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   穿透对流 的翻译结果: 查询用时:0.474秒
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穿透对流
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  “穿透对流”译为未确定词的双语例句
     The punctuated turn over and avalanche effect in phase transition layer may play a key role for the resurfacing and lithosphere foundered of Venus in 500 Ma intervals.
     金星地幔相变边界层的穿透对流可能是推动其表层岩石层全球性更新的关键,导致其表层火山活动和地表构造以大致500 Ma时间间隔更新和重造.
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  相似匹配句对
     A STATISTICAL THEORY OF THE NON-LOCAL CONVECTION
     非局部的对流理论
短句来源
     Determination of Cooling Curve at Convection
     对流冷却的测定
短句来源
     oxidation and penetration of separator;
     隔膜的氧化和穿透
短句来源
     The Penetration of X-Rays
     X射线的穿透深度
短句来源
     A quasi-linear parameter estimation method based on convection-dispersion equation is proposed to determine the parameters of solute transport in porous.
     拟线性化方法是基于溶质运移“穿透曲线”(BTC)数据估计对流-弥散方程(CDE)中运移参数。
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  penetrative convection
Penetrative convection in the isothermally incompressible fluid approximation
      
The onset of penetrative convection in an infinite horizontal fluid layer bounded by isothermal rigid or free nondeformable surfaces is numerically examined.
      
The results are compared with those previously obtained for the equations of penetrative convection in the Boussinesq approximation.
      
The waves are generated via a mechanism related to the loss of stability and periodic separation of the upper, heavier and cooler liquid layer (penetrative convection).
      
Penetrative convection in thawing subsea permafrost
      
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This paper utilizes the real sounding data of the south China to comp- ute the space-time distribution of the new potential pseudo-equivalent temperature. The results show that the term of latent teat of waterdroplets freezing exists a zero-contribution height in the atmosphere; the net contribution of it on θ_(sc) is 3. 1K in average, with a maximum of 3.8K, with the contribution or specific heat of the water substances, the total increment is 5.1 K in ordinary, with a maximum of 6.4K, both the terms heat is...

This paper utilizes the real sounding data of the south China to comp- ute the space-time distribution of the new potential pseudo-equivalent temperature. The results show that the term of latent teat of waterdroplets freezing exists a zero-contribution height in the atmosphere; the net contribution of it on θ_(sc) is 3. 1K in average, with a maximum of 3.8K, with the contribution or specific heat of the water substances, the total increment is 5.1 K in ordinary, with a maximum of 6.4K, both the terms heat is able to increase the atmospheric latent instability, potential convection depth and net bouyancy force of convection system, and the atmospheric apparent heights which penetrative convection can reach. This temp- erature can be used in the both operational application and theoretical research on the convection and the cumulus development.

本文利用华南实际探空资料计算了新假相当位温的时空分布,结果表明,水滴冻结潜热项在大气中存在零贡献高度,它对θ_se的净贡献,平均达3.2K,最大达3.9K,加上水质物比热的贡献,两项台计通常可达5.2K,最大达6.7K,两项热量都可增加大气中的不稳定性,增加大气的潜在对流深度,增加对流系统的净浮力,使穿透对流能够到达视高度,这种温度可用于对流和积云发展的业务应用和理论研究。

Venus' mean surface age suggests that there may have extensive resurfacing of Venus prior to that epoch.Such global resurfacing is relative with the thermal evolution in the interior.Base on the properties and parameters of the Venus and the theory of mantle convection,we calculate the thermal evolution history of Venus.The results show that Venus' thermal evolution is a non-monotonic cooling process.In this process,Venus' mantle convection displays an overturn with a quasi-periodicity.Because of the different...

Venus' mean surface age suggests that there may have extensive resurfacing of Venus prior to that epoch.Such global resurfacing is relative with the thermal evolution in the interior.Base on the properties and parameters of the Venus and the theory of mantle convection,we calculate the thermal evolution history of Venus.The results show that Venus' thermal evolution is a non-monotonic cooling process.In this process,Venus' mantle convection displays an overturn with a quasi-periodicity.Because of the different parameters,the stales of mantle overturn may appear in three modes.The punctuated turn over and avalanche effect in phase transition layer may play a key role for the resurfacing and lithosphere foundered of Venus in 500 Ma intervals.

金星表层年龄和构造活动特点表明其岩石层在最近的地质历史时期经历过广泛的更新.这种全球性的表层改造与其内部热演化历史进程密切相关.如果金星存在相变形成的上、下地幔,依据现今所了解的金星物理性质和参量化的热对流理论,并且考虑金星地幔相变边界层状态对对流的控制作用,我们计算了金星热演化历史.结果表明,金星的热演化历史是一种非单调的冷却过程,在这种非单调的热演化历史进程中,金星地幔会出现大体等周期的翻转.由于参数选取的不同,翻转时金星上、下地幔的温差随时间可能出现稳定变化、逐渐加强、逐渐减弱三种不同演化模式,目前尚不能确定实际金星热演化历史究竟是哪一种模式.金星地幔相变边界层的穿透对流可能是推动其表层岩石层全球性更新的关键,导致其表层火山活动和地表构造以大致500 Ma时间间隔更新和重造.

 
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