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Table 4 Differences in R1d (dR1d) and SAT (dSAT) between d1.5 and d2 with standard errors of the ensemble mean

From: Scalability of future climate changes across Japan examined with large-ensemble simulations at + 1.5 K, +2 K, and + 4 K global warming levels

 dR1d(%)dSAT(K)dR1d/dSAT(%K-1)
ALL2.7 ± 0.40.67 ± 0.284.0 ± 1.1
Hokkaido5.0 ± 0.80.74 ± 0.266.8 ± 1.3
Kyushu3.3 ± 0.80.62 ± 0.265.3 ± 1.1
Honshu2.0 ± 0.50.65 ± 0.273.1 ± 0.5
  1. The right column shows the increase rate of the R1d per 1 K (dR1d/dSAT). All land grids in the Japanese Islands are used for ALL