过去2000年亚洲气候变化(PAGES-Asia2k)集成研究进展及展望

[1] 过去2000年中国气候变化研究的新进展 [J]. 地理学报, 2014, 69 (09) : 1248 - 1258

[2] “过去2000年全球典型暖期的形成机制及其影响研究”进展 [J]. 地理研究, 2012, 31 (04) : 769 - 769

[3] Reconstruction of temperature series of China for the last 1000 years[J]. WANG ShaoWu1,2, WEN XinYu1, LUO Yong2,3, DONG WenJie2,3, ZHAO ZongCi2,3 & YANG Bao4 1 Department of Atmospheric Sciences, School of Physics, Peking University, Beijing 100871, China;2 Laboratory for Climate Studies, China Meteorological Administration, Beijing 100081, China;3 National Climate Center, China Meteorological Administration, Beijing 100081, China;4 Laboratory for Desert and Desertification, Cold and Arid Region

[4] 历史环境变化数据库的建设与应用 [J]. 地理研究, 2002, (02) : 146 - 154

[5] 中国三千年气象记录总集[M]. 江苏教育出版社 , 蒋光美等编写, 2004

[6] Development of tree-ring width chronologies and tree-growth response to climate in the mountains surrounding the Issyk-Kul Lake, Central Asia[J] . Tongwen Zhang,Yujiang Yuan,Qing He,Wenshou Wei,Mamatkanov Diushen,Huaming Shang,Ruibo Zhang.Dendrochronologia . 2014

[7] Tree-ring reconstructed summer temperature anomalies for temperate East Asia since 800 C.E[J] . Edward R. Cook,Paul J. Krusic,Kevin J. Anchukaitis,Brendan M. Buckley,Takeshi Nakatsuka,Masaki Sano.Climate Dynamics . 2013 (11-1)

[8] Historical responses of Quercus variabilis growth to environmental changes in Southern Korea: Evidence from tree ring width and δ 13 C[J] . Jin-Hyeob Kwak,Kwang-Seung Lee,Sang-Sun Lim,Miwa Matsushima,Kye-Han Lee,Sang-Mo Lee,Woo-Jung Choi.Journal of the Korean Society for Applied Biological Chemistry . 2013 (5)

[9] Temperature changes over the past 2000 yr in China and comparison with the Northern Hemisphere[J] . Q. Ge,Z. Hao,J. Zheng,X. Shao.Climate of the Past . 2013 (3)

[10] Dendroecology in Asia [J]. TREES-STRUCTURE AND FUNCTION, 2013, 27 (02): : 341 - 342

[1] 过去2000年中国气候变化研究的新进展 [J]. 地理学报, 2014, 69 (09) : 1248 - 1258

[2] “过去2000年全球典型暖期的形成机制及其影响研究”进展 [J]. 地理研究, 2012, 31 (04) : 769 - 769

[3] Reconstruction of temperature series of China for the last 1000 years[J]. WANG ShaoWu1,2, WEN XinYu1, LUO Yong2,3, DONG WenJie2,3, ZHAO ZongCi2,3 & YANG Bao4 1 Department of Atmospheric Sciences, School of Physics, Peking University, Beijing 100871, China;2 Laboratory for Climate Studies, China Meteorological Administration, Beijing 100081, China;3 National Climate Center, China Meteorological Administration, Beijing 100081, China;4 Laboratory for Desert and Desertification, Cold and Arid Region

[4] 历史环境变化数据库的建设与应用 [J]. 地理研究, 2002, (02) : 146 - 154

[5] 中国三千年气象记录总集[M]. 江苏教育出版社 , 蒋光美等编写, 2004

[6] Development of tree-ring width chronologies and tree-growth response to climate in the mountains surrounding the Issyk-Kul Lake, Central Asia[J] . Tongwen Zhang,Yujiang Yuan,Qing He,Wenshou Wei,Mamatkanov Diushen,Huaming Shang,Ruibo Zhang.Dendrochronologia . 2014

[7] Tree-ring reconstructed summer temperature anomalies for temperate East Asia since 800 C.E[J] . Edward R. Cook,Paul J. Krusic,Kevin J. Anchukaitis,Brendan M. Buckley,Takeshi Nakatsuka,Masaki Sano.Climate Dynamics . 2013 (11-1)

[8] Historical responses of Quercus variabilis growth to environmental changes in Southern Korea: Evidence from tree ring width and δ 13 C[J] . Jin-Hyeob Kwak,Kwang-Seung Lee,Sang-Sun Lim,Miwa Matsushima,Kye-Han Lee,Sang-Mo Lee,Woo-Jung Choi.Journal of the Korean Society for Applied Biological Chemistry . 2013 (5)

[9] Temperature changes over the past 2000 yr in China and comparison with the Northern Hemisphere[J] . Q. Ge,Z. Hao,J. Zheng,X. Shao.Climate of the Past . 2013 (3)

[10] Dendroecology in Asia [J]. TREES-STRUCTURE AND FUNCTION, 2013, 27 (02): : 341 - 342