Impact of Preceding El Niño and the Indian Ocean Dipole on the Southern China Precipitation in Early Summer
Figure 8
Area-mean precipitation anomalies over YRBS in June resulted from the effect of the input SSTA with different durations over TP and TIO regions: (a) SEXP1-PE and (b) SEXP1-PI (mm day−1). The x-axis shows the SSTA durations from September to next June (−9~6), from November to next June (−11~6), from May to June, and only in June, respectively.
