Abstract Knowledge of the temperature variability during the last one to two millennia is
important for providing a perspective to present‐day climate excursions, for assessing the …

Tree-ring chronologies are widely used to reconstruct high-to low-frequency variations in
growing season temperatures over centuries to millennia. The relevance of these timeseries …

An annually resolved and absolutely dated ring-width chronology spanning 4,500 y has
been constructed using subfossil, archaeological, and living-tree juniper samples from the …

An “offline” approach to DA is used, where static ensemble samples are drawn from existing
CMIP climate‐model simulations to serve as the prior estimate of climate variables. We use …

Abstract The North Atlantic experiences climate variability on multidecadal scales, which is
sometimes referred to as Atlantic multidecadal variability. However, the relative contributions …

Over the past two decades, the dendroclimate community has produced various annually
resolved, warm season temperature reconstructions for the extratropical Northern …

Sparse long-term Asian monsoon (AM) records have limited our ability to understand and
accurately model low-frequency AM variability. Here we present a gridded 544-yr (from 1470 …

Although tree-ring-width-based temperature reconstructions of centennial-to-millennial
length have previously been published for many parts of the eastern Tibetan Plateau (ETP) …

There has been a gradual evolution in the way that palaeoclimate modelling and
palaeoenvironmental data are used together to understand how the Earth System works …

In contrast to a global retreating trend, glaciers in the Karakoram showed stability and/or
mass gaining during the past decades. This “Karakoram Anomaly” has been assumed to …