Altitude played a highly significant role in t n trend (Fig. 3 a), which increased linearly with a slope of 0.0032 ± 0.0008 °C year −1 per 100 m and a y-intercept of 0.0418 ± 0.0057 °C year −1 (R 2 = 0.36; p-value = 0.0003).
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Enhanced spring warming in a Mediterranean mountain by atmospheric circulation.
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One low elevation station did not have a significant trend for their t n : Arphy.