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Columbia lava plateau相关的网络例句

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与 Columbia lava plateau 相关的网络例句 [注:此内容来源于网络,仅供参考]

The Qinghai-Tibet plateau underwent rifting and closure of Tethys and uplifting of the Qinghai-Tibet plateau that are different scale and two-stage tectonic processes.

青藏高原现今构造格局主要与青藏特提斯裂解与聚合和青藏高原构造隆升这两个不同尺度和不同阶段的动力学过程有关。

Anomalous anticyclone at the upper level is form in response to the enhanced convective heating off the equator, resulting in increased geopotential height and temperature over the Tibetan Plateau and in favor of the early BOB seasonal transition. Another effect of Positive SST anomalies over the Warm Pool is to induce anomalously strong zonal monsoon circulation. The anomalous zonal monsoon circulation strengths the southerlies in upper levels due to Coriolis force. Thus the enhanced warm meridional advection in connection with the warming over the Tibetan Plateau lead to early seasonal transition over the BOB region.

高空大气通过热力适应过程对这种异常对流加热的响应是产生异常反气旋环流,则高原上空的位势高度偏高,温度偏高,引起季节转换偏早;暖池海温异常偏高的另一作用是,它激发出异常强的季风纬向环流,在高层,季风纬向环流受到柯氏力作用又使得南风加强,导致孟加拉湾东部地区经向暖平流及其北部下沉增温加强,加速了孟加拉湾季节转换进程。

The discharge potential plateau is high and stable and the charge potential plateau is low.

电极放电电压平台较高而且稳定,充电电压平台较低。

The southwest vortex restricted the development of the plateau vortex in some way at the early stage when it appeared in the lower atmosphere. When they were coupled longitudinally, the vertical difference caused by the different vorticity advections between the upper and lower levels excitated the updrafts under 500 hPa and strengthened cyclone vorticity, and then the positive vorticity at 500 hPa and 700 hPa increased by two times The change rate of positive vorticity facilitated the plateau vortex to move eastward.

分析表明:高原涡与西南涡涡心之间的纬向距离在5个纬度的时候,两者上升气流都在500 hPa以下,当两者继续东移,在经向上耦合的时候,二者同时得到发展,西南涡中心的上升气流达到300 hPa,而高原涡中心的上升气流突破200 hPa;西南涡在低层出现初期,在一定程度上制约了高原涡的发展,随着两者在经向方向发生耦合,上下涡度平流不同造成垂直差动,将激发500 hPa以下的上升运动与气旋性涡度加强,使得500 hPa与700 hPa涡心正涡度值的增大近 1倍。

It is found through analysis of the shear line over Qingzang Plateau from May to August in 1979 by the use of scientific experimental data that the plateau shear line can be generated respectively in the easterlies, in the westerlies and in the neighourhood of the zero line between easterlies and westerlies.

切变线;无风带;西风带;毫巴;东风带;大尺度环流;本文利用科实资料对1979年5—8月青藏高原切变线进行分析后发现:高原切变线可以分别在东西风带分界的零线附近、西风带中和东风带中产生。

The weather of Yunnan-Guizhou Plateau is greatly impacted by the emergence of the Ferrel cell, which is resulted from the lifting effect of Tibetan Plateau and the southward anomaly of the Hadley cell.

青藏高原的抬升作用与Hadley环流偏南导致Ferrel环流的生成、加强对云贵高原的天气有重大的影响。

At last, upon the comparison of climate records from the Tibetan Plateau and its neighboring, the paper analyses the characteristics evolution of climate system and forcing mechanism since the last interglacial, especially in the last 40ka, in the Tibetan Plateau.

最后,在对青藏高原及阿拉伯海、印度洋、北大西洋、中国新疆地区气候环境演化的对比基础上,分析了青藏高原气候系统演化特点与动力背景。

The main conclusions are those:(1) the cause of hot-dry climate before elevation of plateau is that the efficiency of atmospheric heat engine is lower than after the elevation owing to flatter global landform;(2) at the beginning of Oligocene Epoch,the horizontal scale of plateau reached the cr...

主要结论:(1)高原隆起前的干热气候是由于隆起前全球地势平坦,致使大气热机效率很低之故;(2)渐新世初高原的水平尺度达到了斜压大气地转适应的临界尺度,大气环流从南北两极&两涡对峙&突变成地球三极的&三涡鼎立&,气候发生突变;(3)分析了2.5Ma时高原抬升到2000m这一重要临界高度后大气环流的一系列相应变化;(4)计算、比较了最大冰期地气系统能量平衡与现代的差异,并由此分析了当时的气候状况

The ice raft and the glacier mud rock flow deposited along the northern and northwest edge of the plateau during early Cretaceous, implies that the northern edge of the plateau may be of the suitable height, may be similar to present's Himalaya Mountain.

该区中生代构造特征表明,该区侏罗纪和早白垩世的构造特点有着巨大的差异:侏罗纪,尤其是晚侏罗世末期以南北向的挤压构造为主,而早白垩世中期以后演变为以伸展构造为特征,古地理古环境明显改变。

The glacial response to climatic change is more sensitivity at the margins of Qinghai-Tibetan Plateau than those inlands of Qinghai-Tibetan Plateau.

显示出青藏高原冰川对气候变化响应的敏感性在边缘山区较中腹地区更为敏感。

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另外,康威特罗勒斯可以使用同步整流器本身或亏损减少电感电流检测方法,以提供低功耗过载保护。

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