1738 years of Mongolian temperature variability inferred from a tree‐ring width chronology of Siberian pine
- 1 February 2001
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 28 (3) , 543-546
- https://doi.org/10.1029/2000gl011845
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Long-Term Temperature Trends and Tree Growth in the Taymir Region of Northern SiberiaQuaternary Research, 2000
- Seeing the Wood from the TreesScience, 1999
- Northern hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitationsGeophysical Research Letters, 1999
- Mongolian Tree Rings and 20th-Century WarmingScience, 1996
- Tree ring width and density evidence of climatic and potential forest change in AlaskaGlobal Biogeochemical Cycles, 1995
- Was there a ?medieval warm period?, and if so, where and when?Climatic Change, 1994
- A 2000-Year Tree Ring Record of Annual Temperatures in the Sierra Nevada MountainsScience, 1993
- Climatic Change in Tasmania Inferred from a 1089-Year Tree-Ring Chronology of Huon PineScience, 1991
- Frost rings in trees as records of major volcanic eruptionsNature, 1984
- The early medieval warm epoch and its sequelPalaeogeography, Palaeoclimatology, Palaeoecology, 1965