Impact of Preceding El Niño and the Indian Ocean Dipole on the Southern China Precipitation in Early Summer
Figure 2
Temporal variation of normalized boreal autumn NINO3 (solid line) and IODI (dashed line) from 1951 to 2000 (a) and the temporal variation of composite monthly mean NINO3 (solid line) and IODI (dashed line) for co-occurring event years (1963, 1972, 1982, 1987, and 1997) (b).
