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| 1 | Abrupt Holocene changes of the Asian monsoon at millen-nial-and centennial-scales: Evidence from lake sediment document in Minqin Basin, NW China显示文摘Considerable research is now focusing on abrupt Holocene changes at millennial- and centennial-scales all over the world. This study shows that the changes in theHolocene summer monsoon can be divided into two main periods, based on climatic proxy records of lake sediments from the Sanjiaocheng section located at the NW boundary of the summer monsoon, Gansu Province. The early and middle Holocene was humid with stronger summer monsoon, while the late Holocene is dry with weak summer monsoon. Detailed results also show a series of millennial- and centennial-scale changes in the intensity of the summer monsoon, with a periodicity of 1600 years during the whole Holocene, and with a periodicity of 800 years during the early Holocene. Ten dry events during the Holocene are associated with the weakening of the summer monsoon. These rapid climatic changes may be representative of a global climatic change pattern during the Holocene. | CHEN Fahu ZHU Yan LI Jijun SHI Qi JIN Liya B.Wunemann | 2001 | Chinese Science Bulletin2001，46，23： | 61 |
| 2 | Spatiotemporal precipitation variations in the arid Central Asia in the context of global warming显示文摘This study analyzed the temporal precipitation variations in the arid Central Asia (ACA) and their regional differences during 1930-2009 using monthly gridded precipitation from the Climatic Research Unit (CRU). Our results showed that the annual precipitation in this westerly circulation dominated arid region is generally increasing during the past 80 years, with an apparent increasing trend (0.7 mm/10 a) in winter. The precipitation variations in ACA also differ regionally, which can be divided into five distinct subregions (I West Kazakhstan region, II East Kazakhstan region, III Central Asia Plains region, IV Kyrgyzstan region, and V Iran Plateau region). The annual precipitation falls fairly even on all seasons in the two northern subregions (regions I and II, approximately north of 45°N), whereas the annual precipitation is falling mainly on winter and spring (accounting for up to 80% of the annual total precipitation) in the three southern subregions. The annual precipitation is increasing on all subregions except the southwestern ACA (subregion V) during the past 80 years. A significant increase in precipitation appeared in subregions I and III. The long-term trends in annual precipitation in all subregions are determined mainly by trends in winter precipitation. Additionally, the precipitation in ACA has significant interannual variations. The 2-3-year cycle is identified in all subregions, while the 5-6-year cycle is also found in the three southern subregions. Besides the inter-annual variations, there were 3-4 episodic precipitation variations in all subregions, with the latest episodic change that started in the midto late 1970s. The precipitations in most of the study regions are fast increasing since the late 1970s. Overall, the responses of ACA precipitation to global warming are complicated. The variations of westerly circulation are likely the major factors that influence the precipitation variations in the study region. | CHEN FaHu HUANG Wei JIN LiYa CHEN JianHui WANG JinSong | 2011 | Science China Earth Sciences2011，54，12： | 64 |
| 3 | Relationship of Helicobacterpylori eradication with gastric cancer and gastric mucosal histological changes: a 10-year follow-up study显示文摘 | Zhou Liya Lin Sanren Ding Shigang Huang Xuebiao Jin Zhu Cui Rongli Meng Lingmei Li Yuan Zhang Li Guo Changji Xue Yan Yan Xiu'e Zhang Jing | 2014 | Chinese Medical Journal2014，，8： | 28 |
| 4 | A climatological northern boundary index for the East Asian summer monsoon and its interannual variability显示文摘A long-term perspective on the spatial variation of the northern boundary of the East Asian summer monsoon(EASM) and the related physical mechanisms is important for understanding past climate change in Asia and for predicting future changes. However, most of the meteorological definitions of the EASM northern boundary do not correspond well to the actual geographical environment, which is problematic for paleoclimatic research. Here, we use monthly CMAP and GPCP precipitation data to define a new EASM northern boundary index by using the concept of the global monsoon, which is readily applicable to paleoclimatic research. The results show that the distribution of the 2 mm day^(-1) precipitation isoline(i.e., 300 mm precipitation)has a good relationship with the spatial distribution of modern land cover types, the transitional climate zone and the potential natural vegetation types, in China. The locations of the precipitation isolines also correspond well to the locations of major shifts in wind direction. These results suggest that the 2 mm day^(-1) isoline has a clear physical significance since the climatic, ecological,and geographical boundary can be used as the northern boundary index of the EASM(which we call the climatological northern boundary index). The index depicts the northeast-southwest orientation of the climatological(1981-2010) EASM northern boundary, along the eastern part of the Qilian Mountains-southern foothills of the Helan Mountains-Daqing Mountains-western margin of the Greater Khingan Range, from west to east across Northwest and Northeast China. The interannual change of the EASM northern boundary from 1980 to 2015 covers the central part of Gansu, the northern part of Ningxia, the eastern part of Inner Mongolia and the northeastern region in China. It can extend northward to the border between China and Mongolia and retreat southward to Shangdong-central Henan. There is a 200-700 km fluctuation range of the interannual EASM northern boundaries around the locations of the climatological northern boundary. In addition, the spatial variation of the interannual EASM northern boundaries gradually increases from west to east, whereas the trend of north-south fluctuations maintains a roughly consistent location in different regions. | CHEN Jie HUANG Wei JIN LiYa CHEN JianHui CHEN ShengQian CHEN FaHu | 2018 | Science China Earth Sciences2018，61，1： | 14 |
| 5 | Paleoclimate Modeling in China: A Review显示文摘This paper provides a review of paleoclimate modeling activities in China. Rather than attempt to cover all topics, we have chosen a few climatic intervals and events judged to be particularly informative to the international community. In historical climate simulations, changes in solar radiation and volcanic activity explain most parts of reconstructions over the last millennium prior to the industrial era, while atmospheric greenhouse gas concentrations play the most important role in the20 th century warming over China. There is a considerable model–data mismatch in the annual and boreal winter temperature change over China during the mid-Holocene [6000 years before present(ka BP)], while coupled models with an interactive ocean generally perform better than atmospheric models. For the Last Glacial Maximum(21 ka BP), climate models successfully reproduce the surface cooling trend over China but fail to reproduce its magnitude, with a better performance for coupled models. At that time, reconstructed vegetation and western Pacific sea surface temperatures could have significantly affected the East Asian climate, and environmental conditions on the Qinghai–Tibetan Plateau were most likely very different to the present day. During the late Marine Isotope Stage 3(30–40 ka BP), orbital forcing and Northern Hemisphere glaciation, as well as vegetation change in China, were likely responsible for East Asian climate change. On the tectonic scale,the Qinghai–Tibetan Plateau uplift, the Tethys Sea retreat, and the South China Sea expansion played important roles in the formation of the East Asian monsoon-dominant environment pattern during the late Cenozoic. | JIANG Dabang YU Ge ZHAO Ping CHEN Xing LIU Jian LIU Xiaodong WANG Shaowu ZHANG Zhongshi YU Yongqiang LI Yuefeng JIN Liya XU Ying JU Lixia ZHOU Tianjun YAN Xiaodong | 2015 | Advances in Atmospheric Sciences2015，32，2： | 12 |
| 6 | Diagnosis and management of acquired thrombotic thrombocy- topenic purpura in southeast China: a single center experience of 60 cases显示文摘 | Xinping Zhou XingnongYe Yanling Ren Chen Mei Liya Ma Jiansong Huang Weilai Xu Juying Wei Li Ye Wenyuan Mai Wenbin Qian Haitao Meng Jie Jin Hongyan Tong | 2016 | Frontiers of Medicine2016，10，4： | 2 |
| 7 | Modulation of Beta Oscillations for Implicit Motor Timing in Primate Sensorimotor Cortex during Movement Preparation显示文摘Motor timing is an important part of sensorimotor control. Previous studies have shown that beta oscillations embody the process of temporal perception in explicit timing tasks. In contrast, studies focusing on beta oscillations in implicit timing tasks are lacking. In this study, we set up an implicit motor timing task and found a modulation pattern of beta oscillations with temporal perception during movement preparation. We trained two macaques in a repetitive visually-guided reach-to-grasp task with different holding intervals. Spikes and local field potentials were recorded from microelectrode arrays in the primary motor cortex, primary somatosensory cortex, and posterior parietal cortex. We analyzed the association between beta oscillations and temporal interval in fixedduration experiments(500 ms as the Short Group and1500 ms as the Long Group) and random-duration experiments(500 ms to 1500 ms). The results showed that the peak beta frequencies in both experiments ranged from15 Hz to 25 Hz. The beta power was higher during the hold period than the movement(reach and grasp) period.Further, in the fixed-duration experiments, the mean poweras well as the maximum rate of change of beta power in the first 300 ms were higher in the Short Group than in the Long Group when aligned with the Center Hit event. In contrast, in the random-duration experiments, the corresponding values showed no statistical differences among groups. The peak latency of beta power was shorter in the Short Group than in the Long Group in the fixed-duration experiments, while no consistent modulation pattern was found in the random-duration experiments. These results indicate that beta oscillations can modulate with temporal interval in their power mode. The synchronization period of beta power could reflect the cognitive set maintaining working memory of the temporal structure and attention. | Hongji Sun Xuan Ma Liya Tang Jiuqi Han Yuwei Zhao Xuejiao Xu Lubin Wang Peng Zhang Luyao Chen Jin Zhou Changyong Wang | 2019 | Neuroscience Bulletin2019，35，5： | 2 |
| 8 | Adenocarcinoma transformed into squamous cell carcinoma in non-small cell lung cancer显示文摘Non-small cell lung cancer(NSCLC)is the most common form of lung cancer which remains the deadliest malignancy worldwide(Siegel et al.,2019).In general,NSCLC can be divided into several subtypes,including adenocarcinoma(ADC),squamous cell carcinoma(SCC),adeno-squamous cell carcinoma(AD-SCC)and large cell carcinoma(LCC). | Yueqiang Jiang Jun Zhang Jin Feng Yaping Lu Yuan Fan Ling Cheng Xin Liao Liya Hu Shiying Yu Tiejun Yin | 2021 | Journal of Genetics and Genomics2021，48，7： | 1 |
| 9 | Genome Analyses of Single Human Oocytes显示文摘 | Yu Hou Wei Fan Liying Yan Rong Li Ying Lian Jin Huang Jinsen Li Liya Xu Fuchou Tang X. Sunney Xie Jie Qiao | 2013 | Cell2013，，7： | 1 |
| 10 | Strengthened Indian summer monsoon brought more rainfall to the western Tibetan Plateau during the early Holocene显示文摘The Tibetan Plateau(TP)is considered to be the‘‘Third Pole”of the earth because of its huge area(5 million km2),its high elevation(>4000 m average altitude),and the presence of more than 100,000 km2 of glaciers in this northern mid-latitude region.As a result of these factors,the TP influences both short-term regional and large-scale atmospheric circulation and long-term climate change[1].More than ten large rivers originate from the TP and constitute an essential water supply for nearly one sixth of the global population.Hence the TP is often referred to as‘‘the water tower of Asia”[1,2].Variations of summer rainfall over the TP greatly impact inland closed lakes,river discharge,glaciers,plant phenology,and natural hazards[2]. | Xiangjun Liu Xiaojian Zhang Yanluan Lin Liya Jin Fahu Chen | 2019 | Science Bulletin2019，64，20： | 1 |
| 11 | Local winds in a valley city显示文摘 | Hannu Savijarvi Jin Liya | 2001 | Bound- ary - Layer Meteorology2001，100，2： | 1 |
| 12 | Vegetation Index Reconstruction and Linkage with Drought for the Source Region of the Yangtze River Based on Tree-ring Data显示文摘Variations in vegetation are closely related to climate change, but understanding of their characteristics and causes remains limited. As a typical semi-humid and semi-arid cold plateau region, it is important to understand the knowledge of long term Normalized Difference Vegetation Index(NDVI) variations and find the potential causes in the source region of the Yangtze River. Based on four tree-ring width chronologies, the regional mean NDVI for July and August spanning the period 1665–2013 was reconstructed using a regression model, and it explained 43.9% of the total variance during the period 1981–2013. In decadal, the reconstructed NDVI showed eight growth stages(1754–1764, 1766–1783, 1794–1811, 1828–1838, 1843–1855, 1862–1873, 1897–1909, and 1932–1945)and four degradation stages(1679–1698, 1726–1753, 1910–1923, and 1988–2000). And based on wavelet analysis, significant cycles of2–3 yr and 3–8 yr were identified. In additional, there was a significant positive correlation between the NDVI and the Palmer Drought Severity Index(PDSI) during the past 349 yr, and they were mainly in phase. However, according to the results of correlation analysis between different grades of drought/wet and NDVI, there was significant asymmetry in extreme drought years and extreme wet years. In extreme drought years, NDVI was positively correlated with PDSI, and in extreme wet years they were negatively correlated. | LI Jinjian WANG Shu QIN Ningsheng LIU Xisheng JIN Liya | 2021 | Chinese Geographical Science2021，31，4： | 1 |
| 13 | Climate changes over eastern China during the last millennium in simulations and reconstructions显示文摘 | Youbing Peng Ying Xu Liya Jin | 2009 | Quaternary International2009，，1： | 1 |
| 14 | Rapid warming in mid-latitude central Asia for the past 100 years显示文摘 | Chen Fahu Wang Jinsong Jin Liya | 2009 | Frontiers of Earth Science in China2009，3，1： | 1 |
| 15 | Causes of early Holocene desertification in arid central Asia显示文摘 | Liya Jin Fahu Chen Carrie Morrill Bette L. Otto-Bliesner Nan Rosenbloom | 2012 | Climate Dynamics (-)2012，，7： | 1 |
| 16 | Interannual and interdecadal variations in the North Atlantic Oscillation spatial shift显示文摘The spatial shift of the North Atlantic Oscillation (NAO) is analyzed by using the Twentieth Century Reanalysis version 2 dataset and identifying NAO action centers directly on winter mean sealevel pressure (SLP) anomaly maps. The spatial shift of the NAO is characterized by four NAO spatial shift indices: the zonal and meridional shifts of the NAO southern and northern action centers. It is found that the zonal and meridional shift trends of the NAO action centers move along a path of southwest-northwest direction. Spectral analysis shows that the four NAO spatial shift indices have periodicity of 2-6 years and the NAO index has periodicity of 2-3 years in terms of high-frequency variations. On a decadal time scale, the NAO spatial shift indices are closely (positively) related to the NAO index, which is in agreement with previous studies of the relationship between the NAO index and the spatial shift of the NAO pattern. However, there is no relationship between the NAO index and the meridional shift of the northern action center on an interannual time scale. The significant relationship between the NAO index and the interannual variability of NAO spatial shift indices is very likely to be associated with synopticscale Rossby wave breaking, which generates surface pressure anomalies and thus affects the phase and pattern of the NAO. The correlations of winter westerly winds over 90°W-0° and the NAO index and the NAO spatial shift indices have a '+ - + -' structure from the Equator to the North Pole. Although there is close correlation between the NAO spatial shift indices and the strength of the zonal winds in the North Atlantic region, the effect of the zonal winds on the NAO spatial shift differs at different latitudes. Hence, the role of the zonal winds is probably a result of the NAO spatial shifts. | ZHANG XiaoJian JIN LiYa CHEN ChunZhu GUAN DongSheng LI MingZhi | 2011 | Chinese Science Bulletin2011，56，24： | 1 |
| 17 | Configuration of product extension services in servitisation using an ontology-based approach 显示文摘 | Shen Jin Wang Liya Sun Yiwen | 2012 | International Journal of Production Research2012，50，22： | 1 |
| 18 | Genome Analyses of Single Human Oocytes显示文摘 | Yu Hou Wei Fan Liying Yan Rong Li Ying Lian Jin Huang Jinsen Li Liya Xu Fuchou Tang X. Sunney Xie Jie Qiao | 2013 | Cell2013，，7： | 1 |
| 19 | Enhanced blood–brain barrier penetration and glioma therapy mediated by a new peptide modified gene delivery system显示文摘 | Hui Yao Kaiyuan Wang Yi Wang Shanshan Wang Jianfeng Li Jinning Lou Liya Ye Xueying Yan Weiyue Lu Rongqin Huang | 2014 | Biomaterials2014，，： | 1 |
| 20 | Variable selection approach for zero-inflated count data via adaptive lasso显示文摘 | Ping Zeng Yongyue Wei Yang Zhao Jin Liu Liya Liu Ruyang Zhang Jianwei Gou Shuiping Huang Feng Chen | 2014 | Journal of Applied Statistics2014，，4： | 1 |
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