对流云团,convective cloud
1)convective cloud对流云团
1.Hail s strength are associated withconvective cloud s evolution and strength.北疆夏季两次冰雹天气过程的对比分析发现,充足的水汽、足够大的上升运动和不稳定的层结是冰雹天气出现的必备条件,而降雹的强弱则与对流云团的发展和强度有关。
2.The first strong precipitation is caused by strengthening localconvective clouds generated in the subtropical high,vapor transportation and dynamic conditions offered by strengthened easterly flow in bottom of the troposphere air promote the development of convection;New clouds in the humid air environment will be rapidly strengthened and developed.通过对常规气象资料分析,发现①第一时段的强降水由副热带高压内部产生的局地对流云团加强造成,对流层底层东风气流的加强提供的水汽输送和动力抬升作用,促进了对流发展;②新生云团进入潮湿的大气环境中能够得到迅速的发展加强。
英文短句/例句
1.Detection and Analysis on Deep Convective Clouds in a Frontal Cyclone Using Multispectral Remote Sensing Data一次锋面气旋云系中强对流云团的识别
2.ELEMENTARY STUDY ON NORTHWARD MOVEMENT OF CONVECTIVE CLOUD CLUSTER OVER THE BAY OF BENGAL TO THE LOW LATITUDE PLATEAU DURING EARLY SUMMER初夏孟加拉湾对流云团北上低纬高原的初步研究
3.Low-level jet and monsoon cloud swell are the most important factors for thedevelopment of cloud clusters.低空急流和季风云涌是云团发展的最重要因子。
4.Two-fluid large eddy turbulence model is applied to research the movement of the sand clouds in quiescent water.本文采用双流体大涡紊流模型对静水中泥沙云团下落过程进行了研究。
5.patchy fog, mist, cloud, etc团团的雾、 霭、 云等.
6.8 in 1979. There was an area of mesoscale convergence formed by the upper outflow of the cloud cluster and the environmental flow in the upwind.扰动云团的高空流出气流和环境气流在云团的上风方向形成中尺度辐合区。
7.cumulus convection over tropical ocean热带海洋上积云对流
8.The residual effects of the cloud clusters are generally ignored even though the area they cover is perhaps an order of magnitude larger than the convective region itself.云团的残余影响通常是忽略不计的，即使它们覆盖的地区比对流区本身可能大一个量级也如此。
9.A Reinterpretation of the Court Robes Emblazoned with Eight Roundels Enclosing Golden Dragons in Flight among Coloured Clouds;对清代八团彩云金龙纹吉服的再认识
10.Convective clouds merger into convective and stratiform mixed clouds in mountainous area山地对流云并合形成积层混合云的过程分析
11.For less active convection, cumuliform clouds grow with less rapidity.当对流不太活跃时，积云增长不太快。
12.The Nujiang River Valley under the Administration of Nanzhao and Dali Kingdoms;南诏、大理国对云南怒江流域的经略
13.Effect of turbulence on spark ignition process of dust cloud湍流对粉尘云电火花点火过程的影响
14.Impacts of Picea Crassifolia Forest on Runoff in Pailugou Watershed of Qilian Mountains;青海云杉林对祁连山排露沟小流域径流的影响
15.An Algorithm of Classifying Convective and Strariform Pricipitation and Primary Application in Estimating Precipitation;层状云和对流云雷达回波的自动识别及其在估测降水中的应用
16.Numerical study of influence of cloud-hydrometeor advections on precipitable cloud system.云凝结物平流输送对降水云系发展影响的数值模拟研究
17.It also resembles a person doing Taiji shadow boxing.图案如行云流水，和谐生动，充满运动感，象征世界人民团结、作、流、展，携手共创新世纪。
18.A Comparative Experimentation of Cumulus Parameterization Schemes on Heavy Rainfall;暴雨模拟中积云对流参数化方案的对比试验
相关短句/例句
convective cloud cluster对流云团
1.Based on analysing 9 cases of mesoscaleconvective cloud cluster over clod front cloud system during 1994~2002, it was found that the origin in which the mesoscale convective cloud was outgrowth located in middle and southern parts of Guizhou province .通过对1994～2002年间9次由冷锋云系中尺度对流云团分析,发现广西前汛期冷锋云系中尺度对流云团的源地主要是黔西南和黔中;移动方向是东或东南;当环境云场强度指数≥28有利对流云团的发展,≤26时不利对流云团的发展;初步研究了中尺度对流云团生命史不同阶段的卫星云图形态特征,给出了中尺度对流云团降水的时空分布特征。
2.The mainly features of mesoscaleconvective cloud clusters during four heavy rainfall stages in Changjiang River Basin have been studied by using GMS TBB data of every hour on every day from June to August in 1998.运用１９９８年６～８月逐日逐时ＧＭＳ辐射亮度温度ＴＢＢ资料，统计和分析了长江 流域４个大暴雨时段中各自中尺度对流云团活动的一些主要特征，指出长江流域的这场罕见 大水是在特定的环流形势下，由３１５个β中尺度和α中尺度对流云团直接造成的。
3)strong convective cloud强对流云团
1.Based on EOS/MODIS multi-channel remote sensing data,the characteristics of astrong convective cloud were analysed qualitatively according to a heavy rainfall in the northern of Anhui province from 30, June to 1,July in .根据EOS/MODIS多通道遥感数据,针对6月30日20:00～7月1日20:00安徽省北部出现的一次强降水,定性地分析了产生暴雨的强对流云团的特征,揭示了强对流降水云团的云系特征和结构特征,并用地面雨量观测资料开展验证分析。
4)convective cloud cell splitting对流云团提取
5)convective cloud clusters孟湾对流云团
1.This paper analyses the northward movement and activity ofconvective cloud clusters over the Bay of Bengal through May to June.结果表明:初夏孟湾对流云团活动对低纬高原的初夏降水有明显影响;孟湾北部及其东部海域和沿岸是对流云团北上频数最多的地区;下风方伴随风速大值区的西南气流有利于孟湾云团北上;孟湾云团北上与西太平洋副热带高压的活动和位置关系密切。
6)Tropical convective cloud cluster热带对流云团
延伸阅读
热带云团热带云团tropicalcloudcluster存在于热带地区由大量对流云所组成的直径在4～10个纬度距离(简称纬距)范围内的云区。这种云团是从卫星云图上发现的。云团所经过的地区，常发生大风和暴雨，并能发展成东风波、台风等热带天气系统。热带云团是近年来人们所注意的热带天气系统。从全球范围看，云团有3种类型：①爆玉米花状云团。尺度比较小，多出现在南美大陆的热带地区和中国西藏的南部地区，有明显的日变化。②普通云团。水平直径在4个纬距以上，常发生于热带辐合带中。③季风云团。它和西南季风活动有密切联系，发生于热带的印度洋和东南亚，南北宽达10个纬距，东西长达20～40个经距，冬季约位于北纬5°～10°，自6月中旬开始，随季风的推进，爆发似地向北发展，到8月份，可推进到北纬20°～30°。热带云团的尺度差别较大，有中尺度的和小尺度的，也有中间尺度的和天气尺度的（见天气系统）。云团本身由尺度为10～100千米、生命期为数小时到一天的中对流云系和尺度为4～10千米、生命期为30分钟到数小时的小对流云系(即积雨云塔)所组成。
