Fig. 2: Glaciochemistry and microparticle records from the NGRIP1 ice core.
From: Phasing and climate forcing potential of the Millennium Eruption of Mt. Baekdu
a Non-sea-salt sulfur (nssS) and insoluble particle (large: 4.5–9.5 μm; medium: 2.5–4.5 μm) concentrations from Continuous Flow Analysis (CFA) at the Desert Research Institute (DRI). T3 to T9 represent consecutive ice samples for tephra shard analysis, with corresponding depths shown at the bottom of the panel. b High-resolution liquid conductivity (dimensionless) analyzed at the DRI, and previously published 1-cm resolution H+ measurements based on the electrical conductivity method (ECM)63.
