A Theoretical Explanation of Anomalous Atmospheric Circulation Associated with ENSO Modoki during Boreal Winter

XING Nan^1,², LI Jian-Ping^1,^*, LI Yao-Kun³

Figure 2 Distribution of ideal triple forcing sources given by Eq. 5: a ideal triple forcing sources with A 1 = -1, A 2 = 1, A 3 = -1, 2 L 1 = 4, 2 L 2 = 6, 2 L 3 = 4, d 1 = -1, d 2 = 0, d 3 = 1, l 1 = 5, l 2 = 0, and l 3 = -5; b the same as a except for reversed signs of A 1 , A 2 , and A 3 .