Fig. 6: The comparison between different records.
From: Dipolar hydroclimate pattern changes in southwest China during the last deglaciation

A Tropical Pacific zonal SST gradient59; B Lake Qinghai Westerly climate index (WI, flux of >25 μm fraction)65; C speleothem δ13C record (Yingpan Cave, this study, the red curve indicates 5-point smoothed averages); D speleothem Mg/Ca record (Yingpan Cave, this study, the pink curve indicates the 5-point smoothed averages); E Speleothem trace element records from Haozhu Cave8.