环流的

Though often co-mingled, wave power is distinct from the diurnal flux of tidal power and the steady gyre of ocean currents.

虽然常常易混淆，但海浪能与潮汐力的每日涨落变化和海洋流稳定的环流是不同的。

The result shows that both the typical hail process occured at afternoon in early summer when hailstone occured easily and formed under the influence of the Mongolian cold vortex and the circulation background that high pressure at west of Ningixa and low pressure at east of Ningixa.

结果表明：两次冰雹天气过程均发生在宁夏冰雹易发期夏初季节的午后，是在"西高东低"有利于强对流天气发生的环流背景下，受蒙古冷涡影响而形成的。

Numerical results show that the major change is the environmental circulation of tropical cyclone when the surges immerge into the outmost of the tropical cyclone.

通过研究冷暖空气对热带气旋发展影响的试验发现，冷暖空气在入侵热带气旋外围时，最主要改变的是外围的环流场。

Bring about air temperature of plain change area the reason of unusual change is very much, the sea expresses Pacific Ocean of equatorial middle east temperature is unusual on the high side the on the high side that can cause this area air temperature northing of high pressure of; South Asia and intertropical Pacific Ocean sea lifts lukewarmly on the west , through the influence subtropic circle system all can cause on the high side of air temperature of plain change area .

导致川渝地区气温异常变化的原因很多，赤道中东太平洋海表温度异常偏高会引起该地区气温的偏高；南亚高压北进以及热带西太平洋海温的升高，通过影响副热带环流系统均会造成川渝地区气温偏高。

When the jet stream over Japan disappears and easterly wind be-...

这种在亚洲上空出现的大气环流季节变化，在年与年之间，虽然在时间上有一些出入，但变化的型式却是一致的。

When the jet stream over Japan disappears and easterly wi...

这种在亚洲上空出现的大气环流季节变化，在年与年之间，虽然在时间上有一些出入，但变化的型式却是一致的。

The fifth-generation NCAR/Penn State nonhydrostatic dynamics mesoscale model is used for the numerical study of the sea land breeze.

通过对计算结果的分析，研究了不同的海岸带下垫面特性对于海陆风环流流场的影响。

A numerical study of the along-line variability of a frontal squall line during PRE-STORM.

利用 PRE-STORM 期间在85年6月26~27日出现的一锋面飑线的18小时预报考察了中尺度和大尺度环流在飑线沿线变率生成过程中的作用。

This paper intrueluees the compsing and working principle of logical no cycle current switching circuit syste...

本文对该系统的逻辑无环流切换电路的组成和工作原理作了介绍，并给出各个功能电路的原理图

The mixed problem with lower bound for dry inviscid atmospheric circulation equations is discussed.

该文针对干的无粘大气环流方程组的混合问题，讨论其底部边界的混合问题。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。