向东南

Formation of basin and range province in Southeast China was mainly resulted from geodynamic evolution of west marginal-Pacific tectonic domain, and from collision and squeezing of Indian plate with Euro-Asian continent.

形成中国东南地区盆岭构造的外部条件是滨西太平洋域的地球动力学演变，次要条件是西侧印度板块向北移动与欧亚大陆的碰撞及推挤。

A river that rises in the Catskills in southeastern New York and flows southward along the border of Pennsylvania with New York and New Jersey to northern Delaware where it empties into Delaware Bay.

一条发源于纽约东南的河流，向南绕过宾夕法尼亚洲和纽约以及新泽西州的边缘，最后在特拉华州北部汇入特拉华海湾。

Southeast me some maritime space, a 50 tons cockboat, the speed that carrying brisk cold wind on the head to be controlled with 10 is northeast direction sails.

我东南某海域，一艘50吨的小艇，正顶着凛冽的寒风以10节左右的速度向东北方向驶去。

Therefore, the moist potential vorticity analysis associated with the mesoscale convective system was researched in the paper, so as to reveal the moist potential characteristics of mesoscale convective system in typhoon circulation. The results showed that, during the generation stage, convective instability characterized by MPV1 was a favorable condition for forming MCS, while the vorticity which was caused by the slantwise isentropic surface and the vertical shear of the horizontal wind characterized by MPV2 was an inspiring mechanism. The specific process was that, the atmosphere exhibited the feature of strong convective instability at the low level of convection areas and the southeast areas, which included plenty of erratic energy. The slantwise ascended the stream transfer the erratic energy to northwest, where the stratification stability was small. As decreased, the cyclonic vorticity increased. On the other hand, the vorticity caused by the slantwise isentropic surface and the vertical shear of the horizontal wind inspired the release of convective instability and as a result that the MCS formed. During the development stage, the cyclonic vorticity increased quickly with the persistent decreasing of . Meanwhile, the inclination of isentropic linewas bigger than the absolute momentum line at middle level, which exhibited the feature of conditional symmetric instability , then the conditional symmetric instability was forced to release by the vorticity resulted from the slantwise isentropic surface and the vertical shear of horizontal wind, and the MCS developed.

结果表明，在对流形成阶段，MPV1即对流不稳定为MCS的形成提供背景不稳定条件，由MPV2即湿等熵面的倾斜和水平风的垂直切变而引起的涡旋发展作为强迫机制：MCS形成的区域及东南区域中低层是强对流不稳定层，蕴含丰富的不稳定能量，倾斜上升运动把对流不稳定区具有强不稳定能量的暖湿空气向西北中层的中性层结区输送，由于的减小，气旋性涡度增强，有利于形成对流，另一方面，由于湿等熵面倾斜和低空急流加强而引起的涡旋发展作为一种强迫机制激发对流不稳定能量得到释放，从而形成对流；在对流系统地发展阶段，由于低层的对流不稳定性进一步减弱，进一步减小，气旋性涡度进一步增强，有利于MCS的增强，中层等θe 线的倾斜度比绝对动量M 等值线的倾斜度大，对应有条件对称不稳定区域，满足条件对称不稳定条件，在湿等熵面倾斜和台风低空急流作用下引起的涡旋发展强迫对称不稳定能量释放，从而使得对流得以维持和加强。

In summer, because the vertical incident solar rays regionmoves by the equator to the north, causes of southeast trade crossingthe line the southern hemisphere to change the southwest monsoon toinvade Northern Hemisphere, meets one another with the originalNorthern Hemisphere's Northeast Tradewind, compels crowds this airrise, the increase convection current, again because the southwestmonsoon and the Northeast Tradewind direction is different, meets oneanother often creates the undulation and the whirlpool.

在夏季，因为太阳直射区域由赤道向北移，致使南半球之东南信风越过赤道转向成西南季风侵入北半球，和原来北半球的东北信风相遇，更迫挤此空气上升，增加对流作用，再因西南季风和东北信风方向不同，相遇时常造成波动和旋涡。

From the east and south, a steel grayness crept toward the glaring brilliance of the west.

一种泛蓝的灰色从东南向西部的绚丽色调爬去。

Kuroshio water was an important factor that affects the horizontal distribution of CB in winter.

冬季受黑潮水的影响20m层和表层中的聚球蓝细菌数量自东南向西北递减。

Seed distribution varied with orientation (p.01), with most seeds to the north of the female tree, followed by northeast, north and southeast.

当年下落到地面的东北红豆杉种子，按远离母株的顺序，种子数量逐渐减少；在围绕母株的八个方向上，东向的种子数量最多，其次是东北、北和东南方向，西面的种子数量最少。

A mid-latitude trough will induce a break in the ridge and weaken its western side which will lead to a more northwesterly track after t+24 and a northerly track in the extended taus.

预料一道西风槽将令副高出现弱点，副高届时将转呈西北-东南走向，从而使凤凰在 24 小时后转向西北偏西至西北移动，并於 72 至 96 小时后转向偏北方向移动。

The fault-depressed basins related with the rapid lift-up of ranges spread northwestwardly from the Miocene to the Quaternary.

从中新世经上新世至第四纪，与山体快速隆起相伴的断陷盆地有从东南向西北扩展的趋势。

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。