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For the Arctic Ocean, a 1961–1990 trend analysis of the 2‐m, 6‐hourly air temperatures from the Russian North Pole (NP) drifting ice stations shows a significant warming in May and June, or seasonally in summer. In this analysis, if we choose temperatures from only those stations which report at least 95% of the time, and define an anomaly field by removal of a mean temperature field, then for both the temperature and anomaly fields, we obtain statistically significant May and June warmings of respectively 0.8 and 0.4°C/decade, and a summer seasonal warming of 0.2°C/decade. For the other seasons, although our trends are not statistically significant, they match the trends derived for the same period from the Arctic land stations.
Martin et al. (Thu,) studied this question.
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