The largest discrepancy between observed and simulated trends in cold extremes is found in the Northern mid-latitudes (20 °N–45 °N), where observations indicate a coherent zonal band of decreasing trends over the recent 15 years. This might be connected to the recent hiatus in the warming of global Tmean, which has been characterized mainly as a winter phenomenon (e.g., Kosaka and Xie 2013, Cohen et al 2012). (source)Observed and simulated temperature extremes during the recent warming hiatus (archived here)
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Decadal Fluctuations in Planetary Wave Forcing Modulate Global Warming in Late Boreal Winter
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Asymmetric seasonal temperature trends (full paper pdf)
Ocean boreal winter trend
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Asymmetric seasonal temperature trends (full paper pdf)
Ocean boreal winter trend
Ocean boreal summer trend
Land boreal winter trend
Land boreal summer trend
NCDC spring wheat belt trends winter summer
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