Impact of Preceding Summer North Atlantic Oscillation on Early Autumn Precipitation over Central China |
Figure 1 Correlation distribution between the preceding summer June-August NAOI the North Atlantic Oscillation index and a autumn September-November rainfall, b early autumn September rainfall, c wind field at 850 hPa vector and relative humidity at 700 hPa shaded, and d zonal mean vertical movement shaded and relative humidity contour over Central China 110-115”ćE for 1951-2009. The shaded areas indicate significance at the 0.1 and 0.05 levels, from light to dark. The contour interval is 0.1. |
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