助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   高压— 的翻译结果: 查询用时:0.03秒
图标索引 在分类学科中查询
所有学科
更多类别查询

图标索引 历史查询
 

高压
相关语句
  high-and
     This paper introduces the high-and Ultra-high-pressure experiments being constraint to the layering structure of the Earth, and new experimental results of the origin of the rare magma related to the mantle C-H-O system.
     本侧重介绍高压—超高压实验对地球层圈结构的约束以及与地幔C—H—O系统密切相关的一些稀少的火成岩岩浆起源的实验成果.
短句来源
     The break-off of subducted slab, quick exhumation of high- and ultrahigh-pressure metamorphic (UHPM) rocks, and the late Triassic (205~225 Ma) alkaline magmatism suggest the beginning of Mesozoic lithospheric thinning in the NCC.
     俯冲板片的断离以及高压—超高压变质岩的快速折返和晚三叠世 ( 2 0 5~ 2 2 5Ma)的碱性岩浆作用的存在均暗示 ,华北克拉通中生代岩石圈减薄已经开始。
短句来源
  “高压—”译为未确定词的双语例句
     The GIS rated voltage range covers 72kV — 120kV — 300kV — 550kV — 800kV — 1100kV, namely the high voltage- supervoltage and extra high voltage
     日本GIS的额定电压从72kV—120kV—300kV—550kV—800kV—1100kV,也就是从高压——超高压——特高压。
短句来源
     Exhumation Structure and Mechanism of the Sulu Ultrahigh-pressure Metamorphic Belt, Central China
     苏鲁高压—超高压变质带的折返构造及折返机制
短句来源
     METAMORPHIC CHARACTERISTICS &P-T-t PATHS OF THE HIGH-ULTRAHIGH PRESSURE METAMORPHIC TERRANE IN SOUTHERN HUAIYANG
     南淮阳高压—超高压变质地体的变质作用特征及其P—T—t轨迹
短句来源
     PETROGRAPHY AND METAMORPHISM STUDY ON HIGH-UITRAHIGH PRESSURE ECLOGITE FROM GUANPO ARE, NORTHERN QINLING MOUNTAIN
     北秦岭官坡地区高压—超高压榴辉岩岩相学及变质作用研究
短句来源
     During the period of 150~100 Ma, the extension events involved the formation of both the transtension shear zone at the northern boundary and the Laiyang Cretaceous basin, the emplacement of the granites, and the formation of an anticline form with ductile-brittle normal slip structures due to curved exhumed foliations.
     150~100 Ma期间的伸展事件包含了北界韧性伸展转换性剪切带及莱阳盆地的形成、苏鲁高压—超高压变质带北部花岗岩侵位、折返面理弯曲形成背形构造及伴随的韧-脆性正滑构造。
短句来源
更多       
  相似匹配句对
     HIGH PRESSURE HEAT EXCHANGER
     高压换热器
短句来源
     Selection of HV Electrical Equipment
     高压电气设备选择
短句来源
     ON THE ULTRAHIGH PRESSURE AND HIGH PRESSURE SHEAR ZONES
     超高压高压剪切带
短句来源
查询“高压—”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  high-and
X-ray diffraction (XRD), optical microscopy (OM) and micro-infrared (IR) spectroscopy have been applied to characterize the crystallized layers of high- and low-quality seawater-cultured pearls produced in South China.
      
combined administration of high-and lowmolecular-weight microbial autoregulators (extracellular RNase fromBacillus intermedius and anabiosis inducing factord1) are reported for the first time for cultured cells of higher eukaryotes.
      
meyerii consists of the high- and low-molecular-weight fractions (40 and 2-5 kDa, respectively) and contains a large number of β-1→6-bound glucose residues.
      
Both hormones increased heterogeneity of high-and medium-molecular-weight nonhistone chromatin proteins but had no effect on the polypeptide profile of histones.
      
Possibilities of Combining High- and Low-Thrust Engines in Flights to Mars
      
更多          


In the summer half year,the average intensity of the Pacific high pressurechanges more or less abruptly.It strongly increaseses from June to July and de-creases gradually from April to June.In middle September it decreasees suddenly. In.the summer season(from June to August),tha advance and retreat of theWestern Pacific pressure ridge(moving from east to west or reversed)is intimatelycorrelated with teh upper westerlies.At the same time,the Pacific High itselfis an important factor of the atmospheric circulation.When...

In the summer half year,the average intensity of the Pacific high pressurechanges more or less abruptly.It strongly increaseses from June to July and de-creases gradually from April to June.In middle September it decreasees suddenly. In.the summer season(from June to August),tha advance and retreat of theWestern Pacific pressure ridge(moving from east to west or reversed)is intimatelycorrelated with teh upper westerlies.At the same time,the Pacific High itselfis an important factor of the atmospheric circulation.When the zonal circulationis strong,the intensity of the Pacific High is also relatively strong and the posi-tion of the western Pacific pressure ridge changes little.When the small wavesin the westerlies move out from Asia into the Pacific Ocean,the position ofthe western Pacific pressure ridge only vibrates slightly.But,when the waves in thewesternlies are strong,the western Pacific pressure ridge advances westward andthen retreats eastward apparently.The period advance and retreat of the ridgeis about five or six days During the period of fow zonal circulation index, thewestern Pacific pressure ridge moves eastward.when the circulation index growsfrom low to high,the ridge advances westward.The range of longitudes ofoscillation of the ridge in this type is largest,about 30-40 degrees,and the periodof oscillation is longest,about half month in general.The longest period reachesone month. Besides,the movement of the Pacific High ridge is also studied in relationto he tropical systems,such as typhoons.

夏半年太平洋高压的平均变化,带著突变性质的增强和减弱,突然的增强发生6月到7月,而4月至6月更有逐渐减弱的趋向,到9月中旬以後则突然的减退。 夏季西太平洋高压脊的东西进退和整个西风环流变化及西风环流的情况密切关连,同时太平洋高压本身也是西风环流及其变化的重要因素之一。当西风环流强时,太平洋高压比较强大,这时太平洋高压脊的变化很少,在西风环流小波动东移的过程中,太平洋高压脊只有微小的摆动。但西风带波动较大时,随着西风槽和高压脊的东移,太平洋高压脊便有了比较长时期的和明显的东退和西伸,它的周期一般都在5、6天左右。如果西风环流起了大型的变化,即西风环流由强转弱,再由弱转强,太平洋高压脊随之不断的东退和西伸,进退的范围可达30-40经距。它的周期较长,一般都在半个月的光景,最长的可达一个月,10天以内的很少。 太平洋高压脊除了和西风带的环流,极地高压和低压槽有关外,也和它南边的气压系统,如台风和热带风暴有关。

This is a brief report of a preliminary survey of certain rain-bearing systems over China in later spring and summer. In the first part, a general description of the methods of analysis used in this survey is given. As the temperature and wind fields are weak, and the precipitation is heavy, smaller intervals for the isotherms and contours in the constant pressure surface and pseudo-equivalent potential instead of potential temperature in the cross section analysis are used.In the second part, there are descriptions...

This is a brief report of a preliminary survey of certain rain-bearing systems over China in later spring and summer. In the first part, a general description of the methods of analysis used in this survey is given. As the temperature and wind fields are weak, and the precipitation is heavy, smaller intervals for the isotherms and contours in the constant pressure surface and pseudo-equivalent potential instead of potential temperature in the cross section analysis are used.In the second part, there are descriptions of the structure and development of five frequently observed rain-bearing systems i.e. cold front, blocking high and cold vortex, monsoon heat low, warm front and typhoon.The last part consists of discussions of some points of view in synoptic meteorology in China. It is stated that the monsoon precipitation is various in intensity and duration according the large-scale flow patterns. The difference of moisture content in the middle troposphere as a criterion for the identification of equatorial or tropical maritime air mass is proved to be missleading. It is shown that the upper air moist content is high only within the raining region near the polar or equatorial front. To the south of the equatorial front within the so-called equatorial air mass, the moist content in the middle troposphere is as low as within the tropical maritime air mass. It is the convergence and lifting of the tropical air mass which releases the convective instability and induces the surface moist air rising to the middle troposphere. The phenomenon of the forward-inclination of the so-called North-West Trough based on the time cross-section of wind is proved to be a mistake by combining two systems into one trough. The terminology of shear line, and the correct application of synoptic models in weather analysis and forecas-ting are also discussed.

本文是一年来从事夏季降水天气初步普查的简单报告。第一节首先指出所用分析方法与一般国内所通用者,稍有不同。高空等压面分析,取20米作为等高缐间隔,2℃作为等温缐间隔。代替40米及5℃的间隔,以适应夏半年较弱的温度场与气压形势场,在剖面分析中以等假相当位温缐代替位温缐,与等温缐配合以适应降水天气的凝结降水过程。 第二节讨论了五种夏半年基本降水天气系统,即冷锋、阻塞高压与冷涡、季风热低压、 暖锋及有风的结构,并简单地叙述了演变过程。 第三节对某些天气概念提供一些批判性的讨论。根据现已增加的观测材料,论证季风与梅雨是多样性的,决定于大规模的温度场与流场特性,以高空湿度大小区分赤道气团与热带海洋气团,证明是不适当的,因为中国赤道锋降水区域以南,即在所谓南南季风的赤道气团中,中层大气仍是干燥的。降水区域内,中层对流层的大量水份,是由于辐合或抬升的作用,使潜势的对流不稳定性成为现实的不稳定性,而由下层空气上升带上去的。文中还论证了所谓西北槽槽缐前倾是将两个系统混作—个系统的不正确桔果。最后还讨论了切交缐及一般模型在天气分析预报中的应用与限制。

The synoptic process on 500mb over Asiatic natural synoptic region have been analized for 5 summers. The results are given below:1.The variation of the position and strength of the maximum westerly wind belt at 500mb surface along four meridians 65°E, 105°E, 120°E, 140°E gives a good index in determing the natural synoptic seasons over Eastern Asiatic synoptic natural region. The disappearence of the low latitude westerly wind maximum along 65°E is the first indication of the beginning of Bai-U period. When...

The synoptic process on 500mb over Asiatic natural synoptic region have been analized for 5 summers. The results are given below:1.The variation of the position and strength of the maximum westerly wind belt at 500mb surface along four meridians 65°E, 105°E, 120°E, 140°E gives a good index in determing the natural synoptic seasons over Eastern Asiatic synoptic natural region. The disappearence of the low latitude westerly wind maximum along 65°E is the first indication of the beginning of Bai-U period. When the westerlies wind maximum belt to the south of 40°N completely disappears along 140°E summer begins. This is accompanied with the filling of the Asiatic main trough over Japan and the Northward shiff of the Pacific subtropical high pressure belt from low latitudes to 30°-40°N. The mean date on which summer begins is nearly on 13th, July. It is also the end of Bai-U over middle Yangtze river. Thence the synoptic process in Bai-U period is the prevailing process before summer season. The precipitation in this period is closely related to the strength of the maximum wind belt i.e. socalled frontal zone.2.When the 600mb maximum westerly wind belt appears again at 30°-40°N along 140°E, begins author. The synoptic process, which associates with it, is the reestablishment of the Asiatic main trough over Japan. And the surface cold continental high comes down to North China from the east of Novaya Zemlya Island. The average time of the arrival of Autumn is nearly on 5th, September. Hence the duration of summer is on the average only 55 days.8. According to the analysis of the time variation of maximum westerlies on 30°-40 °N along each of the four meridians, the westerly maximum generally disappears earlier in west than in east but establishes later in west than in east during autumn. The phenomeanon that the maximum westerly first generates in the east during autumn can hardly be explained by the splitting of the jet stream.4. From the analysis, the prevailing process of the natural summer season largely depends upon the variations in the upper westerlies over Ural region and the west-east relative position of the Pacific subtropical high with respect to the Tibet plateau.

本文根据1951—1955年五年高空和地面的资料,对夏季过程进行了分析,得到下面几点结果: 1.在东亚地区的四个主要经度带上以65°,120°和140°经度带的500毫巴强西风中心的位置和强度变化,对东亚自然天气季节的划分是最良好的指标。东经65°经度带上南边低纬度强西风的消失是梅雨期开始前的征兆。东经140°经度带上强西风在北纬40°以南消失时是夏季开始的征兆。和它相关联的过程是东亚高空大槽的消失和太平洋副热带高压带北移至30°—40°纬度带间,这个期间平均是在7月13日左右,也是江南梅雨结束的时候。故梅雨是夏季以前的盛行过程,它和500毫巴强西风区或锋区是有密切的联系的。 2.东经140°经度带上500毫巴强西风在北纬30°—40°重现时,是夏季结束秋季开始的征兆,和它相关连的天气过程是在该经度带上高空大槽重新建立,地面大陆冷高压从新地岛东部向东南下达华北地区。这个时间平均是在9月5日左右。故东亚夏季的长度平均仅55日。 3.从500毫巴强西风在各经度带上出现的情况来看,一般是西部比东部消失得早,出现得迟,不如冬季那样先在上游首先建立,在春夏之交这种相反的演变,似非地形的分支可以解...

本文根据1951—1955年五年高空和地面的资料,对夏季过程进行了分析,得到下面几点结果: 1.在东亚地区的四个主要经度带上以65°,120°和140°经度带的500毫巴强西风中心的位置和强度变化,对东亚自然天气季节的划分是最良好的指标。东经65°经度带上南边低纬度强西风的消失是梅雨期开始前的征兆。东经140°经度带上强西风在北纬40°以南消失时是夏季开始的征兆。和它相关联的过程是东亚高空大槽的消失和太平洋副热带高压带北移至30°—40°纬度带间,这个期间平均是在7月13日左右,也是江南梅雨结束的时候。故梅雨是夏季以前的盛行过程,它和500毫巴强西风区或锋区是有密切的联系的。 2.东经140°经度带上500毫巴强西风在北纬30°—40°重现时,是夏季结束秋季开始的征兆,和它相关连的天气过程是在该经度带上高空大槽重新建立,地面大陆冷高压从新地岛东部向东南下达华北地区。这个时间平均是在9月5日左右。故东亚夏季的长度平均仅55日。 3.从500毫巴强西风在各经度带上出现的情况来看,一般是西部比东部消失得早,出现得迟,不如冬季那样先在上游首先建立,在春夏之交这种相反的演变,似非地形的分支可以解释的。 4.在夏季自然天气季节所出现的盛行天气过程主要是表现在太平洋副热带高压随上游气压场的不同,及其和?

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关高压—的内容
在知识搜索中查有关高压—的内容
在数字搜索中查有关高压—的内容
在概念知识元中查有关高压—的内容
在学术趋势中查有关高压—的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社