资源环境科技发展态势分析平台

Warming in Central Asia has been accelerating over the past three decades and is expected to intensify through the end of this century. Here we develop a summer temperature reconstruction for western Mongolia spanning eight centuries (1269-2004 C.E.) using delta blue intensity measurements from annual rings of Siberian larch. A significant cooling response is observed in the year following major volcanic events and up to 5 years post-eruption. Observed summer temperatures since the 1990s are the warmest over the past eight centuries, an observation that is also well captured in CMIP5 climate model simulations. Projections for summer temperature relative to observations suggest further warming of between ∼3-6°C by the end of the century (2075-2099 cf. 1950-2004) under the RCP4.5 and RCP8.5 emission scenarios. We conclude that projected future warming lies beyond the range of natural climate variability for the past millennium as estimated by our reconstruction.