Warming Amplification of Minimum and Maximum Temperatures over High-Elevation Regions across the Globe

An analysis of the annual mean temperature (T_MEAN) (1961–2010) has revealed that warming amplification (altitudinal amplification and regional amplification) is a common feature of major high-elevation regions across the globe against the background of global warming since the mid-20th century. In this study, the authors further examine whether this holds for annual mean minimum temperature (T_MIN) and annual mean maximum temperature (T_MAX) (1961–2010) on a global scale. The extraction method of warming component of altitude, and the paired region comparison method were used in this study. Results show that a significant altitudinal amplification trend in T_MIN (T_MAX) is detected in all (four) of the six high-elevation regions tested, and the average magnitude of altitudinal amplification trend for T_MIN (T_MAX) 0.306±0.086 °C km^-1(0.154±0.213 °C km^-1)] is substantially larger (smaller) than T_MEAN (0.230±0.073 °C km^-1) during the period 1961–2010. For the five paired high- and low-elevation regions available, regional amplification is detected in the four high-elevation regions for T_MIN and T_MAX (respectively or as a whole). Qualitatively, highly (largely) consistent results are observed for T_MIN (T_MAX) compared with those for T_MEAN.