Fig. 4: Observed atmospheric circulation and precipitation anomalies between P2 (period 2002–2018) and P1 (period 1988–2001). | Nature Communications

Fig. 4: Observed atmospheric circulation and precipitation anomalies between P2 (period 2002–2018) and P1 (period 1988–2001).

From: Increasing tropical cyclone intensity in the western North Pacific partly driven by warming Tibetan Plateau

Fig. 4

a Difference in Climate Research Unit precipitation (mm; the plus sign is at the 0.05 level). b Latitude-height section of differences in zonal wind (m s−1; light shaded areas are at the 0.05 level) along 127.5° E. c 500–200 hPa Fh (m2 s−2; vector) and Fz (m2 s−2; shaded) of anomalous wave. All data are for July, August, and September only. a was created using Grid Analysis and Display System (GrADS) Version 2.2.1.oga.1 (https://sourceforge.net/projects/opengrads/files/grads2/2.2.1.oga.1/). b–c were created using Grid Analysis and Display System (GRADS) Version 2.0.a9.oga.1 (https://sourceforge.net/projects/opengrads/files/). Source data are provided as a Source Data file.

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