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Progress in Earth and Planetary Science

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)

ALL

2.7 ± 0.4

0.67 ± 0.28

4.0 ± 1.1

Hokkaido

5.0 ± 0.8

0.74 ± 0.26

6.8 ± 1.3

Kyushu

3.3 ± 0.8

0.62 ± 0.26

5.3 ± 1.1

Honshu

2.0 ± 0.5

0.65 ± 0.27

3.1 ± 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
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