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 …

2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …

Climate changes across the past 24,000 years provide key insights into Earth system
responses to external forcing. Climate model simulations, and proxy data,,,,–have …

The AR5 concluded that human influence on the climate system is clear, evident from
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …

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 …

Anthropogenic climate change is currently driving environmental transformation on a scale
and at a pace that exceeds historical records. This represents an undeniably serious …

古气候与现代气候变化研究如何有效结合, 特别是古气候研究如何为理解现代气候变化过程提供
背景条件, 边界约束和理论框架, 值得深入探讨. 文章以现代, 历史时期, 全新世 …

The Holocene thermal maximum, a period of global warmth evident in early to mid-Holocene
proxy reconstructions, is controversial. Most model simulations of the Holocene have not …