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| 1 | Altered trends in carbon uptake in China’s terrestrial ecosystems under the enhanced summer monsoon and warming hiatus显示文摘The carbon budgets in terrestrial ecosystems in China are strongly coupled with climate changes.Over the past decade,China has experienced dramatic climate changes characterized by enhanced summer monsoon and decelerated warming.However,the changes in the trends of terrestrial net ecosystem production(NEP)in China under climate changes are not well documented.Here,we used three ecosystem models to simulate the spatiotemporal variations in China's NEP during 1982–2010 and quantify the contribution of the strengthened summer monsoon and warming hiatus to the NEP variations in four distinct climatic regions of the country.Our results revealed a decadal-scale shift in NEP from a downtrend of–5.95 Tg C/yr^2(reduced sink)during 1982–2000 to an uptrend of 14.22 Tg C/yr^2(enhanced sink)during 2000–10.This shift was essentially induced by the strengthened summer monsoon,which stimulated carbon uptake,and the warming hiatus,which lessened the decrease in the NEP trend.Compared to the contribution of 56.3%by the climate effect,atmospheric CO2 concentration and nitrogen deposition had relatively small contributions(8.6 and 11.3%,respectively)to the shift.In conclusion,within the context of the global-warming hiatus,the strengthening of the summer monsoon is a critical climate factor that enhances carbon uptake in China due to the asymmetric response of photosynthesis and respiration.Our study not only revealed the shift in ecosystem carbon sequestration in China in recent decades,but also provides some insight for understanding ecosystem carbon dynamics in other monsoonal areas. | Honglin He Shaoqiang Wang Li Zhang Junbang Wang Xiaoli Ren Lei Zhou Shilong Piao Hao Yan Weimin Ju Fengxue Gu Shiyong Yu Yuanhe Yang Miaomiao Wang Zhongen Niu Rcmg Ge Huimin Yan Mei Huang Guoyi Zhou Yongfei Bai Zongqiang Xie Zhiyao Tang Bingfang Wu Leiming Zhang Nianpeng He Qiufeng Wang Guirui Yu | 2019 | National Science Review2019，6，3： | 24 |
| 2 | Carbon Dynamics in Woody Biomass of Forest Ecosystem in China with Forest Management Practices under Future Climate Change and Rising CO_2 Concentration显示文摘It is critical to study how different forest management practices affect forest carbon sequestration under global climate change regime.Previous researches focused on the stand-level forest carbon sequestration with rare investigation of forest carbon stocks influenced by forest management practices and climate change at regional scale.In this study,a general integrative approach was used to simulate spatial and temporal variations of woody biomass and harvested biomass of forest in China during the 21st century under different scenarios of climate and CO2 concentration changes and management tasks by coupling Integrated Terrestrial Ecosystem Carbon budget(InTEC) model with Global Forest Model(G4M).The results showed that forest management practices have more predominant effects on forest stem stocking biomass than climate and CO2 concentration change.Meanwhile,the concurrent future changes in climate and CO2 concentration will enhance the amounts of stem stocking biomass in forests of China by 12%–23% during 2001–2100 relative to that with climate change only.The task for maximizing stem stocking biomass will dramatically enhance the stem stocking biomass from 2001–2100,while the task for maximum average increment will result in an increment of stem stocking biomass before 2050 then decline.The difference of woody biomass responding to forest management tasks was owing to the current age structure of forests in China.Meanwhile,the sensitivity of long-term woody biomass to management practices for different forest types(coniferous forest,mixed forest and deciduous forest) under changing climate and CO2 concentration was also analyzed.In addition,longer rotation length under future climate change and rising CO2 concentration scenario will dramatically increase the woody biomass of China during 2001–2100.Therefore,our estimation indicated that taking the role of forest management in the carbon cycle into the consideration at regional or national level is very important to project the forest carbon sequestration under future climate change and rising atmospheric CO2 concentration. | ZHOU Lei WANG Shaoqiang Georg KINDERMANN YU Guirui HUANG Mei Robert MICKLER Florian KRAXNER SHI Hao GONG Yazhen | 2013 | Chinese Geographical Science2013，23，5： | 3 |
| 3 | Vertical distribution of soil organic carbon in China显示文摘 | Wang Shaoqiang Huang Mei Shao Xuemei | 2004 | Environmental Management2004，33，： | 1 |
| 4 | The effect of endotracheal tube cuff pressure change during gynecological laparoscopic surgery on postoperative sore throat: a control study显示文摘 | Guiqi Geng Jingyi Hu Shaoqiang Huang | 2015 | Journal of Clinical Monitoring and Computing2015，29，1： | 1 |
| 5 | Effect of dexmedetomidine combined with sufentanil for post-caesarean section intravenous analgesia: A randomised, placebo-controlled study显示文摘 | Yuyan Nie Yuqi Liu Qingyan Luo Shaoqiang Huang | 2014 | European Journal of Anaesthesiology2014，，4： | 1 |
| 6 | Acceleration of diabetic wound healing with chitosan-crosslinked collagen sponge containing recombinant human acidic fibroblast growth factor in healing-impaired STZ diabetic rats显示文摘 | Wei Wang Shaoqiang Lin Yechen Xiao Yadong Huang Yi Tan Lu Cai Xiaokun Li | 2007 | Life Sciences2007，，3： | 1 |
| 7 | 保护电子传递链完整性的小分子可以阻断线粒体凋亡途径显示文摘细胞凋亡的刺激会使得哺乳动物细胞中的线粒体释放细胞色素c和其他凋亡蛋白,导致胱天蛋白酶的激活和细胞死亡。Bcl-2蛋白家族的促凋亡成员如Bim和Bax可促进这一过程,Bim和Bax分别从线粒体启动和执行细胞色素c释放。 | Xian Jiang Li Li Zhengxin Ying Chenjie Pan Shaoqiang Huang Lin Li Miaomiao Dai Bo Yan Ming Li Hui Jiang She Chen Zhiyuan Zhang 王晓东 | 2017 | 科学新闻2017，19，4： | 0 |
| 8 | 在成纤维细胞中通过一个化学小分子诱导的类XEN状态实现直接重编程显示文摘文章简介直接谱系重编程已经成为了一种具备应用前景的制备目的细胞类型的新方法。在通过化学小分子将小鼠成纤维细胞诱导为多能干细胞形成的过程中。 | Xiang Li Defang Liu Yantao Ma Xiaomin Du Junzhan Jing Lipeng Wang Bingqing Xie Da Sun Shaoqiang Sun Xueqin Jin Xu Zhang Ting Zhao Jingyang Guan Zexuan Yi Weifeng Lai Ping Zheng Zhuo Huang Yanzhong Chang 柴真 Jun Xu 邓宏魁 | 2018 | 科学新闻2018，0，4： | 0 |
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