Tree ring width and reconstructed precipitation soil water condition data series of the Northeastern Tibetan Plateau and dating data of the Delingha Area (1580B.C.-2006A.D.)
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Projection:+proj=longlat +datum=WGS84 +no_defs
Data Format: GeoTIFF, 1100rows×1800columes (0.01°×0.01°), 220 rows×360 columes (0.05°×0.05°)
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LST Valid Range:240-340
Filled Value:0
Wang, J., Shao, X. (2018). Tree ring width and reconstructed precipitation soil water condition data series of the Northeastern Tibetan Plateau and dating data of the Delingha Area (1580B.C.-2006A.D.). A Big Earth Data Platform for Three Poles, DOI: 10.11888/Ecology.tpe.9.db. CSTR: 18406.11.Ecology.tpe.9.db. (Download the reference: RIS | Bibtex )
Related Literatures:1. Shao, X.M., Wang, S.Z., Zhu, H.F., Xu, Y., Liang, E.Y., Yin, Z.Y., Xu, X.G., &Xiao, Y.M. (2009). A 3585-year ring-width dating chronology of Qilian juniper from the northeastern Qinghai-Tibetan Plateau. Iawa Journal, 30(4), 379–394.( View Details | Bibtex)
2. Yin, Z.Y., Shao, X.M., Qin, N.S., &Liang, E.Y. (2008). Reconstruction of a 1436-year soil moisture and vegetation water use history based on tree-ring widths from Qilian junipers in northeastern Qaidam Basin, northwestern China. International Journal of Climatology, 28 (1), 37-53.( View Details | Bibtex)
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To respect the intellectual property rights, protect the rights of data authors, expand services of the data center, and evaluate the application potential of data, data users should clearly indicate the source of the data and the author of the data in the research results generated by using the data (including published papers, articles, data products, and unpublished research reports, data products and other results). For re-posting (second or multiple releases) data, the author must also indicate the source of the original data. Contact: Xuemei Shao. Email:shaoxm@igsnrr.ac.cn; Affiliation:Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences. Address: No.11 Datun Road Chaoyang District, Beijing. Post Code:100101.
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