赌博论坛

师资队伍

代表性成果:

1. Zhang, P., J.-H. Jeong, J.-H. Yoon, H. Kim, S. Y. S.  Wang, H. W. Linderholm, K. Fang, X. Wu, and D. Chen (2020). Abrupt  shift to hotter and drier climate over inner East Asia beyond the  tipping point, Science, 370(6520): 1095-1099. DOI:


2. Chen, D., P. Zhang, K. Seftigen, T. Ou, M. Giese,  and R. Barthel (2020). Hydroclimate changes over Sweden in the twentieth  and twenty-first centuries: a millennium perspective, Geografiska  Annaler: Series A, Physical Geography, DOI:


3. Linderholm, H. W., M. Nicolle, P. Francus, K. Gajewski, S. Helama, A. Korhola, O. N. Solomina, Z. Yu, P. Zhang,  W. J. D’Andrea, M. Debret, D. Divine, B. E. Gunnarson, N. J. Loader, N.  Massei, K. Seftifgen, E. K. Thomas, J. Werner, S. Andersson, A.  Berntsson, T. Luoto, L. Nevalainen, S. Saarni, and M. Väliranta (2018).  Arctic hydroclimate variability during the last 2000 years – current  understanding and research challenges, Climate of the Past, 14(4):  473-514. DOI:


4. Zhang, P., M. Ionita, G. Lohmann, D. Chen, and H. W.  Linderholm (2016). Can tree-ring density data reflect summer temperature  extremes and associated circulation patterns over Fennoscandia? Climate  Dynamics, 49: 2721-2736. DOI:


5. Zhang, P., H. W. Linderholm, B. E. Gunnarson, J.  Björklund, and D. Chen (2016). 1200 years of warm-season temperature  variability in central Scandinavia inferred from tree-ring density,  Climate of the Past, 12(6): 1297-1312. DOI:


6. Zhang, P., J. Björklund, and H. W. Linderholm (2015).  The influence of elevational differences in absolute maximum density  values on regional climate reconstructions, Trees, 29: 1259-1271, DOI:








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