Fig. 10: LBM experiment in accordance with the WPSST.

The a 200 hPa, b 300 hPa, c 400 hPa, d 500 hPa, e 850 hPa, and f 1000 hPa geopotential height anomalies derived from LBM with the boreal summer background conditions and the thermal forcing sources localised as the positive WPSST pattern.