We codify previously published means of calculating exposure ages and erosion rates from
10Be and 26Al concentrations in rock surfaces, and present a single complete and …

Two fundamental questions about the ice-age climate system await satisfactory resolution.
First, if summer solar radiation intensity truly controls the orbital signature of the last glacial …

Abstract Models of the production of cosmogenic nuclides typically incorporate an
adjustable production rate parameter that is scaled for variations in production with latitude …

Several models have been proposed for scaling in situ cosmogenic nuclide production rates
from the relatively few sites where they have been measured to other sites of interest. Two …

As cosmogenic nuclide applications continue to expand, the need for a common basis for
calculation becomes increasingly important. In order to accurately compare between results …

A global compilation of glacier advances and retreats for the past two millennia grouped by
17 regions (excluding Antarctica) highlights the nature of glacier fluctuations during the late …

This paper reviews the application of cosmogenic-nuclide exposure dating to glacier
chronology. Exposure dating of glacial landforms has made an outsize impact on this field …

Over the last decades, cosmogenic exposure dating has permitted major advances in many
fields of Earth surface sciences and particularly in paleoglaciology. Yet, exposure age …

Reconstructions of the Holocene geomagnetic field and how it varies on millennial
timescales are important for understanding processes in the core but may also be used to …

Knowledge of the Holocene evolution of Earth's magnetic field is important for
understanding geodynamo processes in the core, is necessary for studying long-term solar …