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
   经度 的翻译结果: 查询用时:1.026秒
图标索引 在分类学科中查询
所有学科
气象学
林业
天文学
自然地理学和测绘学
地球物理学
农作物
船舶工业
力学
工业通用技术及设备
更多类别查询

图标索引 历史查询
 

经度
相关语句
  longitude
     Changes in its body shape in the specific waters(l75°E-172°W,39°N-42°N)tend to increase with the latitude and longitude.
     其形体变化规律在特定的海域(175°E~ 172°W、39°~42°N)有随经度和纬度增加而增大;
短句来源
     3. Fat content of wild type was significantly negatively related to east longitude (r = 0. 8862* * ), and the relationship with the latitude (°N) performed on mono -peak curve manner, the peak region was located at 38°N.
     3.野生型脂肪含量与原产地经度(°E)呈显著负相关(r=-0.8862~(**)),与原产地纬度呈单峰曲线关系,高峰区出现在38°N。
短句来源
     The resolution of the system is that latitude and longitude: 1 milliarcsecond, height: 0.01 m, velocity: 0. 01 m/s.
     接收系统的分辨率:经度和纬度为1marcs,高程为0.01m,速度为0.01m/s。
短句来源
     By employing GIS, VB6 0 and 1km×1km DEM of northeast of China ,1km×1km databases in aspects of longitude、latitude、altitude、slope were established.
     借助GIS平台和DEM数据 ,生成东北地区 1km× 1km经度、纬度、海拔高度、坡度、坡向数据库。
短句来源
     Longitude effect of the S_q variations
     S_q的经度效应
短句来源
更多       
  degree of longitude
     Their regression correlations show that in subtropical evergreen broadleaved forest region, while increasing each one degree of latitude towards north, APE would decrease 25. 28 mm and IM would decrease 3.09; while increasing each one degree of longitude towards east, APE would decrease 5.00 mm and IM would increase 4. 36;
     每向东移动1个经度,APE则降低5.00mm,IM增加4.36;
短句来源
  longitudes
     And the solar active longitudes during the rising phase are determined to be L 220°-300° and L70°-130°.
     并确定了上升期的活动经度:L220°—300°和L70°—130°。
短句来源
     The solar active longitudes of the rising phase are determined which are Ll60°-210° and L50°-90°.
     本文确定了上升相的活动经度:L160°~210°和L50°~90°。
短句来源
     (2) propagating range of the latitudes ( - 60°-+40°) is less than that of the longitudes(>±90);
     (2)传播的纬度范围(-60°—十40°)远比传播的经度范围(<—90°—+90°)小.
短句来源
     The results indicated that the mungbean accessions were distributed in about 28 latitudes and 60 longitudes,and most of them over a area between latitudes 29-41°N and longitudes 107-123°E.
     结果表明:我国绿豆种质资源分布在约28个纬度、60个经度内,其中29~41°N×107~123°E范围内分布最多,占总材料数的75.99%。
短句来源
     (3) The density and tbe flux have minimums at longitudes 120°and 240°, respectively, and have maximums at longitudes 0° when K_≥ 6and have maximums, respectively, at 60°and at 300°when K_p<6.
     O~+离子密度和通量密度分别在经度120°和240°附近最小,K_p≥6时,在经度0°处最大,K_p<6时,分别在经度60°和300°附近最大。
短句来源
更多       
  “经度”译为未确定词的双语例句
     The observed whistler occurrence rates at Wuchang (30.5°N Geog., 114.6°E; 19.3°N Geom) and Kagoshima (31.5°N, 130.8°E; 20.5°N) are in good agreement with the theoretical predictions in this paper.
     武昌(地理30.5°N,114.6°E;地磁19.3°N). 和鹿儿岛(31.5°N,130.8°E;20.5°N)两台站观测到的哨声出现率的经度效应证实了本文的理论预言.
短句来源
     The gene flows (Nm) of cluster analysis for the four factors are 2.880,5.219,2.437, and 1.528 in order and the gene differentiations (Gst) are 0.148, 0.087, 0.170 and 0.247, respectively.
     纬度、经度、空间实际距离及省份进行分群的基因流(Nm)分别是2.880、5.219、2.437、1.528:基因分化系数(Gst)依次是0.148、0.087、0.170、0.247;
短句来源
     05′N to 40? 43′N and 106? 04′ W to 116?
     臭柏分布的范围纬度在 38°05′~43°40′之间,经度在 106°04′~116°34′之间。
短句来源
     80°-160°, 200°, 340° for the scuthern hemisphere and 240°-280°, 340°-360° for the northern hemisphere.
     北半球活动较强的黑子群主要集中在240°-280°和340°-360°经度带。
短句来源
     Based on the data of whistle observations at Hefei (37.73°N, 117.15°E, Geograph.; Geomagnetic latitude 20.60°N), the raising factor, absorption coefficient and lifetime of ducts of whistles around sunset are analized and calculated.
     本文根据1986年初合肥地区(地理纬度31.73°N,经度117.15°E;地磁纬度20.60°N)哨声观测资料,分析和计算了日落哨导管的抬升因子、吸收系数和导管寿命.
短句来源
更多       
查询“经度”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。
  longitude
Historical forest fire records from Alaska State (1950-2000), California State (1895-2001), USA and Heilongjiang Province (1980-1999), China were used to calculate the longitude and latitude of the annual burned area's centroids for these regions.
      
The fluctuation of the burned area's centroids in Alaska State and California State in longitude has obvious periodicity, and the periodicities are 4.2 years, 6.25 years in Alaska State and 6.24 years, 106 years in California State.
      
The fluctuation of the burned area's centroids in Heilongjiang Province has a periodicity both in longitude and latitude, and the periodicities are both 3.3 years, 6.67 years.
      
soongorica are not significantly correlated with altitude, latitude or longitude, and a spatial distribution trend of d13C values of R.
      
On the basis of the same data, a strong longitude effect in the N(He++) concentration occurring under certain heliogeophysical conditions is discovered, an effect amplitude attaining one order of magnitude on adjacent orbits.
      
更多          
  degree of longitude
A degree of longitude is some 20 percent shorter in Acadia, Maine than in Everglades, Florida.
      
The formula comes from assuming a second order polynomial, and regressing the length of a degree of longitude at a given latitude on latitude.
      
The data contain measurements from the Australia coastline at every half-degree of longitude and latitude.
      
  longitudes
Leaves and soil samples were simultaneously collected from the ten major distribution areas in Northwest China at altitudes from 394 m to 1 987 m above sea level, at latitudes from 36°10'N to 44°33'N, and at longitudes from 81°43'E to 106°37'E.
      
The most intense electron fluxes are observed at the lower edge of the near-equatorial boundary of the inner radiation belt on longitudes of the South Atlantic Anomaly between 14 and 20 h MLT.
      
It is demonstrated that the simulation result correctly reproduces the AMS data, and differences in spectra averaged over longitudes on various magnetic latitudes are small (including the low-energy range) for different models of the magnetosphere.
      
The sole spectral feature in the near infrared, observed at some longitudes, is a possible pyroxene absorption band at 0.95 μm, which can be used to investigate the abundance and distribution of FeO in the regolith.
      
A shift in the position of an activity maximum for smaller masses in the direction of lower solar longitudes is confirmed for the Geminids.
      
更多          


1. In order to study the distribution of the two species of bedbugs,Cimex lectularius and C. hemiptera, 81 representative localities of 23provinces and Inner Mongolia were selected for the collection ofbedbugs.2. Among the 81 localities, 55 had only C. lectularius, 11 had onlyC. hemiptera, while the remaining 15 localities had both species.3. Atmospheric temperature forms one of the most important factorslimiting the distribution of bedbugs. Consequently C. hemipteralimits itself in the North at Chian-Yang of...

1. In order to study the distribution of the two species of bedbugs,Cimex lectularius and C. hemiptera, 81 representative localities of 23provinces and Inner Mongolia were selected for the collection ofbedbugs.2. Among the 81 localities, 55 had only C. lectularius, 11 had onlyC. hemiptera, while the remaining 15 localities had both species.3. Atmospheric temperature forms one of the most important factorslimiting the distribution of bedbugs. Consequently C. hemipteralimits itself in the North at Chian-Yang of Fukien, Lo-Chang ofKuangtung, Heng-Yang of Hunan, Tsun-I of Kweichow, Ch'eng-Tuof Szechuan and Ya-An of Sik'ang. In these localities the wintertemperature is usually at 4°- 8℃. North of this belt, because thewinter temperature is much lower, the condition is not suitable forthe existence of this species. Cimex lectularius is more resistant tocold. It is, however, less resistant to extreme heat. In localities inSouth China where the summer temperature runs over 30℃, thecondition is not suitable for the survival of this species. Its southernlimit of distribution has been found to be a line connecting Amoy,Chu-Kiang of Kuangtung, Kwei-Lin of Kuangsi, P'ing-T'ang of Kwei-chow and Meng-Tze of Yunnan.4. The relationship of latitude, altitude, atmospheric pressure andhumidity to the biology of bedbugs were briefly discussed.

(一)作者在1950—1951年,曾收集中国81个地区的臭虫标本,作一系统的调查研究,这81个地区包括23省和内蒙古自治区。 (二)在81个地区所采集到的标本,有55个地区只有温带臭虫,44个地区只有热带臭虫,其余15个地区两种臭虫均有发生。 (三)气温是影响臭虫分布的重要因素之一。热带臭虫的分布,北至福建的建阳,广东的乐昌,湖南的衡阳,贵州的遵义,四川的成都(李、孟1951),西康的雅安,这些地区的冬季气温大都在4°—8℃。在这些北分布地区以北的地区,冬季气温较低,大多不适于它的生长,温带臭虫的抗寒力较强,在华北、东北、西北均有发生,它的分布南至福建的厦门,广东的曲江、广西的桂林、贵州的平塘(李、孟1951)、云南的蒙自,这些地区夏季气温均在30℃以下,仍可适于它的生长。 (四)地理上的经度与臭虫的分布并无关系,但纬度与臭虫的分布有关,热带臭虫的分布北至北纬30°41″(成都),它的发生地带以热带为主,在亚热带亦可生长,温带臭虫的分布南至北纬23°25′(蒙自),它的发生地带以亚热带及温带为主但传入部分的热带地区,亦可生长。 (五)地势过高可以影响热带臭虫的发生,在昆明、大理、昭通、丽江等地,拔...

(一)作者在1950—1951年,曾收集中国81个地区的臭虫标本,作一系统的调查研究,这81个地区包括23省和内蒙古自治区。 (二)在81个地区所采集到的标本,有55个地区只有温带臭虫,44个地区只有热带臭虫,其余15个地区两种臭虫均有发生。 (三)气温是影响臭虫分布的重要因素之一。热带臭虫的分布,北至福建的建阳,广东的乐昌,湖南的衡阳,贵州的遵义,四川的成都(李、孟1951),西康的雅安,这些地区的冬季气温大都在4°—8℃。在这些北分布地区以北的地区,冬季气温较低,大多不适于它的生长,温带臭虫的抗寒力较强,在华北、东北、西北均有发生,它的分布南至福建的厦门,广东的曲江、广西的桂林、贵州的平塘(李、孟1951)、云南的蒙自,这些地区夏季气温均在30℃以下,仍可适于它的生长。 (四)地理上的经度与臭虫的分布并无关系,但纬度与臭虫的分布有关,热带臭虫的分布北至北纬30°41″(成都),它的发生地带以热带为主,在亚热带亦可生长,温带臭虫的分布南至北纬23°25′(蒙自),它的发生地带以亚热带及温带为主但传入部分的热带地区,亦可生长。 (五)地势过高可以影响热带臭虫的发生,在昆明、大理、昭通、丽江等地,拔海高度均在1922米以上,热带臭虫并无发生,但对温带臭虫并不影响。 (六)气压与地势的高低有关,昆明、大理,昭通、丽

Integrating with respect to time the equation for the balance of angular momentum of the atmosphere north of certain latitude (30°N say)we obtainIn the above equation ρ is thedensity; (?), the zonal wind; v, the meridional wind; R, the earth's radius; Ω, the angular speed-of the earth's rotation; dm, the mass element of the atmosphere; dτ, the volume element; ds, the area element on the earth's surface, and dσ, the urea element on the vertical surface over the latitudial circle of 30°N. The first two terms (in...

Integrating with respect to time the equation for the balance of angular momentum of the atmosphere north of certain latitude (30°N say)we obtainIn the above equation ρ is thedensity; (?), the zonal wind; v, the meridional wind; R, the earth's radius; Ω, the angular speed-of the earth's rotation; dm, the mass element of the atmosphere; dτ, the volume element; ds, the area element on the earth's surface, and dσ, the urea element on the vertical surface over the latitudial circle of 30°N. The first two terms (in the parenthesis) On the left side of (2) are evaluated from the mean westerlies in summer and winter given by Mintz. The last two terms on the left and the first two terms on the right side of (2) are evaluated from the mean surface pressure charts of July and January. The transfer of angular momentum across latitude 30°N given by Starr and White is used to evaluate the 3rd. term on the right. Then the value of the last two terms in the parenthesis on the right of (2) is calculated. The result agrees very well with that obtained by other authers.It is further found that: 1. From summer to winter the transfer of angular momentum from low to high latitudes by gross weather systems overcompensates the destruction by the earth's surface. The small residue of these two factors acounts for the main part (about85%)of increase of westerly circulation from summer to winter. The remaining small part of the increase of the westerly circulation may be acounted for by the advection of mass of the atmosphere, which carries the angular momentum due to earth's rotation (difference between the first two terms on the right and the last two terms on the left side of (2)).2. The transfer of angular momentum or the destruction of angular momentum, as well as the intensity of the westerly circulation has annual variation. However this annual variation is not of sine or cosine type, i,θ, the variation from summer to winter is not the opposite of that from winter to. summer. The property of this asymmetry is explained by the irreversible heat addition and subtraction. From winter, to summer heat is added to, and summer to winter heat is subtracted from the atmosphere (N.H.). Since the process of adding and subtracting heat is irreversible, the variation from summer to winter can not be symmetric to that from winter to summer.3. Transfer of angular momentum from easterlies to westerlies occurs mainly in the period of breakdown of zonal circulation (low index), mainly in the belt of longitudes of"extended troughs" (troughs extending from high to low latitudes) and "extended ridges" (ridges extending from low to highlatitudes), and mainly in the high levels of the atmosphere.

把30°N以北大气角動量平衡方程由七月積分到一月,則其中各項都可計算:此緯度以北大气相对西風角動量的改变可用Mintz平均西風冬夏分佈圖算出;地轉角動量的改变可用冬夏地面平均气压圖算出;通过30°N緯度的角動量的渦動輸送已为Starr和White算出,因此利用積分結果可求得30°N以北地面应力和山脈东西兩側气压差所引起的角動量消耗,結果与别的作者用别的方法所得數值極为符合。 作者更指出: 1.从夏到冬大型天气系統的角动量輸送勝过地面摩擦的消耗,从夏到冬西風环流增强的主要部分(約85%)即由於二者之差,西風环流增强的其餘一小部分則由於大气的質量平流,而引起地轉角動量的傳送。 2.角動量的输送,角動量的消耗以及西風环流强度都有年变化。但这种年变化並非正餘弦型,即从夏到冬的变化並不正是从冬到夏变化的反面,此种非对称性可由加熱过程和减熱过程的不可逆性解釋。在北半球从冬到夏对大气來说是加熱的,而从夏到冬大气失去熱量,因为加熟过程和減熱过程都不是可逆的,故从夏到冬的变化也不与从冬到夏的变化对称。 3.东風帶向西風帶的角動量輸送,主要發生於西風环流破坏的時候;主要發生於“引伸槽”和“引伸脊”的經度帶;同時也主要發生於大气的...

把30°N以北大气角動量平衡方程由七月積分到一月,則其中各項都可計算:此緯度以北大气相对西風角動量的改变可用Mintz平均西風冬夏分佈圖算出;地轉角動量的改变可用冬夏地面平均气压圖算出;通过30°N緯度的角動量的渦動輸送已为Starr和White算出,因此利用積分結果可求得30°N以北地面应力和山脈东西兩側气压差所引起的角動量消耗,結果与别的作者用别的方法所得數值極为符合。 作者更指出: 1.从夏到冬大型天气系統的角动量輸送勝过地面摩擦的消耗,从夏到冬西風环流增强的主要部分(約85%)即由於二者之差,西風环流增强的其餘一小部分則由於大气的質量平流,而引起地轉角動量的傳送。 2.角動量的输送,角動量的消耗以及西風环流强度都有年变化。但这种年变化並非正餘弦型,即从夏到冬的变化並不正是从冬到夏变化的反面,此种非对称性可由加熱过程和减熱过程的不可逆性解釋。在北半球从冬到夏对大气來说是加熱的,而从夏到冬大气失去熱量,因为加熟过程和減熱过程都不是可逆的,故从夏到冬的变化也不与从冬到夏的变化对称。 3.东風帶向西風帶的角動量輸送,主要發生於西風环流破坏的時候;主要發生於“引伸槽”和“引伸脊”的經度帶;同時也主要發生於大气的高層。

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...

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经度的内容
在知识搜索中查有关经度的内容
在数字搜索中查有关经度的内容
在概念知识元中查有关经度的内容
在学术趋势中查有关经度的内容
 
 

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