A significant altitude amplification trend in T MIN is detected in all the high-elevation regions tested (the Tibetan Plateau, Loess Plateau, Yunnan-Guizhou Plateau, Alps, US Rocky Mountains, and Appalachian Mountains), whereas a significant or a marginally significant altitude amplification trend in T MAX is observed in four of the high-elevation regions (significant: the Yunnan-Guizhou Plateau, Alps, and Appalachian Mountains; marginally significant: the Tibetan Plateau).
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Warming Amplification of Minimum and Maximum Temperatures over High-Elevation Regions across the Globe.
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