NUMERICAL SIMULATION OF EXTREMELY HEAVY RAIN AND MESO-β SCALE LOW VORTEX IN INVERTED TYPHOON TROUGH

Large-scale and mesoscale analyses are made for extremely heavy rain (EHR) and meso-β scale low vortex (MSLV) in Jiading District of Shanghai Municipality during 6-7 July 2001.It is shown that the EHR forms in the situation of northern westerly trough linking together with southern inverted typhoon trough at northwest side of the West Pacific Ocean subtropical high. Numerical simulation is made using a 21-layer improved REM (regional η coordinate model) for this course.The results show that the precipitation forms earlier than MSLV.and the strong convergence in wind velocity mate (WVM) triggers the strong precipitation.The formative reasons of WVM.especially the weak wind velocity center are discussed,and the formative mechanisms of the MSLV and EHR are discussed using high spatial and temporal resolution model- output physical fields.The results show that the heavy rain releases latent heat and warms the air column,and enhances the low level positive vorticity that existed before.Then it causes the formation of MSLV.There is a positive feedback mechanism between low vortex and precipitation,so CISK must be an important mechanism.

Research on the dry intrusion accompanying the low vortex precipitation

By employing the 6.7μm satellite vapor cloud images and NCEP/NCAR 1°×1° reanalysis datasets, the characteristics and mechanism of the dry intrusion, as well as its impacts on the low vortex precipita- tion at the Meiyu front are explored in this paper. It is found that the formation,development and main- tenance of the low vortex precipitation at the Meiyu front are closely related to the evolution of the dry intrusion. The dry intrusion is characterized by high potential vorticity (PV), low humidity and cold air. The dry intrusion exhibits as an obvious dark zone on vapor cloud images, an area in which atmos- pheric relative humidity is lower than 60%. However, the features of the dry intrusion on the vapor im- ages are clearer than that of the humidity field, for the former is the digital vapor cloud images with high temporal and spatial resolution, and it can be used to explore the finer characteristics of the develop- ment, evolution and supplement of the intrusion during the development of the low vortex. The dry intrusion impacts accompanying the low vortex precipitation at the Meiyu front come from all levels of the troposphere, with the strongest intrusion located at the upper troposphere. The dry and cold air intrudes the vicinity of the low vortex from the upper isentropic surface to the lower one, slanting eastward from lower to higher level. The low vortex precipitation region is usually situated in front of the dry intrusion where the relative humidity gradient is higher. The research also reveals that the mechanism of the dry intrusion is that the high potential vorticity descends from the upper troposphere to the lower level, therefore, the dry intrusion can be used as an important index of the high PV forcing. To the west of the low vortex precipitation, the upper level northerlies descend across the isentropic surface, then the dry cold advection can trigger the instable development in the mid-low troposphere. The dry intrusion enhances the low vortex precipitation. Meanwhile, because of the good agreement between the high PV at the upper level and the dry intrusion illustrated by the vapor cloud images, the dry intrusion in the vapor cloud images is the direct and clear description of the high PV forcing which provides a new insight in understanding the evolution and development of the practical weather sys- tems. Besides, both the skills of isentropic analysis and potential temperature coordinates system analysis are important to revealing the three-dimension structure of the dry intrusion.

Low-Frequency Vortex Pair over the Tropical Eastern Indian Ocean and the South China Sea Summer Monsoon Onset

In this paper,the relationship between a pair of low-frequency vortexes over the equatorial Indian Ocean and the South China Sea(SCS) summer monsoon onset is studied based on a multi-year(1980-2003) analysis.A pair of vortexes symmetric about the equator is an important feature prior to the SCS summer monsoon onset.A composite analysis shows that the life cycle of the pair of vortexes is closely associated with the SCS summer monsoon onset.The westerly between the twin cyclones is an important factor to the SCS summer monsoon onset process.

Study of vortex in flow fields induced by surface dielectric barrier discharge actuator at low pressure based on Q criterion

Flow fields induced by a surface dielectric barrier discharge actuator at low pressure of 7 kPa are measured by particle image velocimetry. The distribution of local vortices in the flow field is revealed by the Q criterion. The reason for the generation of vortices is analyzed and the influence of pulse frequency and duty cycle on vortices is studied. The results show that the Q criterion can reveal the small-scale vortices, which cannot be indicated by the streamline. The direction transition zone where the induced jet moves from the vertical to the tangential and the shear layer between the jet and stationary air are prone to the generation of strong vortices. The influence of pulse frequency on vortices is not obvious, but the variation of duty cycle can significantly affect the strength and distribution of vortices.

Design and Numerical Simulation of Low-Fiber Hollow Spindle in Air-Jet Vortex Spinning

Based on the mechanical system of free-end fibers and the analysis of pulling free-end fibers out of the spun yarn during spinning,a low-fiber hollow spindle is designed and the air distribution of fluent field is simulated numerically. The negative pressure effect is much bigger at the top of low-fiber hollow spindle than that in Murata No.861,which is more conducive for single fiber to get into the channel of hollow spindle. The tangential velocity in 0-3 mm at the top of hollow spindle increases and the fluctuation of radial velocity is much stronger,which enhance the wrapping effect. In the addition,the distribution of axial velocity remains the same.

The Impact of Deformation on Vortex Development in a Baroclinic Moist Atmosphere

A mathematical relation between deformation and vertical vorticity tendency is built by introducing the frontogenesis function and the complete vertical vorticity equation, which is derived by virtue of moist potential vorticity. From the mathematical relation, it is shown that properly configured atmospheric conditions can make deformation exert a positive contribution to vortex development at rates comparable to other favorable factors. The effect of deformation on vortex development is not only related to the deformation itself, but also depends on the current thermodynamic and dynamic structures of the atmosphere, such as the convective stability, moist baroclinicity and vertical wind shear （or horizontal vorticity）. A diagnostic study of a heavy-rainfall case that occurred during 20-22 July 2012 shows that deformation has the most remarkable effect on the increase in vertical vorticity during the rapid development stage of the low vortex during its whole life cycle. This feature is mainly due to the existence of an approximate neutral layer （about 700 hPa） in the atmosphere where the convective stability tends to be zero. The neutral layer makes the effect of deformation on the vertical vorticity increase significantly during the vortex development stage, and thus drives the vertical vorticity to increase.

动力电池测试用高低温试验箱温度场分析与流场模拟优化

以试验区置有两个动力电池的294 L高低温试验箱作为研究对象,通过CFD模拟了高低温试验箱恒温45℃时箱内电池的温升和散热情况,并对高低温试验箱的流场进行优化。结果表明:对于同侧上送风下回风的气流组织形式,在试验区上部放置多孔板进行孔板送风有助于提高流场均匀性;两个动力电池之间会出现涡旋现象,通过增加置物架与内箱底部的间距、适当增大回风口截面积均能减轻甚至消除涡旋现象,提高流场均匀性,当置物架与内箱底部的间距增至0.2 m,回风截面的高度增至0.15 m后,试验箱流场的整体不均匀度由1.73降至0.4,电池间的涡旋现象消失。

清远一次极端龙舟水的中尺度系统演变分析

利用多源观测数据和ERA5再分析资料,对2022年6月20到21日发生在清远的一次极端特大暴雨过程进行分析。结果表明:(1)该次强降水是在200 hPa分流辐散的背景下,由低涡切变配合其前侧西南急流缓慢东移经过清远造成的。(2)强降水发生前大气层结已处于极不稳定状态,低层来自孟加拉湾和南海的水汽不断在清远市上空辐合,为暴雨的发生提供充足的水汽条件和不稳定能量。(3)强降水的触发机制主要是前期广西降水造成的冷池与低空急流带来的暖湿气团形成的温度锋区和地面辐合线;地形的抬升作用和狭管效应,对降水起到增幅作用。(4)该次强降水主要有2个低质心的热带海洋型中尺度对流系统先后影响发生。

一种下单翼飞机近距耦合导流片的设计与研究

某下单翼通用飞机在大迎角时出现上翼面翼根气流分离,导致飞机最大升力系数降低。在机翼翼根前方的机身上加装小展弦比导流片,通过尾涡为分离区注入的高能气流改善了后方机翼的流场,后方机翼则通过绕流流场诱导导流片尾涡贴近机翼翼面,二者形成了有利耦合。导流片参数影响研究表明导流片与机翼根部翼型相对重叠量约0.023时取得了较好的增升效果,最大升力系数增加量可达0.32。若导流片位置进一步远离机翼则不能与机翼流场耦合,重叠量加大则导流片受机翼干扰自身涡强不足。导流片较优的安装角应保证在机翼大迎角时导流片法向力系数足够大,且失速迎角大于机翼失速迎角。

Diagnostic Analysis of the Evolution Mechanism for a Vortex over the Tibetan Plateau in June 2008

Based on the final analyses data （FNL） of the Global Forecasting System of the NCEP and the obser- vational radiosonde data, the evolution mechanism of an eastward-moving low-level vortex over the Tibetan Plateau in June 2008 was analyzed. The results show that the formation of the vortex was related to the convergence between the northwesterly over the central Tibetan Plateau from the westerly zone and the southerly from the Bay of Bengal at 500 hPa, and also to the divergence associated with the entrance re- gion of the upper westerly jet at 200 hPa. Their dynamic effects were favorable for ascending motion and forming the vortex over the Tibetan Plateau. Furthermore, the effect of the atmospheric heat source （Q1） is discussed based on a transformed potential vorticity （PV） tendency equation. By calculating the PV budgets, we showed that Q1 had a great inffuence on the intensity and moving direction of the vortex. In the developing stage of the vortex, the heating of the vertically integrated Q1 was centered to the east of the vortex center at 500 hPa, increasing PV tendency to the east of the vortex. As a result, the vortex strengthened and moved eastward through the vertically uneven distribution of Q1. In the decaying stage, the horizontally uneven heating of Q1 at 500 hPa weakened the vortex through causing the vortex tubes around the vortex to slant and redistributing the vertical vorticity field.

北京“23·7”极端强降雨特征和成因分析

利用北京地区加密气象站、补盲的北京市规划和自然资源委员会雨量站、双偏振雷达、风廓线雷达、GPS水汽等观测数据和ERA5再分析数据,对北京“23·7”极端强降雨阶段性特征和成因进行了分析。结果表明:“23·7”极端强降雨累计降水量(331 mm)和单点最大降水量(1025 mm)均打破历史纪录,最大雨强(126.6 mm·h^(-1))排名历史第二位,具有显著的极端性。强降雨可分为5个阶段,其中第Ⅱ和第Ⅳ阶段降水量分别占过程累计降水量的37.1%和39.7%,第Ⅳ阶段雨强更大,对应急流更强,高温、高湿特征也更明显。地形对降雨的增幅作用显著,降水量在海拔100~300 m山区迅速增加,极大值出现在海拔约400 m的山区,第Ⅱ(第Ⅳ)阶段山区平均降水量和小时雨强分别是平原的2.1(3.0)倍和2.0(2.7)倍;第Ⅱ阶段主要为地形对急流的直接抬升,第Ⅳ阶段为地形绕流辐合和直接抬升共同作用。7月31日上午(第Ⅳ阶段)边界层急流出口区与低空急流入口区耦合导致低层上升运动增强,促使西部山前β中尺度对流系统由块状发展成线状并有γ中尺度涡旋产生,该β中尺度对流系统北上时形成短暂的列车效应,引发了西部山区8个站次100 mm·h^(-1)以上的极端短时强降水。

COMPUTATIONAL AND EXPERI-MENTAL STUDY ON TIP LEAKAGE VORTEX OF CIRCUMFERENTIAL SKEWED BLADES

In the steady operation condition, the experiments and the numerical simulations are used to investigate the tip leakage flow fields in three low pressure axial flow fans with three kinds of circumferential skewed rotors, including the radial rotor, the forward-skewed rotor and the back- ward-skewed rotor. The three-dimensional viscous flow fields of the fans are computed. In the experiments, the two-dimensional plane particle image velocimetry （PIV） system is used to measure the flow fields in the tip region of three different pitchwise positions of each fan. The results show that the computational results agree well with the experimental data in the flow field of the tip region of each fan. The tip leakage vortex core segments based on method of the eigenmode analysis can display clearly some characteristics of the tip leakage vortex, such as the origination position of tip leak- age vortex, the development of vortex strength, and so on. Compared with the radial rotor, the other two skewed rotors can increase the stability of the tip leakage vortex and the increment in the forward-skewed rotor is more than that in the backward-skewed one. Among the tip leakage vortices of the three rotors, the velocity of the vortex in the forward-skewed rotor is th6 highest in the circumferential direction and the lowest in the axial direction.

Study on local topology model of low/high streak structures in wall-bounded turbulence by tomographic time-resolved particle image velocimetry

The relationship between the in the logarithmic law （log-law） region of bursting event and the low/high-speed streak a turbulent boundary layer is investigated. A tomographic time-resolved particle image velocimetry （TRPIV） system is used to measure the instantaneous three-dimensional-three-component （3D-3C） velocity field. The momentum thickness based Reynolds number is about 2 460. The topological information in the log-law region is obtained experimentally. It is found that the existence of the quadrupole topological structure implies a three-pair hairpin-like vortex packet, which is in connection with the low/high-speed streak. An idealized 3D topological model is then proposed to characterize the observed hairpin vortex packet and low/high-speed streak.

A Climatology of the Southwest Vortex during 1979–2008

Using a new vortex detection and tracing method, a dataset of the Southwest Vortex(SWV) is established based on Japanese 25-year Reanalysis(JRA-25) reanalysis data during 1979–2008. The spatiotemporal features of the SWV are derived from the dataset. In comparison to other seasons, summer yields the least SWVs, but with the highest probability that they will migrate from their region of origin. SWVs mostly emerge in the southwest of the Sichuan Basin and the southeast of the Tibetan Plateau. Migratory SWVs mainly move along either an eastward or southeastward path. Detailed composite analysis of warm-season SWVs shows that the subtropical high is a key factor in determining the direction of migratory SWVs. Furthermore, the steering wind at 700 hPa dominates the moving direction of migratory SWVs. Potential stability diagnosed by pseudo-equivalent potential temperature ? se is of certain significance for the evolution and movement of SWVs. On the other hand, migratory SWVs possess relatively greater strength than stationary SWVs, due to a stronger low-level jet with enhanced baroclinicity and moisture transport providing more energy to support the growth of SWVs along their paths of movement.

A Study on the Dynamic Mechanism of the Formation of Mesoscale Vortex in Col Field

The mesoscale vortex associated with a mesoscale low-level jet （mLLJ） usually causes heavy rainfall in the col field. The col field is defined as a region between two highs and two lows, with the isobaric surface similar to a col. Using a two-dimensional shallow water model, the meso-β scale vortex couplets （MβVCs） induced by eight types of mesoscale wind perturbations in an ideal col field were numerically simulated. With the sizes of -100 km, the MβVCs induced by northerly perturbation （NP） and southerly perturbation （SP） moved toward the col point. The sizes of MβVCs induced by southwesterly perturbation （SWP）, southeasterly perturbation （SEP）, northwesterly perturbation （NWP）, and northeasterly perturbation （NEP） were relatively small for the perturbations moving toward dilatation axis. The MβVC induced by easterly perturbation （EP） and westerly perturbation （WP） could not develop because they quickly moved away from the col point, before the circulation could form. The size of the circulation was determined by the distance between the vortex and the col point. The closer to the col point the vortex was, the larger the size of vortex. The comparisons of maximum vorticity and vorticity root mean square error （RMSE） of the NP, the SWP, and the WP show that the maximum vorticity and the vorticity RMSE of the NP decreased slower than other perturbations. Therefore, the weak environment of the col field favors the maintenance of vorticity and the formation of vortex. When a mesoscale vortex forms near the col point or moves toward the col point, it may maintain a quasitationary state in the stable col field.

多能互补条件下转轮优化对水轮机低负荷区稳定性能的影响

多能互补系统中新能源发电的不稳定性使得作为调能机组的水电机组频繁在水力效率低、振动剧烈的低负荷区运行,严重影响机组的寿命。该研究以多能互补系统中的混流式水轮机为研究对象,在前期考虑工况权重系数的转轮多工况优化设计结果基础上,对比分析了优化前后转轮叶片的几何参数变化,不同负荷区的水轮机内部流动状态及压力脉动特征差异。研究结果表明:优化后叶片包角、安放角以及叶片长度均有所增加,叶片表面压力分布及转轮进出水边速度矩分布更加均匀,有助于改善水轮机低负荷区的空化性能、提高能量转换能力。转轮进出口安放角的增加很好地抑制了转轮进口背面脱流涡及出水边的脱流涡区,改善了尾水管的入流条件,使得尾水管涡带的强度和影响范围明显减小。叶片优化后,转轮内各频率的压力脉动幅值均有不同程度的降低,尾水管内压力脉动改善明显。尾水管内0.2f_(n)(f_(n)为转频)和14f_(n)压力脉动在低负荷工况(OP1)幅值降幅分别为45%和40%,额定工况(OP4)尾水管内0.2f_(n)压力脉动基本消除,14f_(n)压力脉动幅值降幅为31%。本文所得研究结果对多能互补系统中水轮机转轮的设计优化及运行具有参考意义。

MODULATION OF MADDEN-JULIAN OSCILLATION ON TIBETAN PLATEAU VORTEX

This study uses NCEP/NCAR daily reanalysis data,NOAA outgoing long-wave radiation(OLR) data,the real-time multivariate MJO(RMM) index from the Australian Bureau of Meteorology and Tibetan Plateau vortex(TPV)data from the Chengdu Institute of Plateau Meteorology to discuss modulation of the Madden-Julian Oscillation(MJO)on the Tibetan Plateau Vortex(TPV).Wavelet and composite analysis are used.Results show that the MJO plays an important role in the occurrence of the TPV that the number of TPVs generated within an active period of the MJO is three times as much as that during an inactive period.In addition,during the active period,the number of the TPVs generated in phases 1 and 2 is larger than that in phases 3 and 7.After compositing phases 1 and 7 separately,all meteorological elements in phase 1 are apparently conducive to the generation of the TPV,whereas those in phase 7 are somewhat constrained.With its eastward propagation process,the MJO convection centre spreads eastward,and the vertical circulation within the tropical atmosphere changes.Due to the interaction between the mid-latitude and low-latitude atmosphere,changes occur in the baroclinic characteristics of the atmosphere,the available potential energy and eddy available potential energy of the atmosphere,and the circulation structures of the atmosphere over the Tibetan Plateau(TP) and surrounding areas.This results in significantly different water vapour transportation and latent heat distribution.Advantageous and disadvantageous conditions therefore alternate,leading to a significant difference among the numbers of plateau vortex in different phases.

小流量工况下混流泵涡识别及其演变规律

为了研究小流量工况下混流泵内部流动状态及涡结构的演化规律,采用大涡模拟的计算方法并结合先进的Omega涡识别方法,对某混流泵小流量工况下的涡结构进行识别,获得了叶轮内部典型涡结构的特征和演化规律,并与叶片表面的涡量生成和流动分离情况进行对比分析.研究结果表明:Omega方法克服了第二代涡识别方法需要人为调节阈值的缺陷,可以较好地识别小流量工况下混流泵内部的精细涡结构;在小流量工况下,混流泵内的叶片斜向涡带、叶尖涡和叶尖分离涡、通道涡以及尾缘脱离涡是叶轮流道内生成的典型涡结构,它们有各自独立的生成和发展过程,又相互作用,使叶轮内流场更加紊乱.本研究揭示了小流量工况下混流泵内部特有的涡结构特征与演变规律,可为包括混流泵在内的叶轮机械流场分析和性能优化提供一定的理论指导和技术支撑.

Numerical Investigation on a Dual-jet Consisting of a Plane Wall Jet and a Parallel Offset Jet at Low-Reynolds Number

A dual-jet consisting of a wall jet and an offset jet has been numerically simulated using lattice Boltzmann method to examine the effects of jet spacing between two jet centerlines,defined as s.The Reynolds number based on jet-exit-width dis set to be Re = 56 and the jet spacing is set to be less than or equal 10 times the jet-exitwidth.Computational results reveal that the flow field displays periodic vortex shedding when the jet spacing is in the range of 9≤s/d ≤ 10,while it remains steady with two counter-rotating vortices in the converging region when s/d ≤ 8.When s/d = 9,the power spectral analyses indicate that the vortex shedding phenomenon has specific frequency.The significant oscillation stresses induced by the periodic components of velocities are found to mainly exist in the inner shear layer regions,implying stronger momentum transfer occuring in these regions.

桂林“5·22”大暴雨的MCS特征及对短时强降雨的影响

利用常规观测资料、风云气象卫星四号A星(FY4A)资料、欧洲中期天气预报中心全球第五代大气再分析数据集(EAR5)以及桂林和柳州多普勒雷达资料,分析2023年5月22日桂林极端大暴雨过程的中尺度对流系统(MCS)特征及其对短时强降雨的影响。结果表明,此次过程降水时段集中、局地性强、极端性大,强降水时段与对流云团的强烈组织发展阶段基本一致。在“北槽南涡”的环流背景下,高原低涡东移及其切变线诱发MCS生成,地面冷空气和辐合线使其强烈发展。降水回波强度强,质心低,降水效率高,强回波柱在桂林市区维持。MCS具有低层正涡度、负散度,高层负涡度、正散度的垂直结构,上升速度大,利于发展维持。MCS发展前期对流有效位能(CAPE)值迅速增大,桂林处于有利的抬升环境中,大气可降水量峰值出现时间与强降水发生时间对应。