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surface heterogeneity中文什么意思

發(fā)音:   用"surface heterogeneity"造句
  • 表面不均勻性
  • 表面不勻性
  • 表面多相性
  • surface:    n. 1.表面;地面;水面;廣場(chǎng),空地。 2.外觀,外表 ...
  • heterogeneity:    n. 1.【生物學(xué)】異質(zhì)性。 2.【化學(xué)】不均勻性。 3 ...
  • heterogeneity:    n. 1.【生物學(xué)】異質(zhì)性。 2.【化學(xué)】不均勻性。 3.【數(shù)學(xué)】不純一性。
  • allelic heterogeneity:    等位異質(zhì)性
  • antibody heterogeneity:    抗體不均一性
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例句與用法

  1. Could be two scales for the adjustment process . results show that , qualitatively , the larger scale of surface heterogeneity , the higher value of dimensionless kinetic energy
    此2個(gè)特征量與地面非均勻性尺度的定性關(guān)系是,非均勻性尺度越大,過渡時(shí)間
  2. The result is as following . ( 1 ) the appearance of heterogeneity can be observed widely in nature . the surface heterogeneities have different impacts on the estimation of area - averaged flux for different parameterization schemes
    結(jié)果表明: ( 1 )地表的非均勻性是普遍存在的,對(duì)不同的地表通量參數(shù)化方案來說,地面非均勻性對(duì)對(duì)網(wǎng)格區(qū)面積平均通量計(jì)算的影響程度可能不同。
  3. Wavelengths or scales of surface heterogeneity are less than 20km . simulation results show that cbls do reach a quasi - stationary state correspondent to specified surfaces , after a long enough evolution . in this transition process and after that , horizontal statistics , i . e . mean potential temperature and vertical heat - flux , show profiles little differences to those over homogeneous flat surface . main effect of surface heterogeneity is to increase kinetic energy in cbl and the increase concentrates in the direction of surface heterogeneity . the time of cbl spent to reach its first peak of mean kinetic energy ,
    模擬結(jié)果表明,在充分長(zhǎng)的時(shí)間后,邊界層達(dá)到一種適合于地面條件的準(zhǔn)定常態(tài)。這種準(zhǔn)定常態(tài)和向其過渡的過程中,水平平均的邊界層廓線性質(zhì),如平均位溫廓線垂直熱通量廓線等幾乎與平坦均勻地面的結(jié)果相同,或差異極小。地面非均勻性的主要作用是使邊界層動(dòng)能增大,并以地面非均勻性變化方向的動(dòng)能增加為主。
  4. Hi this paper , firstly , a preliminary theoretically analysis of the possible impact of sub - grid land surface heterogeneity on model results is carried out . and then on the basis of calculation with the numerical modeling and the observed data respectively , we discussed the basic characteristics of the influence induced by most sub - grid scale landscape heterogeneities on the estimation of the land surface flux
    本文首先從理論出發(fā)分析了陸面次網(wǎng)格非均勻性對(duì)區(qū)域(大尺度模式網(wǎng)格尺度)通量計(jì)算存在的影響及原因,繼而以數(shù)值模擬計(jì)算和實(shí)測(cè)資料計(jì)算初步討論了不同氣象要素次網(wǎng)格尺度的非均勻性分布特征及對(duì)模式地表各通量計(jì)算的影響特點(diǎn)。
  5. In the numerical models studies , it is necessary to estimating the area - averaged flux of a grid including many kinds of surface types . due to different scales of land surface spatial heterogeneity , there is a considerable debate , however , over the influence of sub - grid scale land surface heterogeneity on the computation of all grid - scale flux between the land surface and atmosphere , and over the necessary to parameterize all types of the influence induced by land surface heterogeneities
    在數(shù)值模式研究中,需要確定包含了各種陸面類型的某一區(qū)域的平均通量,而真實(shí)的自然陸面具有多重尺度的非均勻性,次網(wǎng)格非均勻分布對(duì)地氣之間的各類通量計(jì)算的影響到底有多大,是否要對(duì)所有的非均勻性的影響都要考慮等都有進(jìn)一步研究的必要。

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