Fig. 5: Anomalies forced by the warming Tibetan Plateau (TP). | Nature Communications

Fig. 5: Anomalies forced by the warming Tibetan Plateau (TP).

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

Fig. 5

a For the longitude-height section of temperature (°C) along 32.5°–37.5° N, in which light shaded areas are at the 0.05 level. b For 500–250 hPa mean temperature (°C; shaded; the black plus sign is at the 0.05 level) and 200 hPa wind (m s−1; vector; thick vectors are at the 0.05 level). c For surface air temperature (°C; shaded; the black plus sign is at the 0.05 level) and 850 hPa wind (m s−1; vector; thick vectors are at the 0.05 level). d For precipitation (mm; the black plus sign is at the 0.05 level). e For 500–200 hPa Fh (m2 s−2; vector) and Fz (m2 s−2; shaded). f For latitude-height section of zonal wind (m s−1; light shaded areas are at the 0.05 level) along 127.5° E. g For vertical wind shear (m s−1; thick vectors are at the 0.05 level) between 200 hPa and 850 hPa. All data are for July, August, and September only. This figure was 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.

Back to article page