Research Article

Impacts of Sea Surface Temperature and Atmospheric Teleconnection Patterns in the Northern Mid-Latitudes on Winter Extremely Cold Events in North China

Figure 6

Correlation coefficients between INP in summer (a), fall (b), and winter (c), IATL in winter (d) and the SSECE frequency in North China in winter. The shaded regions represent statistical significance at the 90% confidence level using Student’s t-test.
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(b)
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(d)