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| 1 | Study on wavy distribution of rainfall associated with typhoon Matsa (2005)显示文摘An analysis is made to investigate the structure features of the extensive heavy rainfall left by typhoon Matsa, after its landfall in China's Mainland in August 2005, based on a range of observational results, including surface intensive observation data, TBB data from China's FY-2 satellite, and NCEP 1°×1° reanalysis data. The study tries to explore the interaction between atmospheric waves, 3-D atmospheric structures, and typhoon rainbands. Observational facts, diagnostic analysis, and atmospheric wave theory are used to look into the formation mechanism of distant typhoon rainbands. Results show that (1) Matsa rainbands have the features of noticeable wave train distribution and long distance propaga-tion; (2) the typhoon rainbands extend as far as 2000 km northwardly from the typhoon center, with a wavelength of 500―1000 km and a wave period of 12―24 h; (3) the wave structure of Matsa rainbands is closely associated with the corresponding wave variation of the ambient 3-D atmospheric structures, including disturbance vorticity, divergence field, vertical motion field, water vapor flux divergence field, etc. (4) both observational facts and theoretical analysis show that the northward extending typhoon rainbands are associated with the mixed effects of atmospheric inertia wave and internal gravity wave; (5) only under proper atmospheric stratification and vertical wavenumber of gravity wave, can a ty-phoon stimulate such a wave being able to reach such a distance, and result in extending wavy rain-bands. | LI Ying WANG JiZhi CHEN LianShou YANG YuanQin | 2007 | Chinese Science Bulletin2007,52,7: | 10 |
| 2 | Impact assessment of landfalling tropical cyclones:introduction to the special issue显示文摘1 Introduction Tropical cyclones(TCs)are one of the most destructive natural phenomena in the world.The accompanied damaging winds,heavy precipitation,and storm surges have caused great economic losses and life casualties to human beings.There are eight disaster events related to TC among the top tenwhich caused the highest amount of insurance losses in the world. | Hui YU Lianshou CHEN | 2019 | Frontiers of Earth Science2019,13,4: | 9 |
| 3 | ADVANCES IN UNDERSTANDING AND FORECASTING RAPIDLY CHANGING PHENOMENA IN TROPICAL CYCLONES显示文摘This review of new understanding and forecasting of tropical cyclones(TCs) is based on presentations at the International Top-level Forum on Rapid Change Phenomena in Tropical Cyclones in Haikou, China. The major topics are the sudden changes in tracks, rapid changes in structure and intensity, rapid changes in rainfall, and advances in forecasting and forecaster requirements. Although improved track forecast guidance has been achieved with the Australian ACCESS-TC model and in track forecasts to 120 h by the China Meteorological Administration, there is a continuing need for better understanding and improved track forecast guidance. Advances in understanding of processes related to rapid intensification(RI), secondary eyewall formation, mechanisms controlling inner-core structure and size changes, and structure and intensity changes at landfall have been achieved, but progress in prediction of rapid changes in structure and intensity has been slow. Taking into account complex interactions involved in TC-related rainfall, a prioritized list of physical processes that govern rainfall from landfalling TCs in China has been developed. While forecaster participants were generally encouraged by the progress being made, they expressed a strong desire for a transition of that new knowledge to timely and reliable forecast guidance products. | RUSSELL L.ELSBERRy LIANSHOU CHEN JIM DAVIDSON ROBERT ROGERS YUQING WANG LIGUANG WU | 2013 | Tropical Cyclone Research and Review2013,2,1: | 7 |
| 4 | Science and prediction of monsoon heavy rainfall显示文摘With the increasing incidence of heavy rainfall events,particularly over the monsoon regions,the highly dense populations are more vulnerable[1].Research initiatives on observation,modeling,and prediction of monsoon heavy rainfall have been promoted actively by World Weather Research Programme's(WWRP)Working Group on Tropical Meteorology Research(WGTMR)of the World Meteorological Organization(WMO)since 2010.Series of monsoon-heavy-rainfall workshops were held in Beijing(2011),Petaling Jaya(2012),and New Delhi(2015)to benefit scientists worldwide and forecasters from the National Meteorological and Hydrological Services.An international Research and Development Project,namely,the Southern China Monsoon Rainfall Experiment(SCMREX)[2]was established in 2013 to coordinate field campaign experiments and to conduct scientific research on presummer(April-June)heavy rainfall processes in southern China. | Yali Luo Liye Li Richard HJohnson Chih-Pei Chang Lianshou Chen Wai-Kin Wong Jing Chen Kalli Furtado John LMcBride Ajit Tyagi Nanette Lomarda Thierry Lefort Esperanza O.Cayanan | 2019 | Science Bulletin2019,64,21: | 4 |
| 5 | Characteristics of Near Surface Winds over Different Underlying Surfaces in China: Implications for Wind Power Development显示文摘Accurate wind and turbulence information are essential to wind energy research and utilization, among which wind shear and turbulence intensity/scale have seldom been investigated. In this paper, the observational data from the100-m high wind towers in Xilinhot in Inner Mongolia(2009–10; grassland region), Huanghua in Hebei Province(2009–10; coastal flat region), and Xingzi County in Jiangxi Province(2010–11; mountain–lake region) are used to study the variations in near surface winds and turbulence characteristics related to the development of local wind energy over different underlying surfaces. The results indicate that(1) the percentage of the observed wind shear exponents exceeding 0.3 for the grassland region is 6%, while the percentage is 13% for the coastal flat region and 10%for the mountain–lake region. In other words, if the wind speed at 10 m is 10 ms^(–1), the percentage of the wind speed at 100 m exceeding 20 ms^(–1) for the grassland region is 6%, while the percentage is 13% for the coastal flat region and 10% for the mountain–lake region.(2) In terms of the turbulent intensity in the zonal, meridional, and vertical directions(I_u, I_v, and I_w, respectively), the frequencies of I_v/I_u < 0.8 in the grassland, coastal flat, and mountain–lake regions are 23%–29%, 32%–38%, and 30%–37%, respectively. Additionally, the frequencies of I_w/I_u < 0.5 in the grassland, coastal flat, and mountain–lake regions are 45%–75%, 52%–70%, and 43%–53%, respectively. The frequencies of I_v/I_u < 0.8 and Iw/I_u < 0.5 in each region mean that I_u is large and the air flow is unstable and fluctuating,which will damage the wind turbines. Therefore, these conditions do not meet the wind turbine design requirements,which must be considered separately.(3) At 50-and 70-m heights, the value of the turbulence scale parameter Λ in the grassland region is greater than that in the coastal flat region, and the latter is greater than that in the mountain–lake region. Therefore, under the same conditions, some parameters, e.g., the extreme directional change and extreme operating gust at the hub height in the grassland region, are greater than those in the coastal flat region,which are greater than those in the mountain–lake region. These results provide a reference for harnessing local wind energy resources and for the selection and design of wind turbines. | Xi GONG Rong ZHU Lianshou CHEN | 2019 | Journal of Meteorological Research2019,33,2: | 3 |
| 6 | A Monte Carlo study of the quark-and gluon-jets of difierent hardness in three-jet events identied by b-tag method显示文摘 | Chen Gang Liu Lianshou | 2004 | J Phys G:Nucl Part Phys2004,30,: | 1 |
| 7 | Rainfall rein forcement associated with landfalling tropical cyclones显示文摘 | Dong Meiying Chen lianshou Li Ying | 2010 | J Atmos Sci2010,67,11: | 1 |
| 8 | A Monte Carlo study on the Identication of quark and gluon Jets显示文摘 | Yu Meiling Liu Lianshou | 2002 | Chin Phys Lett2002,19,: | 1 |
| 9 | Intermittency in Cascade model显示文摘 | WU Yuanfang ZHANG Kunshi LIU Lianshou | 1991 | Chinese Science Bulletin1991,21,1: | 1 |
| 10 | A numerical study on the formation and development of its land induced cy clone and its impact on typhoon structure change and motion 显示文摘 | Meng Zhiyong Nagata Masashi Chen Lianshou | 1996 | Acta Meteor Sin1996,10,4: | 1 |
| 11 | Multiplicity and energy distributions in high-energy, e^+ e^- , pp, and p p collisions 显示文摘 | Liu Lianshou Meng Tachung | 1983 | Phys Rev1983,27,: | 1 |
| 12 | Koba-Nielsen-Olesen scaling and production mechanism in high-energy collisions 显示文摘 | Chou Kuangchao Liu Lianshou Meng Tachung | 1983 | Phys Rev1983,28,: | 1 |
| 13 | Interaction between Tropical Cyclone and Meiyu Front显示文摘 | Cheng Zhaohui Kang Di Chen Lianshou Xu Xiangde | 1998 | Acta Meteerologica Sinica1998,13,1: | 1 |
| 14 | The impact of Middle Troposphere Circulation Pattern over Tibetan Plateau on the Track of Typhoon over Western Pacific显示文摘 | Xu Jing Cben Lianshou Xu Xiangde | 2000 | Acta Meteorologica Sinica2000,14,3: | 1 |
| 15 | In there anomalous scaling in multiparticle final states of high energy collision? 显示文摘 | Wu Yuanfang Zhang Yang0 Liu Lianshou | 1995 | Phys Rev1995,51,: | 1 |
| 16 | On the influence of momentum conservation upon the scaling behaviour of factorial moments in high energy multiparticle production显示文摘 | Liu Lianshou Zhang Yang Deng Yue | 1997 | Z Phys1997,73,: | 1 |
| 17 | Monte Carlo study of the Dynamical fluctuation property of the hadronic system显示文摘 | Liu Lianshou Chen Gang Fu Jinghua | 2001 | Phys Rev2001,63,05: | 1 |
| 18 | A Nu- merical Study on the Formation and Development of Is Land -Induced Cyclone and Its Impact on Typhoon structure change and motion ACTA显示文摘 | Meng Zhiyong Nagata Masashi and Chen Lianshou | 1996 | Meteorological Siniea1996,10,4: | 1 |
| 19 | Interaction of typhoon and mesoscale vortex 显示文摘 | Chen Lianshou Luo Zhexian | 2004 | Adv Atmos Sci2004,21,4: | 1 |
| 20 | Recent progress on tropical cyclone research in China显示文摘 | Meng Zhiyong Chen Lianshou Xu Xiangde | 2002 | Adv Almos Sci2002,19,1: | 1 |