Fig. 6: Differences in geopotential height. | npj Climate and Atmospheric Science

Fig. 6: Differences in geopotential height.

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

Fig. 6

a Differences in CESM2LE-simulated 200-hPa, 500-hPa, and 850-hPa geopotential height [Z200, Z500, and Z850; unit: gpm] in July between WIO-LSI and WIO-noLSI cases. b Differences in Z200, Z500, and Z850 in July between atmosphere model (CAM6) experiments (see “Methods” section for details). The stippling represents statistical significance at the 5% level.

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