Temperature reconstruction (1750-2008) from Dahurian larch tree-rings in an area subject to permafrost in Inner Mongolia, Northeast China

27Citations
Citations of this article
21Readers
Mendeley users who have this article in their library.

Abstract

May-September temperatures were reconstructed for the past 250 yr based on Dahurian larch Larix gmelinii Rupr. growing in permafrost region of Northeast China. The reconstruction accounts for 39.3% of the actual temperature variance over the period 1958-2008. The reconstruction captured 3 relatively cold periods in 1847-1852, 1861-1866 and 1935-1941; 2 relatively warm periods in 1874-1879 and 2001-2008; and a persistent warming trend since the mid-20th century. The longterm changes in temperature documented here correspond well with regional temperature change from observational records, other global and regional proxy-based temperature reconstructions, and documented changes in regional permafrost. Thus, valuable information might be preserved in our reconstruction about local-to regional-scale climatic variation during the past 2.5 centuries. © Inter-Research 2011.

Cite

CITATION STYLE

APA

Zhang, X., He, X., Li, J., Davi, N., Chen, Z., Cui, M., … Li, N. (2011). Temperature reconstruction (1750-2008) from Dahurian larch tree-rings in an area subject to permafrost in Inner Mongolia, Northeast China. Climate Research. https://doi.org/10.3354/cr00999

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free