Fig. 9: Imposed anomalous diabatic heating and response in the LBM. | npj Climate and Atmospheric Science

Fig. 9: Imposed anomalous diabatic heating and response in the LBM.

From: A pathway for Northeast Pacific marine heatwaves to influence temperatures in western Europe during early winter

Fig. 9

a Vertical profile of imposed anomalous diabatic heating (red line) in the LBM. b Geopotential height anomalies (contour; red for positive and blue for negative; values 3, 6, 9, 12, 15, 18, and 21 plotted; unit: gpm) at 500 hPa averaged over days 16–18, as the quasi-equilibrium response to the heating. Shading indicates the imposed heating (shading; unit: K day–1) at 500 hPa.

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