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| 1 | A model for assessing effects of climate change on runoff in China显示文摘A model is established for assessing the effects of climate change on runoff in China based on the land surface parameterization scheme variable infiltration capacity (VIC). The entire area of China is represented by 2604 cells with a resolution of 60 km×60 km for each cell. Forcing data, soil and vegetation parameters needed by the VIC model for the entire area of China are prepared. Daily forcing data, which are obtained from 740 stations between 1980 and 1990, are interpolated to the 60 km×60 km grid system. The VIC model is run on every grid cell over the whole China, and a routing scheme is run offline with daily input of surface runoff and drainage from the VIC to get hydrograph at basin outlets. The spatial patterns of simulated runoff and mean annual precipitation are consistent very well. The results of monthly streamflow simulations over the Huaihe and Weihe River basins indicate that there is a good agreement between the observed and simulated values, and also initially indicate the rationality and feasibility of the evaluation model. | SU Fengge and XIE Zhenghui(LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China) | 2003 | Progress in Natural Science:Materials International2003，13，9： | 22 |
| 2 | The HuangZaoSi Maize Genome Provides Insights into Genomic Variation and Improvement History of Maize显示文摘Maize is a globally important crop that was a classic model plant for genetic studies. Here, we report a 2.2 Gb draft genome sequence of an elite maize line, HuangZaoSi (HZS). Hybrids bred from HZS-improved lines (HILs) are planted in more than 60% of maize fields in China. Proteome clustering of six completed sequeneed maize genomes show that 638 proteins fall into 264 HZS-specific gene families with the majority of contributions from tandem duplication events. Resequencing and comparative analysis of 40 HZSrelated lines reveals the breeding history of HILs. More than 60% of identified selective sweeps were clustered in identity.by.descent conserved regions, and yield-related genes/QTLs were enriched in HZS characteristic selected regions. Furthermore, we dem on strated that HZS-specific family genes were not uniformly distributed in the genome but enriched in improvement/function.related genomic regions. This study provides an important and novel resource for maize genome research and expands our knowledge on the breadth of genomic variation and improvement history of maize. | Chunhui Li Wei Song Yingfeng Luo Shenghan Gao Ruyang Zhang Zi Shi Xiaqing Wang Ronghuan Wang Fengge Wang Jidong Wang Yanxin Zhao Aiguo Su Shuai Wang Xin Li Meijie Luo Shuaishuai Wang Yunxia Zhang Jianrong Ge Xinyu Tan Ye Yuan Xiaochun Bi Hang He Jianbing Yan Yuandong Wang Songnian Hu Jiuran Zhao | 2019 | Molecular Plant2019，12，3： | 15 |
| 3 | DischargeRegime and Simulation for the Upstream of Major Rivers overTibetan Plateau 显示文摘 | ZHANG Leilei SU Fengge YANG Daqing | 2013 | Journal of Geophysical Research2013，118，： | 1 |
| 4 | Evaluation of TRMM multi-satellite precipitation analysis (TMPA) and its utility in hydrologic prediction in La Plata Basin显示文摘 | SU Fengge YANG Hong LETTENMAIER D P | 2008 | Journal of Hydrometeorology2008，9，： | 1 |
| 5 | Potential Utility of the Real?Time TMPA?RT Precipitation Estimates in Streamflow Prediction显示文摘 | SU Fengge GAO Huilin HUFFMAN G J | 2010 | Journal of Hydrometeorology2010，12，： | 1 |
| 6 | Applications of a Surface runoff model with Horton and Dunne runoff for VIC显示文摘 | Xie Zhenghui Su Fengge Xu Liang | | 0，，02： | 1 |
| 7 | An Application of the VIC-3L Land Surface Model with the new surfaee runoff model in simulating streamflow for the Yellow River basin显示文摘 | Xie Zhenghui Liu Qian Su Fengge | 2004 | IAHS Publiction2004，289，： | 1 |
| 8 | Applications of a surface runoff model with Horton and Dunne runoff for VIC 显示文摘 | Xie Zhenghui Su Fengge Liang Xu | 2003 | Advances in Atmosphere Science2003，20，2： | 1 |
| 9 | A 50-year sedimentary record of heavy metals and their chemical speciations in the Shuangtaizi River estuary(China):implications for pollution and biodegradation显示文摘Two parallel sediment cores collected from tidal flat located in the Shuangtaizi River estuary were analyzed for heavy metal concentrations and chemical speciations.Based on the ^(137)Cs activity profile,mean sedimentation rate at the sampling site during the past 50 years was estimated to be 1.3 cm·a^(-1).Correlation analyses show that almost all the metals are associated with each other,suggesting that these metals might be derived from same sources and/or affected by same geochemical processes.Influence of total organic carbon(TOC)content on the concentrations of Cr,Ni,Cu and Cd is evident.Silt and clay contents,instead of sand content,play an important role in the distribution of these metals.The dominant binding phases for most of the metals(except for Cd)are the residual.The relative decrease of the residual fraction of Cd and Pb in the upper 66 cm of the core is striking.The distribution of chemical fraction confirms that the residual fractions of these metals have a natural origin,while only the non-residual fractions of Cd and Pb increased upward the core due to pollution in the past five decades.Pollution assessment on these heavy metals based on Index of Geoaccumulation(I_(geo))also demonstrates that most of the metals are unpolluted.The weak pollution as observed in the sediments is perhaps related to a local plant,the Suaeda heteroptera Kitag,which may have played a significant role in the biodegradation of these metals and the metal distribution in the estuary. | Baolin LIU Ke HU Zhenglong JIANG Fengge QU Xin SU | 2011 | Frontiers of Environmental Science & Engineering2011，5，3： | 1 |
| 10 | Evaluation of TRMM Multisat- ellite Precipitation Analysis (TMPA) and its utility in hydrologic prediction in the La Plata Basin显示文摘 | Su Fengge Yang Hong Dennis P | 2008 | Journal of Hydrometeorology2008，9，4： | 1 |
| 11 | Applications of a Surface Runoff Model w ith H orton and Dunne Runoff for VIC显示文摘 | Xie Zhenghui Su Fengge Liang Xu | | 0，，02： | 1 |
| 12 | Development and validation of InDel markers for identification of QTL underlying flowering time in soybean显示文摘Soybean [Glycine max(L.) Merrill] is a major plant source of protein and oil. An accurate and well-saturated molecular linkage map is a prerequisite for forward genetic studies of gene function and for modern breeding for many useful agronomic traits. Next-generation sequence data available in public databases provides valuable information and offers new insights for rapid and efficient development of molecular markers. In this study, we attempted to show the feasibility and facility of using genomic resequencing data as raw material for identifying putative In Del markers. First, we identified 17,613 In Del sites among 56 soybean accessions and obtained 12,619 primer pairs. Second, we constructed a genetic map with a random subset of 2841 primer pairs and aligned 300 polymorphic markers with the 20 consensus linkage groups(LG). The total genetic distance was 2347.3 c M and the number of mapped markers per LG ranged from 10 to 23 with an average of 15 markers. The largest and smallest genetic distances between adjacent markers were 52.3 c M and 0.1 cM, respectively. Finally, we validated the genetic map constructed by newly developed In Del markers by QTL analysis of days to flowering(DTF) under different environments. One major QTL(qDTF4) and four minor QTL(qDTF20, qDTF13, qDTF12,and q DTF11) on 5 LGs were detected. These results demonstrate the utility of the In Del markers developed in this work for map-based cloning and molecular breeding in soybean. | Jialin Wang Lingping Kong Kanchao Yu Fengge Zhang Xinyi Shi Yanping Wang Haiyang Nan Xiaohui Zhao Sijia Lu Dong Cao Xiaoming Li Chao Fang Feifei Wang Tong Su Shichen Li Xiaohui Yuan Baohui Liu Fanjiang Kong | 2018 | The Crop Journal2018，6，2： | 1 |
| 13 | Tibetan Plateau precipitation as depicted by gauge observations, reanalyses and satellite retrievals显示文摘 | Kai Tong Fengge Su Daqing Yang Leilei Zhang Zhenchun Hao | 2014 | Int J Climatol2014，，2： | 1 |
| 14 | Contributions of moisture sources to precipitation in the major drainage basins in the Tibetan Plateau显示文摘Tracking and quantifying the moisture sources of precipitation in different drainage basins in the Tibetan Plateau(TP)help to reveal basin-scale hydrological cycle characteristics under the interactions between the westerlies and Indian summer monsoon(ISM) systems and to improve our understanding on the mechanisms of water resource changes in the ‘Asian Water Tower' under climate changes. Based on a Eulerian moisture tracking model(WAM-2) and three atmospheric reanalysis products(ERA-I, MERRA-2, and JRA-55), the contributions of moisture sources to the precipitation in six major sub-basins in the TP were tracked during an approximately 35-year period(1979/1980–2015). The results showed that in the upper Indus(UI),upper Tarim River(UT), and Qaidam Basin(QB), the moisture sources mainly extended westward along the mid-latitude westerlies to the western part of the Eurasian continent. In contrast, in the Yarlung Zangbo River Basin(YB), inner TP(ITP), and the source area of three eastern rivers(TER, including the Nujiang River, Lancang River, and Yangtze River), the moisture sources extended both westward and southward, but mainly southward along the ISM. In winter and spring, all of the sub-basins were dominated by western moisture sources. In summer, the western sources migrated northward with the zonal movement of the westerlies, and simultaneously the southern sources of the YB, ITP, and TER expanded largely toward the Indian Ocean along the ISM. In autumn, the moisture sources of the UI, UT, and QB shrank to the western sources, and the moisture sources of the YB, ITP, and TER shrank to the central-southern TP and the Indian subcontinent. By quantifying the moisture contributions from multiple sources, we found that the terrestrial moisture dominated in all of the sub-basins, particularly in the UT and QB(62–73%). The oceanic contributions were relatively high in the UI(38–42%) and YB(38–41%). In winter, evaporation from the large western water bodies(such as the Mediterranean, Red Sea, and Persian Gulf) was significantly higher than that from the continental areas. This contributed to the peak(valley) values of the oceanic(terrestrial) moisture contributions to all of the subbasins. In summer, the terrestrial moisture contributions to the UI, UT, and QB reached their annual maximum, but the abundant oceanic moisture transported by the ISM restrained the appearance of land source contribution peaks in the YB, ITP, and TER,resulting in almost equal moisture contributions in the YB from the ocean and land. | Ying LI Fengge SU Qiuhong TANG Hongkai GAO Denghua YAN Hui PENG Shangbin XIAO | 2022 | Science China Earth Sciences2022，65，6： | 0 |
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