Bifurcations in a Nonlinear Dynamical Model between Western Pacific Subtropical High Ridge Line Index and Its Summer Monsoon Impact Factors

Table 1

Delay-dependent analysis of the three impact factors and SHRL index.

Number	The main member of the summer monsoon system	The correlation coefficient (time)
1	The Mascarene cold high strength index (MH)	0.91 (16 d)
2	Somali low-level jet (D)	0.90 (13 d)
3	Latent heat flux of the Indian monsoon (FLH)	0.87 (4 d)

Remark: in the time-delayed numbers, the positive means that the change of monsoon members is ahead of that of SHRL index and the negative indicates a lag.