Connection between Two Leading Modes of Autumn Rainfall Interannual Variability in Southeast China and Two Types of ENSO-Like SSTA

Figure 8

The difference between the positive year and negative year of dipole mode: (a), (b), (c), and (d) same as (a), (b), (c), and (d) in Figure 5. (a) 850 hPa u; & vorticity diff. (b) Moisture cliff & divergence diff. (c) u;  − 100 diff. (d) ;  − 100 diff.

(a)

(b)

(c)

(d)