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订正     
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  revision
     A TAXONOMIC REVISION OF NUBRA PIKA (Ochotona nubrica Thomas, 1922)
     努布拉鼠兔(Ochotona nubrica Thomas,1922)的分类订正
短句来源
     A Revision and Addition of Oleaceae from Henan
     河南木犀科(Oleaceae)增补与订正
短句来源
     A Revision and Addition of Rubiaceae from Henan
     河南茜草科(Rubiaceae)增补与订正
短句来源
     A Revision of the Genus ROEGNERIA C. Koch of China
     国产鹅观草属ROEGNERIA C.Koch之订正
短句来源
     A Revision and Addition of Polygonum Linn. from Henan
     河南蓼属(Polygonum Linn.)增补与订正
短句来源
更多       
  correction
     Atmospheric Correction of CBERS-02 CCD Image
     CBERS-02卫星CCD图像的大气订正
短句来源
     THE CORRECTION OF Z.NEHARI'S PROOF OF |α_4|≤4
     关于|α_4|≤4的Z.Nehari证明的订正
短句来源
     Atmospheric Correction for AMTIS Based on BRDF Loop and MODTRAN4. 1
     AMTIS大气订正算法——基于MODTRAN4.1与BRDF大气订正
短句来源
     FY-1C VISIBLE CHANNELS' ALBEDO ATTENUATION ANALYSIS AND CORRECTION EXPERIMENT
     FY-1C可见光通道衰减分析及订正试验
短句来源
     A feasible method on atmospheric correction to channel 1 and 2 for MODIS
     MODIS通道1和通道2大气订正的一种快速实用方法
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  a revision
     A Revision and Addition of Oleaceae from Henan
     河南木犀科(Oleaceae)增补与订正
短句来源
     A Revision and Addition of Rubiaceae from Henan
     河南茜草科(Rubiaceae)增补与订正
短句来源
     A Revision of the Genus ROEGNERIA C. Koch of China
     国产鹅观草属ROEGNERIA C.Koch之订正
短句来源
     A Revision and Addition of Polygonum Linn. from Henan
     河南蓼属(Polygonum Linn.)增补与订正
短句来源
     A Revision and Addition of Loranthaceae from Henan
     河南桑寄生科订正与增补
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更多       
  correction experiment
     The Correction Experiment of Atmospheric Effects on NOAA/AVHRR Channel Albedos and Vegetation Indexes
     对NOAA/AVHRR通道反照率和植被指数的大气影响订正试验
短句来源
     FY-1C VISIBLE CHANNELS' ALBEDO ATTENUATION ANALYSIS AND CORRECTION EXPERIMENT
     FY-1C可见光通道衰减分析及订正试验
短句来源
     Correction Experiment on Precipitation Forecast of MM5
     MM5降水预报订正试验
短句来源

 

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  revision
Once More about Hepatoid Circumanal Glands of Dogs; History of Their Discovery and Causes of Revision of Their Structure and Fun
      
The available data substantiate revision of the data on the structure of many skin glandular organs containing atypical sebaceous glands.
      
Revision of the polytypic complex Polyommatus icarus Rott.
      
It includes the revision of T-cell antigen receptor (TCR), which implies the secondary rearrangement of TCR genes in peripheral T-lymphocytes and surface expression of a new antigen receptor with altered specificity.
      
Revision of Phylogenetic Relationships in the Antilopinae Subfamily on the Basis of the Mitochondrial rRNA and β-Spectrin Nuclea
      
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  correction
Using the stretched variable and the method of boundary layer correction, the formal asymptotic expansion of solution is obtained.
      
A nonmonotonic criterion and the second order correction step are used to overcome Maratos effect and speed up the convergence progress in some ill-conditioned cases.
      
From the linearization procedure, we can find a new approach of system identification, which is on-line real-time modeling and real-time feedback control correction.
      
The text area was extracted after preprocessing such as skew correction and marginal noise removal.
      
Then position correction will be done through the control algorithm and servo system.
      
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  a revision
A revision of the local species of sipunculans is performed for the first time.
      
A new species of the genus Caecosagitta has been found in the southwestern Bering Sea and a revision of Sagitta macrocephala has been performed.
      
The formulated new definitions of "granule" and "intergranular lane" require a revision of the previous results.
      
Recoil correction to hydrogen energy levels: A revision
      
New data on the specific heat, thermal expansion, and magnetization of the CaMn7O12 phase require a revision of the current concepts of the sequence of phase transitions in this compound.
      
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  其他


In this paper the turbulent exchange in the surface layer of the stable at-mosphere is discussed.Firstly,taking the effect of thermal stratification onturbulence,we derived a new form of the function of Richardson' number fromthe energy balance equation of the turbulent atmosphere.Secondly,we furtherproposed a reasonable function,which describes the vertical distribution ofelements in the stable atmospheric surface layer.Thirdly,we give some graphswhich allow us to calculate accurately and quickly the turbulent...

In this paper the turbulent exchange in the surface layer of the stable at-mosphere is discussed.Firstly,taking the effect of thermal stratification onturbulence,we derived a new form of the function of Richardson' number fromthe energy balance equation of the turbulent atmosphere.Secondly,we furtherproposed a reasonable function,which describes the vertical distribution ofelements in the stable atmospheric surface layer.Thirdly,we give some graphswhich allow us to calculate accurately and quickly the turbulent characteristicvalues,such as turbulent austousch based onobserved data.For comparison with others,some calculations based on observed data arefurnished.It shows that our treatment is reasonable and our results arebetter than results.

本文对稳定层结大气中近地层湍流的层结订正函数导出了新的形式.据此而对的湍流普遍函数作出了新的规定.根据该方案对近地层湍流特徵作了若干讨论.最后并绘制了计算近地层湍流特性量的图表,藉此可以很方便而准确地由梯度观测直接估各市地近地层湍流状况.

In this paper the process how an unstable growing disturbance stops developing is investigated. The main mechanism to check the development is the feeding-back effect of the unstable disturbances on the basic current. It is shown that the time elapsed for an unstable disturbance to grow to its maximum intensity is roughly proportional to its initial amplitude. For an amplitude of 100 meters the time is about 8 days, and that for an amplitude of 200 meters is about 5 days. Further, in the vorticity and thermodynamic...

In this paper the process how an unstable growing disturbance stops developing is investigated. The main mechanism to check the development is the feeding-back effect of the unstable disturbances on the basic current. It is shown that the time elapsed for an unstable disturbance to grow to its maximum intensity is roughly proportional to its initial amplitude. For an amplitude of 100 meters the time is about 8 days, and that for an amplitude of 200 meters is about 5 days. Further, in the vorticity and thermodynamic equations we keeped the non-linear terms which are generally dropped. This enables us to study the mutual interaction of the disturbances. It is shown theoretically that this mutual interaction is important in the formation of Ω-shaped blocking highs.

本文討論了已經不稳定的扰动如何停止发展。扰动对基本气流作非线性的反馈,使扰动不再能从基本流場得到能量(位能或动能),于是扰动停止发展。在求解扰动涡度方程时,从略去非线性項的解作为第一近似的解代入非綫性項,重新解扰动方程,得到第二近似的解。在起始不长的时間內,第一近似已足够准确,然而时間稍长,則非线性項的訂正起重要的作用,它可以基本上改变了第一近似流場的形式,出現了閉合的高中心及Ω形流場。

In considering the effect of earth's curvature,the author derives appro- ximate formulas of computating radial velocity of upper wind with methods of(h,δ),(h,l)and(r,δ)respectively.It is shown that without considering the earth's curvature,the radial velocity of upper wind computated with method of (h,r) and method of (r,δ) is smaller than the actural value,but the relative error is less than one percent and can be neglected;while the result computated with methnd of(h,δ)is greater than the actural value, and...

In considering the effect of earth's curvature,the author derives appro- ximate formulas of computating radial velocity of upper wind with methods of(h,δ),(h,l)and(r,δ)respectively.It is shown that without considering the earth's curvature,the radial velocity of upper wind computated with method of (h,r) and method of (r,δ) is smaller than the actural value,but the relative error is less than one percent and can be neglected;while the result computated with methnd of(h,δ)is greater than the actural value, and the relative error may amount to about twenty percent.In order to correct this error,a simple nomogram based on the formula derived is given.Besides,without considering earth's curvature,the height of pilot balloon computated with (r,δ) method is considerably less than its true height,for correcting this error,approximate formula and correcting table are introduced.

对(h,δ)、(r,δ)、(h,r)三种方法,考虑地面曲率,导出了计算高空径向风速的近似公式,公式表明,如不考虑地面曲率,用(h,r)法和(r,δ)法计算出来的径向风速偏小,相对误差小于百分之一,可略而不计;用(h,δ)法算出的结果偏大,相对误差可大到百分之二十左右。为了订正这种误差,根据导得的公式给出了一种简单订正图。另外,不考虑地面曲率,用(r,δ)法算出来的气球高度比它高出地面的真正高度要小得多,为了订正这种误差,介绍了误差的近似公式和订正表。

 
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