Fig. 6: The consistency of ENGPI change with TC genesis and its linear decomposition.
From: Asymmetric response of the Western North Pacific tropical cyclone genesis to symmetric CO2 pathway
a, c, e Same as Fig. 5a, c, e but with ENGPI shown as shading. g Same as Fig. 5g but for linearly reconstructed ENGPI change (Eq. 6). b, d, f, h Same as Fig. 5b, d, f, h but for contributions from (b) low-level absolute vorticity, (d) potential intensity, (f) mid-level relative humidity, and (h) vertical wind shear changes.
