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east
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    Relationships between the Precipitation in China and the SST in the Equatorial East Pacific
    赤道太平洋海面温度与我国降水的关系
短句来源
    Relationships between the Temperature in China and the SST in the Equatorial East Pacific
    赤道太平洋海面温度与中国气温的关系
短句来源
    The Study of Height of Thermal Internal Boundary Layer in the East Coast of Liao Dong Bay
    辽海岸地区热内边界层特性研究
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    Features of “1997.8.6” Storm Rainfall System in East Gansu
    陇“1997.8.6”暴雨天气系统影响特征
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    THE EFFECT OF SPATIALLY NONUNIFORM HEATING ON THE FORMATION AND VARIATION OF SUBTROPICAL HIGH PART II: LAND SURFACE SENSIBLE HEATING AND EAST PACIFIC SUBTROPICAL HIGH
    空间非均匀加热对副热带高压形成和变异的影响II:陆面感热与太平洋副高
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  东部
    CWRF Application in East China Monsoon Area
    CWRF在中国东部季风区的应用
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    THE CLIMATIC AND SYNOPTICAL STUDY ABOUT THE RELATION BETWEEN THE QINGHAI-XIZANG HIGH PRESSURE ON THE 100MB SURFACE AND THE FLOOD AND DROUGHT IN EAST CHINA IN SUMMER
    夏季100毫巴青藏高压与我国东部旱涝关系的天气气候研究
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    MEASUREMENTS OF THE GIANT SALT NUCLEI FROM ISLAND TO INLAND AT 30°N IN EAST CHINA
    我国东部(30°N)从海岛到陆地巨盐核观测
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    A STUDY OF THE RELATIONSHIP OF ZONAL WINDS OSCILLATION BETWEEN EAST AUSTRALIA AND NORTHWESTERN PACIFIC TROPICAL AREA
    澳洲东部与西北太平洋热带地区纬向风振动关系的统计研究
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    STUDY OF TEMPERATURE CHANGES AND ENVIRONMENT FOR LAST 500 YEARS IN THE EAST OF NORTHERN XINJIANG
    北疆东部近500年来温度变化及其趋势研究
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  东部地区
    LAND SURFACE PROCESS MODEL (LPM ZD) AND ITS SIMULATION OF LAND SURFACE CHA RACTERISTICS IN EAST CENIRAL CHINA
    陆面过程模式LPM-ZD及其对我国中东部地区陆面特征的模拟
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    SIMULATION OF SUMMER CLIMATE OVER CENTER AND EAST CHINA USING A HIGH RESOLUTION NESTED REGIONAL CLIMATE MODEL
    高分辨嵌套区域气候模式对我国中、东部地区夏季气候的数值模拟
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    Spring Precipitation Reconstructed in the East of the Qilian Mountain During the Last 280 a by Tree Ring Width
    利用树轮宽度重建近280a来祁连山东部地区的春季降水
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    GMS Data-Estimated Surface Net Radiation over East China in Summer
    由GMS资料估算我国东部地区夏季地表净辐射
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    Interdecadal Features of Correlation Between ENSO and Summer Rainfall in East China
    ENSO与中国东部地区夏季降水相关性年代际变化特征
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  “east”译为未确定词的双语例句
    Study on Optimization of the Dust Model System and Quantitative Classification of Dust Events in East Asia
    沙尘模式优化与东亚沙尘天气量化分级研究
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    THE RELATIONSHIP BETWEEN MAY-Y IN FAR EAST AND THE BEHAVIOUR OF CIRCULATION OVER ASIA
    东亚的梅雨期与亚洲上空大气环流季节变化的关系
短句来源
    THE CLIMATIC FRONTAL ZONES OVER EAST ASIA
    东亚的气候鋒
短句来源
    THE MONTHLY MEAN ATMOSPHERIC HEATING FIELDS AND VARIATIONS OF CIRCULATION IN MAY-JULY OVER EAST ASIA
    东亚地区5—7月平均大气加热场和月平均环流变化
短句来源
    THE CLIMATOLOGICALLY SYNOPTIC CHARACTERISTICS OF THE SHEAR LINE ON THE 700mb SURFACE TO THE EAST OF THE QINGHAI-XIZANG PLATEAU
    青藏高原东侧700毫巴切变线的天气气候特征
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  east
Biocycle of nitrogen in a Cyclobalanopsis glauca-dominated evergreen broad-leaved forest in East China
      
The nitrogen (N) cycling was elucidated in a 40-year-old subtropical evergreen broad-leaved forest dominated by Cyclobalanopsis glauca growing on red soil in Zhejiang Province, East China.
      
In November 2003 and June 2004, the insect borers and their spatial distribution within Pinus massoniana were investigated in Zhoushan City, in East China's Zhejiang Province, where pine wood nematode (Bursaphelenchus xylophilus) are typically found.
      
As for the four transect lines, the east and the northeast scored higher in each diversity index than the others due to less human disturbance, gentler topography uplift and more intercepted materials and energies.
      
The genus has three modern distribution centers: South Europe, North America and East Asia.
      
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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。

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。

 
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