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

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  • Xiaohui Fan
  • Qixiang Wang
  • Mengben Wang
  • Claudia Villarroel Jiménez

Abstract

An analysis of the annual mean temperature (TMEAN) (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 (TMIN) and annual mean maximum temperature (TMAX) (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 TMIN (TMAX) is detected in all (four) of the six high-elevation regions tested, and the average magnitude of altitudinal amplification trend for TMIN (TMAX) [0.306±0.086 °C km-1(0.154±0.213 °C km-1)] is substantially larger (smaller) than TMEAN (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 TMIN and TMAX (respectively or as a whole). Qualitatively, highly (largely) consistent results are observed for TMIN (TMAX) compared with those for TMEAN.

Suggested Citation

  • Xiaohui Fan & Qixiang Wang & Mengben Wang & Claudia Villarroel Jiménez, 2015. "Warming Amplification of Minimum and Maximum Temperatures over High-Elevation Regions across the Globe," PLOS ONE, Public Library of Science, vol. 10(10), pages 1-17, October.
    • Handle: RePEc:plo:pone00:0140213
    DOI: 10.1371/journal.pone.0140213
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    References listed on IDEAS

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    1. Imtiaz Rangwala & James Miller, 2012. "Climate change in mountains: a review of elevation-dependent warming and its possible causes," Climatic Change, Springer, vol. 114(3), pages 527-547, October.
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