Articles | Volume 15, issue 3
https://doi.org/10.5194/cp-15-1113-2019
https://doi.org/10.5194/cp-15-1113-2019
Research article
 | 
25 Jun 2019
Research article |  | 25 Jun 2019

Early summer hydroclimatic signals are captured well by tree-ring earlywood width in the eastern Qinling Mountains, central China

Yesi Zhao, Jiangfeng Shi, Shiyuan Shi, Xiaoqi Ma, Weijie Zhang, Bowen Wang, Xuguang Sun, Huayu Lu, and Achim Bräuning

Data sets

Asian monsoon failure and megadrought during the last millennium (https://www.ncdc.noaa.gov/paleo-search/study/10435) E. R. Cook, K. J. Anchukaitis, B. M. Buckley, R. D. D'Arrigo, G. C. Jacoby, and W. E. Wright https://doi.org/10.1126/science.1185188

The Twentieth Century Reanalysis Project (https://www.esrl.noaa.gov/psd/data/gridded/data.20thC_ReanV2c.html) G. P. Compo, J. S. Whitaker, P. D. Sardeshmukh, N. Matsui, R. J. Allan, X. Yin, B. E. Gleason, R. S. Vose, G. Rutledge, P. Bessemoulin, S. Brönnimann, M. Brunet, R. I. Crouthamel, A. N. Grant, P. Y. Groisman, P. D. Jones, M. C. Kruk, A. C. Kruger, G. J. Marshall, M. Maugeri, H. Y. Mok, Ø. Nordli, T. F. Ross, R. M. Trigo, X. L. Wang, S. D. Woodruff, and S. J. Worley https://doi.org/10.1002/qj.776

A scPDSI-based global data set of dry and wet spells for 1901–2009 (https://crudata.uea.ac.uk/cru/data/drought/) G. van der Schrier, J. Barichivich, K. Briffa, and P. Jones https://doi.org/10.1002/jgrd.50355

GPCC full data monthly product version 7.0 at 0.5°: Monthly land-surface precipitation from rain-gauges built on GTS-based and historic data (https://opendata.dwd.de/climate_environment/GPCC/html/fulldata_v7_doi_download.html) U. Schneider, A. Becker, P. Finger, A. Meyer-Christoffer, B. Rudolf, and M. Ziese https://doi.org/10.5676/DWD_GPCC/FD_M_V7_050

Updated high-resolution grids of monthly climatic observations – the CRU TS3 (https://crudata.uea.ac.uk/cru/data/hrg/cru_ts_4.01/cruts.1709081022.v4.01/tmp/) I. Harris, P. D. Jones, T. J. Osborn, and D. H. Lister https://doi.org/10.1002/joc.3711

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Short summary
We found that the tree-ring earlywood width (EWW) of Pinus tabuliformis from the eastern Qinling Mountains (central China) showed stronger response to May–July scPDSI than the tree-ring total width and latewood width. Therefore, variations in May–July scPDSI were reconstructed back to 1868 CE using the EWW chronology. The reconstruction exhibited a strong in-phase relationship with the East Asian summer monsoon intensity before the 1940s, which was different from that found in recent decades.