Fig. 3: Differences in large-scale and convective precipitation. | npj Climate and Atmospheric Science

Fig. 3: Differences in large-scale and convective precipitation.

From: Sea-ice loss in Eurasian Arctic coast intensifies heavy Meiyu-Baiu rainfall associated with Indian Ocean warming

Fig. 3

a Differences in CESM2LE-simulated precipitation anomalies [unit: mm/day] between WIO-LSI and WIO-noLSI cases in July, as well as the (b) large-scale and (c) convective components. d–e Similar to Fig. 2b, but for large-scale and convective components of the precipitation anomalies. f, g Partitions of July days occurring in WIO-LSI (blue) and WIO-noLSI cases (green) for (f) all the CESM2LE simulation days in July and (g) CESM2LE-simulated extremely heavy rainy days in July (see supplementary for the definition).

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