Climate field reconstructions from networks of tree-ring proxy data can be used to
characterize regional-scale climate changes, reveal spatial anomaly patterns associated …

Based on 10Be, 36Cl and 14C records we reconstruct past changes in the geomagnetic
field intensity under the assumption that radionuclide records are mainly influenced by …

Geological archives record multiple reversals of Earth's magnetic poles, but the global
impacts of these events, if any, remain unclear. Uncertain radiocarbon calibration has limited …

Reducing the uncertainties surrounding the impacts of anthropogenic climate change
requires vetting general circulation models (GCMs) against long records of past natural …

The magnetic field of the Sun is the underlying cause of the many diverse phenomena
combined under the heading of solar activity. Here we describe the magnetic field as it …

Many palaeoclimate records from the North Atlantic region show a pattern of rapid climate
oscillations, the so-called Dansgaard–Oeschger events, with a quasi-periodicity of∼ 1,470 …

Cosmogenic radionuclides extracted from ice cores hold a unique potential for
reconstructing past solar activity changes beyond the direct instrumental period. Taking the …

Rainfall scavenges meteoric cosmogenic 10Be from the atmosphere. 10Be falls to the
Earth's surface, where it binds tightly to sediment particles in non-acidic soils over the life …

High-resolution environmental proxy data from the extratropical North Atlantic prior to the
instrumental era are of critical importance to decipher processes and mechanisms of global …

Weather and climate in the Northern Hemisphere is profoundly affected by the Arctic
Oscillation, a quasi-periodic fluctuation in atmospheric pressure that occurs on interannual …