponding kinetic energy (m2·s−2) with their significance (p value) calculated from t test

From: Added value of high-resolution regional climate model in simulating precipitation based on the changes in kinetic energy

 

80–100%

60–80%

40–60%

20–40%

0–20%

Precipitation

0.04 (0.97)

0.86 (0.42)

0.96 (0.38)

0.45 (0.68)

1.84 (0.07)*

WMA

− 4.29 (0.24)

− 2.01 (0.56)

− 1.17 (0.71)

− 2.75 (0.30)

− 0.53 (0.76)

WMB

0.13 (0.51)

0.26 (0.14)

0.26 (0.11)

0.22 (0.33)

0.74 (0.02)*

  1. The values in bold with stars are statistical significance at 90% level