Role of anthropogenic forcing in Antarctic sea ice variability simulated in climate models.

6c, e ), whereas the SLP shows weaker westerlies associated with a negative trend of the SAM (Supplementary Fig. 6d, f ).

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However, most of CMIP6 models project poleward shift and intensification of westerlies, representing a positive trend of the SAM 25 .

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In particular, Antarctic SIE deviation in the natural forcing run captures an increasing trend of the observed one after 2000 (Fig. 1a ).

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