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
   (integrated 的翻译结果: 查询用时:0.198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
 

integrated
相关语句
  相似匹配句对
     The integrated O. D. (I.O.D.)
     在IBAS图象分析仪上,测量各杂交点自显影曝光斑的积分光密度值(I.O.D.)
短句来源
     Integrated coverage
     综合信息
短句来源
查询“(integrated”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。
  integrated
CHEMICAL GENOMICS FOR FASTAND INTEGRATED TARGET IDENTIFICATION AND LEAD OPTIMIZATION
      
The device has been fabricated using standard integrated circuits processing methods combined with the Micro-Electro-Mechanical Systems process.
      
An integrated approach to modeling and adaptive control
      
The modeling and real-time feedback control have been integrated in the identification approach, with the parameter adaptation model being abandoned.
      
The objective of this paper is to introduce the approach of integrated modeling and control.
      
更多          


The single-electron wave function of the ground state of the helium atom is obtained from Hylleraas' well-known wave function by integrating the latter over the coordinates of one electron. The energy of the ground state calculated with this one-eleetron wave function is -5.717Rh. compared with the value -5.755 given by the seif-consistant field solution.

将Hylleraas 氏之著名波动函数对一个电子之各座标积分之,吾人求得正常状态氦单一电子之波动函子。由此单一电子波动函数所求得之正常状态能量为-5.717h较自身一致场的解法所求得之值-5.755Rh为大。

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...

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。

In 1st part of this paper,we have calculated the distribution of the mean heat sources and sinks in lower troposphere.The Local change of the mean temperature,or the 1000—500mbthickness h,isAssuming a steady state,and taking mean over the range of integration,we obtain.where Q is the heat gained or lossed by ùnit mass of air in unit time.ω=dp/dt is the verticalvelocity,(?),as a constant, p_0=1000 mb,(?)=500 mb,m represents the meanover 1000—500 mb.Using the mean charts of 1000—500 mb thickness and 700 mb topography,we...

In 1st part of this paper,we have calculated the distribution of the mean heat sources and sinks in lower troposphere.The Local change of the mean temperature,or the 1000—500mbthickness h,isAssuming a steady state,and taking mean over the range of integration,we obtain.where Q is the heat gained or lossed by ùnit mass of air in unit time.ω=dp/dt is the verticalvelocity,(?),as a constant, p_0=1000 mb,(?)=500 mb,m represents the meanover 1000—500 mb.Using the mean charts of 1000—500 mb thickness and 700 mb topography,we can calculatethe 1st term of(2)by geostrophic approximation.(Fig.5—6)Vertical velocity at 500 mb surface is calculated by the mean divergence at 1000 mb and 500mb surface with due consideration to the sloping current due to earth's topography,assumingthat ω is linearly decreasing along vertical,we can obtain the mean vertical velocity ω_m(Fig.3—4).The 1000 mb divergence is calculated from the mean surface vector wind,and the 500 mbdivergence,as follows:Introducing the vertically integrated wind velocity components(?)To the steady state tendency equation,we obtain(?)where w_0 is the surface vertical velocity.(?) and (?) are used as mean wind components at 500 mbsurface.Mean 500 mb divergence is then calculated from the mean 500 mb topography,meansurface pressure and mean w_0 due to earth's topography.(Fig.1—2)The hemispheric mean charts of heat sources and sinks in lower troposphere for Jan.andJuly are given as Fig.7 and Fig.8 respectively.From the numerical calculations,it is found that the 2nd term of(2)is as important asthe 1st term,especially in summer season.Qualitative discussion on the formation of the heat sources and sinks in terms of heat energyof condensation,sensible heat and radiation is given.Finally,a detail comparision of present results with those of others is made.

在本研究题目的第—部分中,作者由热量方程利用高空温压场和表面风的平均资料,计算了北半球1月和7月对流层下半部热源和热汇的分布,并讨论了它们的地理分布的特点。作者利用辐射、凝结和湍流等加热过程来解释热源和热汇的分布情况。并将热源和热汇的水平分布图和沿纬圈方向的平均值,与过去其他人的工作在源汇强度和分布形势上予以详细比较。

 
<< 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(integrated的内容
在知识搜索中查有关(integrated的内容
在数字搜索中查有关(integrated的内容
在概念知识元中查有关(integrated的内容
在学术趋势中查有关(integrated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