Spatiotemporal Variability and Trends in Extreme Temperature Events in Finland over the Recent Decades: Influence of Northern Hemisphere Teleconnection Patterns

Figure 10

Spatial distribution maps of most influential NHTP (left) and its corresponding Spearman rank correlation (right) for cold temperature extreme indices including (a) TXn, (b) TNn, (c) FD, (d) ID, (e) TX10p, (f) TN10p, and (g) CSDI in Finland during 1961–2011. The stippling indicates areas where the correlations are statistically insignificant (p > 0.05).

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