Stable carbon isotopes from Torneträsk, northern Sweden provide a millennial length reconstruction of summer sunshine and its relationship to Arctic circulation
Authors:
- N.J. LoaderNLN.J. Loader
- G.H.F. YoungGYG.H.F. Young
- H. GruddHGH. Grudd
- D. McCarrollDMD. McCarroll
- 1 February 2013
- journal article
- research article
- Published by Elsevier in Quaternary Science Reviews
- Vol. 62, 97-113
Abstract
No abstract availableKeywords
This publication has 95 references indexed in Scilit:
- Age trends in tree ring growth and isotopic archives: A case study ofPinus sylvestrisL. from northwestern NorwayGlobal Biogeochemical Cycles, 2011
- Cloud response to summer temperatures in Fennoscandia over the last thousand yearsGeophysical Research Letters, 2011
- A 350 year drought reconstruction from Alpine tree ring stable isotopesGlobal Biogeochemical Cycles, 2010
- Carbon isotopes and water use efficiency: sense and sensitivityOecologia, 2008
- Signal strength and climate calibration of a European tree‐ring isotope networkGeophysical Research Letters, 2007
- On the spatiotemporal characteristics of Fennoscandian tree-ring based summer temperature reconstructionsTheoretical and Applied Climatology, 2007
- The effect of temperature on the radial growth of Scots pine in northernmost FennoscandiaForest Ecology and Management, 2001
- The relation between growth cessation and frost hardening in Scots pines of different originsTrees, 2000
- Long-term c i / c a response of trees in western North America to atmospheric CO 2 concentration derived from carbon isotope chronologiesOecologia, 1998
- Little Ice Age clearly recorded in northern Greenland ice coresGeophysical Research Letters, 1998