Correction to: Distinct diurnal characteristics of summer precipitation and underlying mechanisms in the Tibetan Plateau and surrounding basins (Climate Dynamics, (2024), 62, 9, (9405-9425), 10.1007/s00382-024-07338-4)

In this article the graphics relating to Figs. 13 and 14 captions had been interchanged; the figure(s) should have appeared as shown below. Latitude–altitude cross sections wind vectors (arrows, normalized) and water vapor flux divergence (shaded, unit: 10^(-7) 〖kg m^(-2) s〗^(-1) hPa^(-1)) anomalies at (a) the lowest precipitation time (18–21 LST) and (b) peak precipitation time (01–04 LST), (c) and (d) are same as (a) and (b) but for water vapor transport (shaded, unit: 〖kg s〗^(-1)) and potential temperature θ (contour, unit: K) anomalies, averaged for 29–32°N where the Sichuan Basin is located (see Fig. 12a). Brown shading represents terrain. The vertical velocity is amplified by a factor of 100 Time-latitude distributions of normalized precipitation amount (PA, a) and precipitation frequency (PF, b) averaged for 29–32°N where the Sichuan Basin is located (see Fig. 12a). The black solid line is the mean elevation (right Y-axis). The diurnal cycle is repeated for clarity, and the thick solid blue line characterizes the eastward propagating signature of precipitation The original article has been corrected.