对流不稳定的英文

• conbective instability
• convectional instability
• convective instability
• potential instability

• "对流"英文翻译    convection; convection curre ...
• "不稳定"英文翻译    instability; unstabitily; sw ...
• "对流不稳定性" 英文翻译 :    convective instability
• "对流不稳定性判据" 英文翻译 :    convective instability criterion
• "自动对流不稳定" 英文翻译 :    autoconvective instability
• "束电流对流不稳定性" 英文翻译 :    beam current convective instability
• "滑流不稳定性" 英文翻译 :    slipstream instability
• "气流不稳定性" 英文翻译 :    flow instability; instability in flow
• "双流不稳定性" 英文翻译 :    two-stream instability
• "水流不稳定性" 英文翻译 :    flow instability
• "尾流不稳定性" 英文翻译 :    wake instability
• "非定常流不稳定流" 英文翻译 :    unsteady flow
• "风洞气流不稳定性" 英文翻译 :    instability in tunnel
• "对流性不稳定度" 英文翻译 :    conventional instability
• "离子声电流不稳定性" 英文翻译 :    ion-acoustic current instability
• "双流不稳度" 英文翻译 :    two-stream instability
• "电感量不受电流不稳定所影响" 英文翻译 :    constant inductance with current variation
• "各向异性等离子喷流不稳定性" 英文翻译 :    anisotropic plasma jet instability
• "不稳定" 英文翻译 :    instability; unstabitily; swinging; astable; unsteadiness
• "对流稳定" 英文翻译 :    convectional stability
• "对流稳定性" 英文翻译 :    convective stability
• "不稳定风；不稳定气流" 英文翻译 :    u teady wind; u teadywind
• "摆动，犹豫、不稳定" 英文翻译 :    wobble
• "波动不稳定" 英文翻译 :    oscillating unsteady flow
• "不稳定，动荡" 英文翻译 :    instability

• The weakest convective instability is at the occluded stages of cyclone
  气旋锢囚期对流不稳定最弱。
• In the violent stages of development of cyclone , the convective instability becomes weak greatly
  在气旋强烈发展期对流不稳定大大减弱。
• The north of the low - layer of rain belt was mainly convection instability . so the northern inertia - gravity wave was not easy to develop and to spread
  雨区的北部低层以对流不稳定为主，因此向北的重力惯性波不易发展传播。
• In a word , convective instability strong baxoclinicity barotropic advection of potential vorticity and latent heat release are factors which activize this explosive development of cyclone
  总之，对流不稳定、强斜压性和正压位涡平流、潜热释放是本次气旋发展的启动因子。
• At the same time , the disturbance of the low - level jet might be the triggering condition for heavy rain . but the surface occluded front crossing qinling mountains and strengthening , maybe the direct reason
  同时，由于冷空气是从中层侵入西北地区东部，这样就形成了较强的对流不稳定层结，有利于对流降水的发生。
• So we found that convection instability could inspire inertia - gravity wave . symmetry instability was benefited for spread of inertia - gravity wave and further influenced the development and motion of precipitation
  可见对流不稳定可激发重力惯性波，对称不稳定可使重力惯性波发展与传播，从而影响到降水的发展与活动。
• By the analysis of the relationship among convective instability , symmetric instability and snowstorm , we found that the convective instability level is under 800hpa . snow belt is located in the negative value region of moist potential vorticity and verified the theory of symmetric instability
  最后分析了这场暴雪中西北和东北地区的对流和对称稳定度，个例分析表明，暴雪产生在低层对流不稳定的情况下。
• It is the important mechanism that middle - level dry and cold air current sunk , low - level warm and wet air current ascended . level direction energy sharp section is important to blaze middle scale hypo - circumfluence . severe convection weather was brought by layer - knot latent instability
  上层干冷、下层暖湿的位势不稳定层结可以使对流层中低层出现明显的逆温层，有利于不稳定能量积累，此次天气过程产生的对流不稳定能量大，形成的上升气流深厚。
• We analyzed the meso - scale disturbance field and found that the development and spread of inertia - gravity wave had a close relationship with the development and spread of the rain belt . at the initial stages of precipitation , convection instability was strong in the low level above rain region . convection instability could inspire inertia - gravity wave
  对中尺度扰动场分析发现重力惯性波的发展和传播与雨带的发展与传播有密切的联系：在降水初期，雨区上空低层的对流不稳定较强，对流不稳定可激发出重力惯性波。
• The result indicates that , in the course of the rainstorm in huoshan , there are obvious low - level jet of great intensity , infection of mesoscale shear line , enhancement of plus vorticity which increases intensity of convergence , improves ascending velocity and brings on precipitation , and quick enhancement of helicity which provides the basis to forecast , in addition , convergence of moisture flux and analyzed potential vorticity which reflects baroclinic convective instability sufficiently indicate the characteristics of the rainstorm
  结果表明：此次霍山暴雨发生前后，存在明显的大强度低空急流，并受到中尺度切变线的影响，而且正涡度的加强引起了辐合加剧，提高了上升速度从而引起降水，同时暴雨发生前螺旋度的迅速增强，也为预报提供了根据，另外水汽通量的辐合以及分析位涡反映出的斜压对流不稳定都充分体现了这次降水的特点。

• 对流不稳定的日语：たいりゅうふあんてい