Schematic diagram of how preceding forcings influenced the climate anomalies in dust source area in 2020/21 (IMAGE)
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Negative anomalies of November-December sea ice (shading) resulted in lower SATP1 in Mongolia, while positive January-February sea ice anomalies (red contours) led to higher SATP2 in 2021. Coolest east Pacific and warmest northwest Atlantic during 2011/12–2020/21 jointly contributed to less winter precipitation in Mongolia.
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