Fig. 1: Agreement between the 1st neutral mode (NM1) and the first empirical orthogonal function (EOF1) of East Asian summer monsoon rainfall. | Nature Communications

Fig. 1: Agreement between the 1st neutral mode (NM1) and the first empirical orthogonal function (EOF1) of East Asian summer monsoon rainfall.

From: Robust projection of East Asian summer monsoon rainfall based on dynamical modes of variability

Fig. 1

a NM1 of the global June–July–August (JJA) precipitation extracted from the precipitation linear response function (LRF) (unit is mm day−1). The green dashed contours indicate the 6 mm day−1 isoline of the JJA summer rainfall climatology. b A close-up of NM1 over East Asia to facilitate comparison with the observed EOF1 pattern of summer rainfall over the same region shown in c.

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