Table 2 Pattern correlation and root mean square error of precipitation simulation

From: Role of thermal and dynamical subdaily perturbations over the Tibetan Plateau in 30-day extended-range forecast of East Asian precipitation in early summer

PCC/RMSE

2022

1995

1983

 

EA

Global

EA

Global

EA

Global

ALL

0.85/2.95

0.81/1.71

0.91/3.47

0.83/1.61

0.84/2.80

0.79/1.61

NO

0.71/3.30

0.69/1.97

0.73/3.27

0.72/2.03

0.85/2.47

0.78/1.74

SST

0.57/3.39

0.74/1.89

0.68/3.34

0.72/2.15

0.86/2.32

0.79/1.61

TP_TUV

0.70/3.05

0.68/2.05

0.52/4.09

0.67/2.18

0.79/2.68

0.68/1.96

TP_TA

0.72/2.88

0.72/1.95

0.68/3.40

0.70/2.11

0.78/2.71

0.71/1.90

TP_UV

0.78/2.78

0.69/1.98

0.74/3.07

0.72/2.05

0.84/2.27

0.76/1.73

  1. The East Asia region here covers the (20°N–50°N, 105°E–140°E) range, and the global region covers the (90°S–90°N, 0–360°E) range.
Back to article page