Fig. 7: Eulerian time evolution of atmospheric variables.
From: Enhancement of Indian summer monsoon rainfall by cross-equatorial dry intrusions
Anomalies of a temperature at 850 hPa, b specific humidity at 850 hPa, c ocean evaporation (positive anomaly indicates more evaporation), d total precipitable water, TPW, vertically integrated between the surface and 200 hPa, and e precipitation before ts and after te of DI events. The anomalies in a–c are spatially averaged within the CIO box shown in Fig. 3d. TPW and precipitation anomalies in d, e are averaged within the target region shown in Fig. 4. The left and right y-axis presents the mean absolute anomalies (bold line) and standard deviation (thin line) for the 137 events, respectively.
