Dipole precipitation pattern during mid-Holocene summer over the Arid central Asia driven by amplified heat source of the Tianshan Mountains. (IMAGE)

Science China Press

Dipole precipitation pattern during mid-Holocene summer over the Arid central Asia driven by amplified heat source of the Tianshan Mountains.

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High-resolution model simulated changes during mid-Holocene summer. (a) Precipitation, (b) Diabatic heating rate, (c) Moisture transport.

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