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| 1 | The Sunway TaihuLight supercomputer: system and applications显示文摘The Sunway Taihu Light supercomputer is the world's first system with a peak performance greater than 100 PFlops. In this paper, we provide a detailed introduction to the Taihu Light system. In contrast with other existing heterogeneous supercomputers, which include both CPU processors and PCIe-connected many-core accelerators(NVIDIA GPU or Intel Xeon Phi), the computing power of Taihu Light is provided by a homegrown many-core SW26010 CPU that includes both the management processing elements(MPEs)and computing processing elements(CPEs) in one chip. With 260 processing elements in one CPU, a single SW26010 provides a peak performance of over three TFlops. To alleviate the memory bandwidth bottleneck in most applications, each CPE comes with a scratch pad memory, which serves as a user-controlled cache. To support the parallelization of programs on the new many-core architecture, in addition to the basic C/C++and Fortran compilers, the system provides a customized Sunway Open ACC tool that supports the Open ACC2.0 syntax. This paper also reports our preliminary efforts on developing and optimizing applications on the Taihu Light system, focusing on key application domains, such as earth system modeling, ocean surface wave modeling, atomistic simulation, and phase-field simulation. | Haohuan FU Junfeng LIAO Jinzhe YANG Lanning WANG Zhenya SONG Xiaomeng HUANG Chao YANG Wei XUE Fangfang LIU Fangli QIAO Wei ZHAO Xunqiang YIN Chaofeng HOU Chenglong ZHANG Wei GE Jian ZHANG Yangang WANG Chunbo ZHOU Guangwen YANG | 2016 | Science China(Information Sciences)2016，59，7： | 45 |
| 2 | Drift characteristics of green macroalgae in the Yellow Sea in 2008 and 2010显示文摘In order to investigate the aggregation mechanism of green macroalgae (Enteromorpha prolifera) on the Qingdao coastline,the macroalgal drift characteristics in the Yellow Sea during June and July in 2008 and 2010 were simulated using a three-dimensional wave-tide-circulation coupled model.In June 2008,the monthly-mean surface current flowed onshore and its direction was almost perpendicular to the Qingdao coastline,which was identified as the main reason for a huge accumulation of algae in the coastal waters off Qingdao.The current became parallel to the coastline in July 2008;this shift in current direction led to little accumulation of algae near Qingdao and thus relieved the environmental pressure on the Olympic sailing events.By using the coupled model,we predicted that there would be no serious algal accumulation at Qingdao in late June 2010,which was later confirmed by observations.This study demonstrated that the drift path of macroalgae near Qingdao is mainly controlled by the surface current,which is primarily driven by wind.Regional climate change is therefore one of the means by which physical processes affect marine ecosystems. | QIAO FangLi WANG GuanSuo LüXinGang DAI DeJun | 2011 | Chinese Science Bulletin2011，56，21： | 25 |
| 3 | Surface current field and seasonal variability in the Kuroshio and adjacent regions derived from satellite-tracked drifter data显示文摘The multiyear averaged surface current field and seasonal variability in the Kuroshio and adjacent regions are studied.The data used are trajectories and(1/4)° latitude by(1/4)° longitude mean currents derived from 323 Argos drifters deployed by Chinese institutions and world ocean circulation experiment from 1979 to 2003.The results show that the Kuroshio surface path adapts well to the western boundary topography and exhibits six great turnings.The branching occurs frequently near anticyclonic turnings rather than near cyclonic ones.In the Luzon Strait,the surface water intrusion into the South China Sea occurs only in fall and winter.The Kuroshio surface path east of Taiwan,China appears nearly as straight lines in summer,fall,and winter,when anticyclonic eddies coexist on its right side;while the path may cyclonically turning in spring when no eddy exists.The Kuroshio intrusion northeast of Taiwan often occurs in fall and winter,but not in summer.The running direction,width and velocity of the middle segment of the Kuroshio surface currents in the East China Sea vary seasonally.The northward intrusion of the Kuroshio surface water southwest of Kyushu occurs in spring and fall,but not in summer.The northmost position of the Kuroshio surface path southwest of Kyushu occurs in fall,but never goes beyond 31°N.The northward surface current east of the Ryukyu Islands exists only along Okinawa-Amami Islands from spring to fall.In particular,it appears as an arm of an anticyclonic eddy in fall. | HU Xiaomin XIONG Xuejun QIAO Fangli GUO Binghuo LIN Xiaopei | 2008 | Acta Oceanologica Sinica2008，27，3： | 23 |
| 4 | Predicting the spread of nuclear radiation from the damaged Fukushima Nuclear Power Plant显示文摘Japan suffered a M9.0 earthquake and massive tsunami on March 11, 2011, which seriously damaged the Fukushima Nuclear Power Plant and caused a nuclear crisis. The spread of nuclear radiation from the power plant through the atmosphere and ocean was predicted with a short-term climate forecasting model and an ocean circulation model under some idealized assumptions. If nuclear matter were leaked in the near-ground layer of 992 hPa, the climate model results show that the nuclear radiation would cover North America 10 days after the initial leakage, with the concentration at the forefront dramatically reduced to 10 millionths of the initial model concentration at the source. The radiation would span Europe in 15 days and cover much of the Northern Hemisphere in 30 days. If the initial leakage was assumed to occur in the layer 5000-m above the ground, the radiation would cover Europe in 10 days and cover much of the Northern Hemisphere in 15 days. Moreover, under the assumption that the nuclear matter leaked in the 10000-m layer, the radiation would affect much of China after 10 days. The ocean circulation model indicates that the nuclear material would be slowly transported northeast of Fukushima and reach 150°E in 50 days, and the nuclear debris in the ocean would be confined to a narrow band. Compared with the spread in the ocean, the area affected by leaked nuclear radiation in the atmosphere would be very large. Atmospheric monitors in North America and Europe will be helpful for estimating the effect in China of any leaked nuclear material. | QIAO FangLi WANG GuanSuo ZHAO Wei ZHAO JieChen DAI DeJun SONG YaJuan SONG ZhenYa | 2011 | Chinese Science Bulletin2011，56，18： | 18 |
| 5 | Influences of the surface wave-induced mixing and tidal mixing on the vertical temperature structure of the Yellow and East China Seas in summer显示文摘在影响垂直混合的物理过程的一个分类以后,扩散性由表面波浪动量和潮汐的水流导致了,它对垂直温度结构的影响被讨论。在三上基于混合计划黄和华东海(YECS ) 的垂直温度结构被模仿。结果在夏天显示出那,导致波浪的混合玩的表面处于良好的竟技状态在 YECS 的上面的混合的层的一个关键角色。潮汐的混合在底部上面在 30 m 以内控制更低的层,它是处于良好的竟技状态在南部的黄海(YS ) 的塑造站台的温度结构的主要因素。和强壮的表面导致波浪的混合,潮汐的混合让 thermocline 在南部的 YS 的东方海岸附近通气。在东方脊骨海的更深的层的双冷核心有不同原因。西方的是冬季寒冷水的维护,当东方的被循环设置时。有表面的 YECS 的模仿的垂直温度结构导致波浪的混合并且潮汐的混合有类似的特征到观察,它显示这些混合过程是在模仿沿海的海洋的 thermocline 和 pycnocline 的关键因素。 | QIAO Fangli MA Jian XIA Changshui YANG Yongzeng YUAN Yeli | 2006 | Progress in Natural Science:Materials International2006，16，7： | 14 |
| 6 | The role of surface waves in the ocean mixed layer显示文摘Previously,most ocean circulation models have overlooked the role of the surface waves.As a result,these models have produced insufficient vertical mixing,with an under-prediction of the mixing layer(ML)depth and an over-prediction of the sea surface temperature(SST),particularly during the summer season.As the ocean surface layer determines the lower boundary conditions of the atmosphere,this deficiency has severely limited the performance of the coupled ocean-atmospheric models and hence the climate studies.To overcome this shortcoming,a new parameterization for the wave effects in the ML model that will correct this systematic error of insufficient mixing.The new scheme has enabled the mixing layer to deepen,the surface excessive heating to be corrected,and an excellent agreement with observed global climatologic data.The study indicates that the surface waves are essential for ML formation,and that they are the primer drivers of the upper ocean dynamics;therefore,they are critical for climate studies. | QIAO Fangli YANG Yongzeng XIA Changshui YUAN Yeli | 2008 | Acta Oceanologica Sinica2008，27，3： | 13 |
| 7 | An improvement of the too cold tongue in the tropical Pacific with the development of an ocean-wave-atmosphere coupled numerical model显示文摘在没有流动修正的联合海洋空气将军发行量模型(CGCM ) 的申请的一个普通问题是模仿的赤道的冷舌头一般来说趋于太强壮,狭窄,并且向西延长太远。原因还很好没被理解。一个可能的原因可以是模仿的混合的层深度(MLD ) 由于在 OGCM 的不够的垂直混合在热带太平洋是太浅的。导致波浪的垂直混合罐头极大地改进 MLD 和 thermocline 结构的模拟,这被相信。在这研究,与导致波浪的混合合并的联合海洋空气将军发行量模特儿(FGCM-0 ) 被雇用了模仿热带和平的海表面温度(SST ) 。通常,因为,导致波浪的混合在 OGCM 降低 SST 加强的垂直混合能向上带更多的冷水。在联合模型,然而,在 SST 落下的空间分发的不一致产生海表面空气压力的一个水平坡度,并且因此产出表面风领域异例。风异例导致两个海洋表面发行量异例,并且在能制止的 welling 异例下面过分向西在热带太平洋的冷舌头的扩展。与从原来的模型(FGCM-0 ) 的模型结果相比,建模的 SST 由超过 0.8 ° C 是更高的,与在西方的太平洋的 1.2 ° C 的最大值(160-180 ° E, 0-3 ° N ) 。26.0 ° C 的等温线的东方边界也从 165 ° E 搬到 180 ° E。过分,向西,模仿的赤道的冷舌头的扩展与在联合模型的导致波浪的混合的加入被压制。模仿的 SST 表演一般来说与超过 1 的最大的改进改进了结果。0 ° C。在向北热带的太平洋的模仿的 SST 改进比向南热带的太平洋的好一些。 | Song Zhenya Qiao Fangli Yang Yongzeng Yuan Yeli | 2007 | Progress in Natural Science:Materials International2007，17，5： | 13 |
| 8 | Cutaneous lesions and visceral involvement of tuberous sclerosis显示文摘Background Tuberous sclerosis (TS) is an autosomal dominant disorder with a significant range of clinical expressions. The involvement of vital organs, such as the brain, kidney, heart and lung is the main cause of death in patients with TS. The aim of this study is to summarize the charateristic cutaneous features and common extracutaneous involvement of TS, which are helpful to the early detection of visceral involvement. | SUNXin-fen YANChun-lin FANGLi SHENFu-min LIAOKang-huang | 2005 | Chinese Medical Journal2005，，3： | 11 |
| 9 | The correctness to the spuriously simulated semi-annual cycle of the sea surface temperature in the equatorial eastern Pacific显示文摘One of the challenges faced by the climate model of the Community Climate System Model version 3 (CCSM3) is the spuriously simulated semi-annual cycle of the sea surface temperature (SST) in the equatorial eastern Pacific. This model bias has limited the performance of the climate simulation and prediction. Based on the surface wave-circulation coupled theory, an atmosphere-wave-ocean coupled model was developed, which incorporates the MASNUM (key laboratory of Marine Sciences and Numerical Modeling) wave number spectral model into CCSM3. The new coupled atmosphere-wave-ocean model successfully removes the spurious semi-annual cycle simulated by the original CCSM3 and reasonably produces an SST annual cycle with warm and cold phases in April and August, respectively. The correlation between the simulated and observed SST in the equatorial eastern Pacific is improved from 0.66 to 0.93. The ocean surface layer heat budget analysis indicates that the wave-induced vertical mixing is responsible for improving the simulation of the SST seasonal cycle in the equatorial eastern Pacific. | SONG ZhenYa QIAO FangLi WANG ChunZai | 2011 | Science China Earth Sciences2011，54，3： | 10 |
| 10 | The long-term prediction of the oil-contaminated water from the Sanchi collision in the East China Sea显示文摘The condensate and bunker oil leaked from the Sanchi collision would cause a persistent impact on marine ecosystems in the surrounding areas. The long-term prediction for the distribution of the oil-polluted water and the information for the most affected regions would provide valuable information for the oceanic environment protection and pollution assessment. Based on the operational forecast system developed by the First Institute of Oceanography, State Oceanic Administration, we precisely predicted the drifting path of the oil tanker Sanchi after its collision. Trajectories of virtual oil particles show that the oil leaked from the Sanchi after it sank is mainly transported to the northeastern part of the sink location, and quickly goes to the open ocean along with the Kuroshio. Risk probability analysis based on the outcomes from the operational forecast system for years 2009 to2017 shows that the most affected area is at the northeast of the sink location. | YIN Liping ZHANG Min ZHANG Yuanling QIAO Fangli | 2018 | Acta Oceanologica Sinica2018，37，3： | 9 |
| 11 | Attitudes towards pain management in hospitalized cancer patients and their influencing factors显示文摘Objective: To investigate patients' attitudes towards cancer pain management and analyze the factors influencing these attitudes.Methods: The self-developed Demographic and Disease-Related Information Questionnaires, Pain Management Barriers Questionnaire-Taiwan form(BQT), and Pain Knowledge Questionnaire were administered to 363 pairs of hospitalized cancer patients and their caregivers from the oncology departments of 7 hospitals in Beijing, China.Results: The average patient score for attitudes towards pain management was 2.96±0.49. The dimension scores indicated good attitudes in three areas(scores <2.5), 'Desire to be good'(2.22±1.04), 'Fatalism'(2.08±0.81) and'Religious fatalism'(1.86±1.00), and poor attitudes in six areas(scores ≥2.5), 'Tolerance'(3.83±0.96), 'Use of analgesics as needed(p.r.n.)'(3.73±1.01), 'Addiction'(3.44±1.05), 'Disease progression'(3.28±1.26), 'Distraction of physicians'(3.16±1.07) and 'Side effects'(2.99±0.68). Two factors were entered into the regression equation:the caregivers' attitudes towards cancer pain management and the patients' pain knowledge. These two factors explained 23.2% of the total variance in the patients' average scores for their attitudes towards cancer pain management.Conclusions: The patients' attitudes towards cancer pain management were poor and could be influenced by the caregivers' attitudes and the patients' pain knowledge, and thus need to be improved. | Fangli Lou Shaomei Shang | 2017 | Chinese Journal of Cancer Research2017，29，1： | 9 |
| 12 | Theoretical insight into the enhanced CH_4 desorption via H_2O adsorption on different rank coal surfaces显示文摘The density functional theory was used to investigate the adsorption of CH_4 and H_2O on different rank coal surfaces.The coal rank is the dominant factor in affecting the adsorption capacity of coal.In order to better understand gas and water interaction with coal of different maturity,we developed fourteen coal models to represent the different rank coal.The interactions of CH_4 and H_2O with coal surfaces were studied and characterized by their adsorption energies,Mulliken charges and electrostatic potential surfaces.The results revealed that the interaction between coal and CH_4 was weak physical adsorption,and that the interaction between coal and H_2 O consisted of physical and chemical adsorption.Adsorption energy of coal–H_2O system was larger than that of coal–CH_4 on all rank coals,suggesting that the adsorption priority in the coal models is H_2 O > CH_4.Consequently,the injection of H_2 O into the different rank coal could effectively enhance the coal bed methane(CBM) recovery. | Yanan Zhou Wenjing Sun Wei Chu Xiaoqiang Liu Fangli Jing Ying Xue | 2016 | Journal of Energy Chemistry2016，25，4： | 8 |
| 13 | Probing the sulfur content in gasoline quantitatively with terahertz time-domain spectroscopy显示文摘Terahertz time-domain spectroscopy(THz-TDS)was used for the quantitative detection of sulfur content in gasoline.Models of chemo metrics methods and partial least squares(PLS)were built to measure THz-TDS and the sulfur content.All of the samples were divided into two parts.One part was used for calibration and the other one for validation.In order to evaluate the quality of the models,the correlation coefficient(R)and root-mean-square errors(RMSE)of calibration and validation models were calculated.The value of R and RMSE were close to 1 and 0 within acceptable levels,respectively,indicating that the combination of THz-TDS and PLS is a potential method for further quantitative detection. | QIN FangLi LI Qian ZHAN HongLei JIN WuJun LIU HongLan ZHAO Kun | 2014 | Science China(Physics,Mechanics & Astronomy)2014，57，7： | 8 |
| 14 | Analytical estimation of mixing coefficient induced by surface wave-generated turbulence based on the equilibrium solution of the second-order turbulence closure model显示文摘Based on the equations of motion and the assumption that ocean turbulence is of isotropy or quasi-isotropy, we derived the closure equations of the second-order moments and the variation equations for characteristic quantities, which describe the mechanisms of advection transport and shear instability by the sum of wave-like and eddy-like motions and circulation. Given that ocean turbulence generated by wave breaking is dominant at the ocean surface, we presented the boundary conditions of the turbulence kinetic energy and its dissipation rate, which are determined by energy loss from wave breaking and entrainment depth respectively. According to the equilibrium solution of the variation equations and available data of the dissipation rate, we obtained an analytical estimation of the characteristic quantities of surface-wave-generated turbulence in the upper ocean and its related mixing coefficient. The derived kinetic dissipation rate was validated by field measurements qualitatively and quantitatively, and the mixing coefficient had fairly good consistency with previous results based on the Prandtl mixing length theory. | YUAN YeLi QIAO FangLi YIN XunQiang HAN Lei | 2013 | Science China Earth Sciences2013，56，1： | 7 |
| 15 | Evaluation on data assimilation of a global high resolution wave-tide-circulation coupled model using the tropical Pacific TAO buoy observations显示文摘In order to evaluate the assimilation results from a global high resolution ocean model, the buoy observations from tropical atmosphere ocean(TAO) during August 2014 to July 2015 are employed. The horizontal resolution of wave-tide-circulation coupled ocean model developed by The First Institute of Oceanography(FIOCOM model) is 0.1°×0.1°, and ensemble adjustment Kalman filter is used to assimilate the sea surface temperature(SST), sea level anomaly(SLA) and Argo temperature/salinity profiles. The simulation results with and without data assimilation are examined. First, the overall statistic errors of model results are analyzed. The scatter diagrams of model simulations versus observations and corresponding error probability density distribution show that the errors of all the observed variables, including the temperature, isotherm depth of 20°C(D20), salinity and two horizontal component of velocity are reduced to some extent with a maximum improvement of 54% after assimilation. Second, time-averaged variables are used to investigate the horizontal and vertical structures of the model results. Owing to the data assimilation, the biases of the time-averaged distribution are reduced more than70% for the temperature and D20 especially in the eastern Pacific. The obvious improvement of D20 which represents the upper mixed layer depth indicates that the structure of the temperature after the data assimilation becomes more close to the reality and the vertical structure of the upper ocean becomes more reasonable. At last,the physical processes of time series are compared with observations. The time evolution processes of all variables after the data assimilation are more consistent with the observations. The temperature bias and RMSE of D20 are reduced by 76% and 56% respectively with the data assimilation. More events during this period are also reproduced after the data assimilation. Under the condition of strong 2014/2016 El Ni?o, the Equatorial Undercurrent(EUC) from the TAO is gradually increased during August to November in 2014, and followed by a decreasing process. Since the improvement of the structure in the upper ocean, these events of the EUC can be clearly found in the assimilation results. In conclusion, the data assimilation in this global high resolution model has successfully reduced the model biases and improved the structures of the upper ocean, and the physical processes in reality can be well produced. | SHI Junqiang YIN Xunqiang SHU Qi XIAO Bin QIAO Fangli | 2018 | Acta Oceanologica Sinica2018，37，3： | 7 |
| 16 | A numerical study of summertime expansion pattern of Changjiang (Yangtze) River diluted water显示文摘Observations show that during summer especially in August, the northward expansion of the Changjiang(Yangtze) River diluted water (CRDW) is blocked in the vicinity of the Changjiang Estuary. To explain this phenomenon, Princeton ocean model (POM) is applied to simulate the summertime expansion pattern of CRDW. Numerical experiments show that to the north of the Changjiang Estuary, a tide-induced temperature front of a cold water centered at (34°N,122.5°E) plays the key role in determining the expansion pattern of CRDW. This front splits the CRDW into two parts: the main part expands northeastward, and the other small part expands northwestward off the coast of Jiangsu Province, China. | SHAN Feng QIAO Fangli XIA Changshui | 2009 | Acta Oceanologica Sinica2009，28，3： | 6 |
| 17 | Long baroclinic Rossby waves with periods of about 500 d near 20°N in the northwest Pacific Ocean显示文摘On the basis of maps of sea level anomalies data set from October 1992 to January 2004, pronounced low frequency variations with periods of about 500 d are detected in the area near 20°N from 160°W to 130°E. A linear two-layer model is employed to explain the mechanism. It is found that the first-mode long baroclinic Rossby waves at 20°N in the northwest Pacific propagate westward in the form of free waves at a speed of about 10.3 cm/s. This confirms that the observed low frequency variabilities appear as baroclinic Rossby waves. It further shows that these low frequency variabilities around 20°N in the northwest Pacific can potentially be predicted with a lead up to 900 d. | CHEN Haiying QIAO Fangli FANG Guohong WANG Yonggang WEI Zexun | 2006 | Acta Oceanologica Sinica2006，25，3： | 6 |
| 18 | IL-17RD (Sef or IL-17RLM) interacts with IL-17 receptor and mediates IL-17 signaling显示文摘Interleukin-17 (IL-17 或 IL-17A ) 生产是 TH17 房间的一个特点,贡献多重自体免疫、煽动性的疾病的致病的 CD4+ T 淋巴细胞的一个新唯一的系。IL-17 受体(IL-17R 或 IL-17RA ) 为 IL-17 生物活动是必要的。新兴的数据建议 heteromeric 或 homomeric 受体建筑群的形成为 IL-17 发信号被要求。这里,我们证明孤儿受体 IL-17RD (Sef,类似的表示到 FGF 基因或 IL-17RLM ) 被联系并且有 IL-17R 的 colocalized。重要地, IL-17RD 调停 IL-17 发信号,用一个酶记者评估了由 24p3 的本国的倡导者开车, IL-17 目标基因。另外,主导否定地缺乏细胞内部的领域的 IL-17RD 异种压制 IL-17R-mediated IL-17 发信号。而且,象 IL-17R 一样的 IL-17RD 与 TRAF6 被联系,一个 IL-17R 下游的分子。这些结果显示 IL-17RD 是表明建筑群的 IL-17 受体的部分,因此为通过 heteromeric 或 homomeric 受体建筑群发信号的 IL-17 提供新奇证据。 | Zhili Rong Anan Wang Zhiyong Li Yongming Ren Long Cheng Yinghua Li Yinyin Wang Fangli Ren Xiaoning Zhang Jim Hu Zhijie Chang | 2009 | Cell Research2009，19，2： | 6 |
| 19 | The prediction on the 2015/16 El Nino event from the perspective of FIO-ESM显示文摘Recently atmospheric and oceanic observations indicate the tropical Pacific is at the El Ni?o condition. However,it's not clear whether this El Ni?o event of this year is comparable to the very strong one of 1997/98 which brought huge influence on the whole world. In this study, based on the Ensemble Adjusted Kalman Filter(EAKF)assimilation scheme and First Institute of Oceanography-Earth System Model(FIO-ESM), the assimilation system is setup, which can provide reasonable initial conditions for prediction. And the hindcast results suggest the skill of El Ni?o-Southern Oscillation(ENSO) prediction is comparable to other dynamical coupled models. Then the prediction for 2015/16 El Ni?o by using FIO-ESM is started from 1 November 2015. The ensemble results indicate that the 2015/16 El Ni?o will continue to be strong. By the end of 2015, the strongest strength is very like more than 2.0°C and the ensemble mean strength is 2.34°C, which indicates 2015/16 El Ni?o event will be very strong but slightly less than that of 1997/98 El Ni?o event(2.40°C) calculated relative a climatology based on the years1992–2014. The prediction results also suggest 2015/16 El Ni?o event will be a transition to ENSO-neutral level in the early spring(FMA) 2016, and then may transfer to La Ni?a in summer 2016. | SONG Zhenya SHU Qi BAO Ying YIN Xunqiang QIAO Fangli | 2015 | Acta Oceanologica Sinica2015，34，12： | 6 |
| 20 | Energy budget of surface waves in the global ocean显示文摘Mechanical energy input from atmosphere and losses from wave-breaking dissipation of sea surface waves are estimated by a direct scheme. This scheme is based on the integration in the wavenumber space of the wind input and breaking dissipation source functions of the MASNUM wave model. The global amount of wind energy input, averaged in 2005, is about 57 TW, and the wave-breaking dissipation summed in deep-water is about 33 TW, over a half of the wind energy input. The residual may be dissipated by beach processes. Global distributions of the energy input and breaking dissipation concentrate in the westerlies of the Southern Hemisphere. | TENG Yong YANG Yongzeng QIAO Fangli LU Jing YIN Xunqiang | 2009 | Acta Oceanologica Sinica2009，28，3： | 6 |
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