Analysis on the Extreme Heat Wave over China around Yangtze River Region in the Summer of 2013 and Its Main Contributing Factors
The correlation coefficient distribution between the total HDs in region A and u-component anomaly (m/s) at (a) 250 hPa, (c) 500 hPa, and (e) 700 hPa during 1979–2013 summer, and the distribution of u-component anomaly of (b) 250 hPa, (d) 500 hPa, and (f) 700 hPa in the summer of 2013. In (a, c, and e), the long-term trend is removed, and shaded area denotes the correlation coefficient significant at the 0.05 level.
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