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plateau     
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  高原
     Ecological heterogeneity in the sandy grassland of Ordos Plateau,China
     鄂尔多斯高原沙地草地的生态异质性
短句来源
     The Cenozoic High-k Calc-alkaline Volcanic Rock Series in the Northern Tibetan Plateau: Implications of Crust-mantle Interaction
     藏北高原新生代高钾钙碱性系列火山岩与壳—幔相互作用
短句来源
     Experiment Research of Construction Technique and Technology of the Plateau Tunnels in Permafrost Soil
     高原多年冻土隧道施工技术及工艺试验研究
短句来源
     Studies on Biology and Genetic Diversity of Two Endemic Fishes in Lakes of Yunnan Plateau
     云南高原湖泊特有鱼类的生物学与遗传多样性研究
短句来源
     Studies on the Ecological Adaptability of the Genus Caragana on the Ordos Plateau
     鄂尔多斯高原锦鸡儿属(Caragana Fabr.)植物的生态适应性研究
短句来源
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  平台
     A COMMENT ON THE PLATEAU COMBUSTION MECHANISM OF THE DOUBLE-BASE PROPELLANTS
     评双基推进剂平台燃烧机理
短句来源
     THE PROBLEM IN THE CALCULATION OF VOLTAGE PLATEAU WIDTH OF RF-SQUID TANK CIRCUIT VOLT-AMPERE CURVE
     RF—SQUID谐振电路伏安曲线上电压平台宽度计算中的问题
短句来源
     BOUNDARY AND JUNCTION CONDITIONS FOR PLATEAU STRUCTURE OF DENSITY PROFILE IN A LASER PLASMA
     激光等离子体中平台型密度分布结构的边界条件和连接条件
短句来源
     THE FAILURE ASSESSMENT CURVE AND DUCTILE FRACTURE ASSESSMENT OF METAL MATERIALS WITH YIELDING PLATEAU
     带屈服平台金属材料的失效评定曲线及延性断裂评定
短句来源
     The Study of Model for Catalyzed Combustion of Plateau Propellant with Lead and Carbon
     平台双基推进剂铅炭催化燃烧模型的研究
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     The relations between content of various quenchers (H_2C(OCH_3)_2, C_2H_5OH, C_6H_6 and C_7H_(12)), plateau curves and the efficiency ane dead time of the tube were measured.
     研究了几种不同的猝灭剂(H_2C(OCH_3)_2、C_2H_5OH、C_6H_6、C_7H_(12)含量与曲线的关系;也测量了该计数器的探测效率和死时间。
短句来源
     The single-grain zircon 207Pb/206Pb age is 2675±2 Ma and amphi-bole 40Ar/39Ar plateau and isochron ages are 2372. 98 ± 47. 46 Ma and 2349. 10 ± 46. 98 Ma respectively.
     获得锆石~(207)Pb/~(206)Pb年龄为2675±2 Ma,角闪石~(40)Ar/~(39)Ar年龄和等时线年龄分别为2372.98±47.46Ma和2349.10±46.98Ma。
短句来源
     The experimental results show that the plateau length is 300 V; the plateau slope 0.608%/100V,the lower detection limit 0.221 Bq·cm-2(for 600 s),the stability of the instrument 0.56%/h,the variance coefficient 2.88%,and the detection efficiency 84%(for the 2π surface emissivity of 3H source 1307/min-1).
     经过应用实验表明,仪器性能指标为:长300V,斜0.608%/100V,探测下限0.221 Bq·cm-2(测量时间600s),仪器稳定性0.56%/h,仪器变异系数2.88%,探测效率84%(3H源,2π表面发射率1307min-1)。
短句来源
     The two samples from granite yielded plateau ages of 932.3±0.6Ma and 891.0±1.9Ma, isochron ages of 933. 8±6. 8Ma and 892. 2±32. 7Ma, respectively.
     花岗闪长岩的加~(40)Ar-~(39)Ar年龄为932.3±0.6Ma和891.0±1.9Ma,相应的等时年龄分别为933.8±6.8Ma和892.2±32.7Ma;
短句来源
     the plateau age of~(40)Ar/~(39)Ar of monomineral muscovite in the press-broken mid-fine muscovite was determined at the Beikou, Kaoshan Town, which is 135.66 0.11Ma, and its isochronal dating is 135.43±0.26Ma.
     在靠山镇北口获得中细粒碎裂白云母/二云母花岗白云母单矿物40Ar/39Ar年龄135.66±0.11Ma,等时线年龄135.43±0.26Ma。
短句来源
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  “plateau”译为未确定词的双语例句
     Study on the Potential of Rainwater Resourcfulization and the Model of Network Utilization of Small Watershed in the Loess Plateau
     小流域雨水资源化潜力及网络化利用模式研究
短句来源
     Research into Several Key Problems Existing in Vegetation Construction in Loess Plateau
     黄土高原植被建设中若干关键问题的研究
短句来源
     Study on Soil Water Movement and Its Cycling on a Hillslope of the Loess Plateau
     黄土区坡地土壤水分运动与转化试验研究
短句来源
     Study on Sustainable Development of Minor Crops Production in the Loess Plateau of China
     黄土高原小杂粮生产可持续发展研究
短句来源
     The Technique of ~(39)Ar-~(40)Ar Dating and Isotopic Geochronology Study of Tibetan Plateau
     ~(39)Ar-~(40)Ar定年技术及其在青藏高原多期地质事件年代学中的应用研究
短句来源
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  plateau
Diurnal Course of Gas Exchange and Water Use Efficiency of Platycladus orientalis in the Semiarid Region of the Loess Plateau
      
Relation between Growth and Vertical Distribution of Fine Roots and Soil Density in the Weibei Loess Plateau
      
The influence of woodland soil bulk density on the growth and distribution of fine root system of main planting tree species in the Weibei Loess Plateau was investigated by means of pot culture and field survey.
      
To enrich resource of species, 105 arbor species (25 genera, 15 families) were introduced to the hilly and gully areas on Loess Plateau.
      
Rapid changes of soil properties following Caragana korshinski plantations in the hilly-gully Loess Plateau
      
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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释的。 4.在夏季自然天...

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?

During High-Index Circulation over Far East, A series of cold trough in the upper troposphere may pass over Tibet plateau from the west and move to Eastern China. But in the lower troposphere these troughs are very obscured over the plateau. In this paper the structure and characteristics of these troughs are discussed, and a synoptic example of Feb. 10-12 1956 is given.

在亚洲中部和南部上空平直西风的环流条件下,往往有一个个高空西风带的低压槽从亚洲西部越过西藏高原移到中国东部。这类高空的低压槽在低层对流层大气中表现不很清楚,但在高层对流层中却表现很显著。在本文中对于这类高空槽的结构和性质作了叙述,并举出1956年2月10—12日的一个高空低槽的例子。

The structure of general circulation over the Asia, in the period of Jan. 1st. to Mar. 10th., 1956, is investigated using all available aerological material. It is found that:1.During thus period there existed two jet streams over the continent. This two jets combined into one jet at the meridian 140°E.2.Both jets over Eastern Asia are accelerated downstream. The southern one starts acceleration from the meridian 75°E, while the northern one was not acce 1e rated before reading Ere meridian 100°E.3.The baroclinity...

The structure of general circulation over the Asia, in the period of Jan. 1st. to Mar. 10th., 1956, is investigated using all available aerological material. It is found that:1.During thus period there existed two jet streams over the continent. This two jets combined into one jet at the meridian 140°E.2.Both jets over Eastern Asia are accelerated downstream. The southern one starts acceleration from the meridian 75°E, while the northern one was not acce 1e rated before reading Ere meridian 100°E.3.The baroclinity of the atmosphere over Eastern Asia is mainly concentrated in the vicinity of the Tibetan Plateau.It is considered that the existence of the Tibetan Plateau has the following three effects on the general circulation:1.The existence of the plateau intensifies the baroclinity (along the N-S as well as W-E directions) around the plateau, south of which a vertical circulationis formed.2.The confluence of the two jets, thus also the acceleration of them, is due to the existence of the plateau.3.The existence of plateau makes the southern jet intensified and steady.

根据1956年1月到3月上旬亚洲地区高空资料,对亚洲大陆上空的大气环流进行了探讨。作者得出了下列的事实: 1)在上述时间期限内的平均情况表明,亚洲大陆上空存在着二支急流。这二支急流在东经140°经度上已经汇合。 2)二支急流在东亚部分都表现有向东加速的现象。南支急流自东经75°就开始明显地向东加速。而北支急流的加速自东经100°附近才开始。 3)东亚大陆上大气的斜压性主要是集中在高原的附近。 另外对上述现象也作了一些初步的研究。作者认为西藏高原的存在对大气环流有下列三方面的影响: 1)高原加强了大气的斜压性,并且在高原南方形成垂直环流。因而强烈的加速了南支急流。 2)高原的存在使得南北二支急流在其东侧互相接近,显然地影响了急流的加速。 3)高原保证了南支急流强大而且稳定,这就是说每天每年同季的变化都小。

 
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