Arctic amplification-induced decline in West and South Asia dust warrants stronger antidesertification toward carbon neutrality.

Particularly at the surface level, we also observe a decreasing trend of zonal wind in the main dust transport region of West and South Asia ( Fig. 3 C ), which is also coupled with the regional land-sea warming contrast.

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The decreasing dust loading in West and South Asia may be considered as a positive trend, but it still underscores the ongoing need to address dust issues in this region.

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The land-sea temperature contrast defined as surface temperature difference between the Arabian Peninsula and the Arabian Sea shows an increasing trend ( Fig. 3 D ).

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