However, the Antarctic warming is rather weak with the trend of almost below 0.69 °C per decade, and even a negative trend occurs in austral winter JJA under SSP1-1.9.
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Polar amplification comparison among Earth's three poles under different socioeconomic scenarios from CMIP6 surface air temperature.
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The spring sensible heating over the Third Pole has important influence on the Asian summer monsoon, and the future outputs from CMIP6 confirms an increasing trend, and gets stronger with the increase of forcing from SSP1-2.6 to SSP5-8.5 52 .