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 …

Reproducible climate reconstructions of the Common Era (1 CE to present) are key to
placing industrial-era warming into the context of natural climatic variability. Here we present …

High-resolution late Holocene climate records that can resolve seasonality are essential for
confirming past climatic dynamics, understanding the late 20th century global warming and …

Quantitative estimates of past temperature changes are a cornerstone of paleoclimatology.
For a number of marine sediment-based proxies, the accuracy and precision of past …

Palynological analysis of surface soil and sub-surface sediments from the outwash plain of
Hamtah Glacier, Lahaul-Spiti, India, has brought out the vegetation and climatic changes in …

Systematic comparisons of proxy-based reconstructions and climate model simulations of
past millennium temperature variability offer insights into climate sensitivity and feedback …

Few reconstructions of sea-surface temperature (SST) have focused on seasonal and
interannual variability, two major components of the global climate system, due to the limited …

The elemental and isotopic compositions and abundance of carbonates in marine
sediments are used to reconstruct ancient climate and ocean conditions. These carbonates …

For the global oceans, the characteristics of high‐resolution climate changes during the last
millennium remain uncertain because of the limited availability of proxy data. This study …

Reconstructions of ocean temperatures prior to the industrial era serve to constrain natural
climate variability on decadal to centennial timescales, yet relatively few such observations …