Recent global temperature reconstructions for the current interglacial period (the Holocene,
beginning 11,700 years ago) have generated contrasting trends. This Review examines …

Abstract The Tibetan Plateau (TP) is one of the most sensitive areas to global climate
changes. Quantitative paleotemperature reconstructions on the TP since the Last …

The origin of the temperature divergence between Holocene proxy reconstructions and
model simulations remains controversial, but it possibly results from potential biases in the …

Seasonal biases (the warm-season contribution) of Holocene mean annual temperature
(MAT) reconstructions from geological records were proposed as a possible cause of the …

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 …

The Holocene, the most recent interglacial, provides an important time window for
evaluating current global warming and predicting future temperature changes. With the …

Orbital-scale global climatic changes during the late Quaternary are dominated by high-
latitude influenced~ 100,000-year global ice-age cycles and monsoon influenced~ 23,000 …

Understanding climate variability across interannual to centennial timescales is critical, as it
encompasses the natural range of climate fluctuations that early human agricultural …

Inconsistencies between Holocene climate reconstructions and numerical model
simulations question the robustness of climate models and proxy temperature records …

The patterns and mechanisms of Holocene temperature variability in China remain highly
controversial, possibly due to the lack of sufficient high-resolution records and few …