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Progress in Earth and Planetary Science
Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

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

Fig. 3

Scatter plots of observed vs. model simulated daily temperature and precipitation. The x and y axes indicate the AMeDAS observations and the model simulations, respectively. In order to match the elevations between the model grid and the AMeDAS, the height correction of the surface air temperature is applied to simulated temperatures using a single lapse rate of 0.0065 Km−1 (a annual mean temperature, b Tmin, c Tmax, d annual precipitation, and e R1d)

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