The injection of sulfur into the stratosphere by volcanic eruptions is the dominant driver of
natural climate variability on interannual-to-multidecadal timescales. Based on a set of …

Chemical profiles from Greenland ice cores show that the frequency of volcanism was
higher during the last glacial-interglacial transition (LGIT) and early Holocene,(17–9 ka b2k) …

Major volcanic eruptions (MVEs) have attracted increasing attention from the scientific
community. Previous studies have explored the climatic impact of MVEs over the past two …

Large volcanic eruptions occurring in the last glacial period can be detected by their
accompanying sulfuric acid deposition in continuous ice cores. Here we employ continuous …

Mercury is a pollutant of global concern, especially in the Arctic, where high levels are found
in biota despite its remote location. Mercury is transported to the Arctic via atmospheric …

We synthesize research from complementary scientific fields to address the likely future
extent and duration of the proposed Anthropocene epoch. Intensification of human-forced …

While a significant influence of volcanic activity on Holocene climate is well-established, an
equally prominent role of major eruptions in the climate variability and regime shifts during …

Quantification of land surface–atmosphere fluxes of carbon dioxide (CO 2) and their trends
and uncertainties is essential for monitoring progress of the EU27+ UK bloc as it strives to …

The use of archaeological proxy records representative of population dynamics is
paramount for a richer understanding of prehistoric cultural change, but its use require a …

To assess the impact of ongoing, historically unprecedented Arctic ice melting, precisely
synchronized chronologies are indispensable for past analogs of abrupt climate change …