advection中文是什么意思

• n.
  (热的)对流；(空气的)平流。
  adj.
  -vective
  

• advection cooling    平流冷却
• advection fog    海面雾; 平另; 平流雾
• advection heat    对流热
• advection inversion    平流逆温
• advection layer    平流层; 平流运动层
• advection of heat    平流热效
• advection region    平流区
• ageostrophic advection    非地平流
• cold advection    冷平流
• differential advection    差异平流
• geostrophic advection    地转平流
• horizontal advection    水平平流
• temperature advection    温度平流
• thermal advection    热平流; 温度平流
• thickness advection    厚度平流
• vertical advection    垂直平流
• vorticity advection    涡度平流
• warm advection    暖平流
• advection radiation fog    平流辐射雾
• cyclonic vorticity advection    气旋式涡度平流
• differential thermal advection    差异热平流
• geostrophic advection scale    地转平流尺度
• thermal vorticity advection    热成涡度平流; 热力涡度平流
• advectio    平流
• advect    平流传送; 平流输送; 平流运送
• advcms    腺病毒染色体变更位点

• Then we come to the nonlinear advection - dominated transport problem , only the one - dimensional case is discussed . it is shown that the unknown c and the adjoint p are optimally approximated when it is discretized with the lowest order mixed finite element space
  扩散项均为非线性的情形，对一维问题采用零次混合元空间进行离散，得到了l ~ 2范数意义下关于c ， p的最优误差估计。
• The azimuthally linear advection may results in that the meso - scale vortex of initially circular shape becomes the elongated and spiral vorticity bands ; the radial linear advection may transfer the vorticity of the outer region towards the center of the typhoon
  沿e方向的线性平流可使初始圆形的中尺度涡旋演变为狭长的螺旋状的涡量带;沿径向线性平流的引进可使外区涡量向台风中心方向传播。
• The radial advection of vorticity plays a major role in the inward - propagation process of vorticity , and the nonlinear advection of perturbation vorticity may enhance the inward - propagation of vorticity , which results in the locally strengthening of the typhoon circulation
  径向平流在涡量内传过摘要程中起主要作用，扰动涡量的非线性平流可以加强涡量内传。内传的涡量可以引起台风局域加强。
• By solving the 2 - d viscous navier - stocks equation , the flow field of the microjet was simulated . the results clearly reveal the features of microjet and the process of vortex pairs ? formation , advection , diffusion and entrainment effection on ambient fluid
  结果清晰的反映了作动器出口附近微射流场的形态，同时也再现了此区域内旋涡对的生成、迁移和扩散过程以及微射流对周围流体的卷吸作用。
• The variances of the apparent heat source , apparent moist sink and the heavy rainstorm are well coupled . the time the maximums of them appeared is quite accordance ; the vertical advection term is the main contributor of the apparent heat source and apparent moist sink
  视热源、视水汽汇的变化和暴雨的演变之间存在较强的耦合，两者的极值出现的时间十分一致；垂直平流项是视热源、视水汽汇三个分量中的主要贡献者。
• We make a diagnostic analysis about the evolution and distribution of the wet potential vorticity of the integral result of the model simulation at each time . we find that the explosive of the cyclone has a closely relationship with the advection of the potential vorticity
  从气旋发展过程中的位涡着手，对模式积分结果的各个时次的湿位涡的空间分布和随时间的演变进形了诊断分析，得出：气旋的爆发与位涡的平流关系密切。
• For the advection - dispersion model of one - dimensional reaction solute transport through soils with depth - dependent first - order degradation and depth - dependent linear equilibrium sorption under steady state flow , the numerical model is established by characteristic finite element method
  对于稳态水流条件下，同时考虑随深度变化的一阶降解和随深度变化的线性平衡吸附时，一维反应溶质运移的对流-弥散模型，建立了相应的特征有限元数值模型。
• The quasi - geostrophic process was diagnosed for a case of severe cold air breakout under the blocking situation during 16 - 18 march of 1998 . the attention was focused on the relationship between the surface anticyclone and 500hpa blocking high . the results indicate that the cold outbreak is associated with the adjustment of blocking situation in the ural area , i . e . the collapsing and rebuilding of the ural mountain blocking high . the temperature advections in the lower troposphere shown that the polar cold air invading from the northwest caused the ural blocking high collapsed , and a new ridge developed rapidly was due to the warm advection on the southwestern side which led to the ural blocking high rebuilt . in addition , the distribution of the vertical motion on 700hpa shown that the surface high splitting was related to the considerable upward motion located on the southeastern part of surface high
  对1998年3月中旬一次高空阻塞形势下强冷空气过程进行了诊断分析，着重讨论强冷空气爆发前后地面反气旋活动与高空阻塞形势调整的关系。研究结果表明，强冷空气的爆发与乌拉尔地区阻塞形势的调整阻塞高压的崩溃和重建紧密相关。对流层下部的温度平流分析表明，阻塞形势的调整是由于阻塞高压上游西北方有冷空气侵入导致了阻塞高压的崩溃，而上游来自西南方向的强暖流则导致高压脊迅速发展，使阻塞高压重新建立。
• The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ; the subsidence flow at the middle and low tropospheric levels is favorable for the setting - up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region ; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event ; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation
  结果表明：在中高层暖性高压脊及地面变性冷高压稳定维持的大尺度背景条件下，地表净辐射引起的近地层冷却是大雾过程的触发和加强机制；中低空下沉气流的存在有助于近地层的弱风条件和稳定层结的建立；低层暖平流的输入和边界层的浅层抬升是大雾长时间持续的原因；伴随冷空气南下的偏北大风是驱使大雾消散的动力因子。
• As we all know , the heat transfer of geothermal heat exchanger ( ghe ) is affected by a lot of factors , where groundwater advection has a comparatively great impact indicated by experimental data . while almost all the design tools for ghe are based on principles of heat conduction and rely on some estimate of the ground thermal conductivity and volumetric specific heat . however , the large part of vertical u - type pipe lies in the saturated soil , especially in zones along the coast or with plentiful groundwater , which will be affected by groundwater advection greatly
  但是对于垂直u型埋管来说,管段大部分位于土壤饱和区内,实际上其穿透的地层中总是存在着地下水的渗流,尤其是在沿海(河、湖泊)地区或地下水丰富的地区,埋管的传热性能大部分都受到地下水渗流的影响,此时土壤内发生的是热传导和地下水渗流共同作用下的复杂的、非稳定的传热传质过程(简称热渗耦合传热过程) 。

• advectionとは意味：{名} : 移流｛いりゅう｝