此外，2 1世纪后半段北半球高纬度地区的年平均强升温幅度主要来自于冬季增温。
In addition, the simulated strong warming at northern high latitudes in the second half of the 21st century is mainly due to winter warming.
此外，2 1世纪后半段北半球高纬度地区的年平均强升温幅度主要来自于冬季增温。
In addition, the simulated strong warming at northern high latitudes in the second half of the 21st century is mainly due to winter warming.
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