Research Article
Impact of the Westerly Jet on Rainfall/Runoff in the Source Region of the Yangtze River during the Flood Season
Figure 8
(a) Simultaneous correlation between IW and the zonal vertical circulation averaged over 30–37.5°N. (b) Composite anomalies of the zonal vertical circulation averaged over 30–37.5°N between the high-IW and low-IW years. The dark (light) shading in (a) indicates the correlation coefficients significant at the 99% (95%) confidence level. The shading in (b) indicates the zonal vertical circulation anomalies significant at the 95% confidence level.
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