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east asia area
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  东亚地区
     Using the Singular Value Decomposition (SVD) technique, the relationship between the surface heating field in QinghaiXizang Plateau and 500 hPa geopotential height field of East Asia area and spring air temperature field of SichuanChongqing area and its forming anomalous causes of are studied.
     应用奇异值分解(SVD)技术,研究了青藏高原地面加热场与东亚地区上空500hPa高度场及其东侧川渝地区春季气温场的时空联系和冷暖异常成因。
短句来源
     (3)The southward migration of East Asia area since Paleozoic was further supported by plaeomagnetic study of late Paleozoic to early Tertiary in the eastern and northern Xinjiang.
     (3)通过新疆东部和北部晚古生代到早第三纪古地磁研究,进一步证明了东亚地区从中生代开始南向移动的存在;
短句来源
     According to my primary statistics,there are 34 families 49 genera and 975 species appearing in disjunct distribution type both in East Asia and North America, of which 730 species are in East Asia area,making up 75% of the total,245 in North America area,making up 25%,The fact shows that the species in East Asia far outnumber those in North America. It′s estimated that the genera number in this disjunct distribution area is the greatest among the continents in the world.
     东亚-北美间断分布区的木本植物种类,初步统计共有34科49属975种,其中东亚地区730种,占总数的75%,北美地区245种,占25%,说明东亚种数远多于北美,估计本间断分布区中属的总数为全世界诸多洲际间断分布中极为丰富的类群。
短句来源
     This brings about far-reaching significance to the long-range development of the bilateral relationship and the prosperity and stability of the East Asia area.
     这对双方关系的长远发展和东亚地区的繁荣稳定具有深远意义。
短句来源
     The body is divided into three following parts again:The first part: the contents is to definite East Asia and to describe the influence of international relationship developed by the nation, the religion and the culture, and to analyze in detail the trait of them in East Asia area.
     文章正文包括以下三部分:第一部分在界定东亚概念的基础上,系统介绍了东亚地区民族、宗教、文化对国际关系的影响,并详细分析了东亚地区民族、宗教、文化的特点。
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  东亚区域
     First EAS and East Asia Area Cooperation
     首届东亚峰会与东亚区域合作
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     A Research on Monetary Integration of East Asia Area
     东亚区域货币一体化研究
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     But east Asia area trade reliance degree and economic opening are both relatively high, which offers the foundation for the fact that the currency of east Asia integrates;
     但东亚区域内贸易依赖度及经济开放度较高,这为东亚货币一体化提供了基础;
短句来源
     This paper analyzes the international background of this new East Asia area cooperation mode and the difficulties to achieve this goal.
     本文就这一东亚区域合作的新模式产生的国际背景 ,以及实现目标所面临的困难进行分析。
短句来源
     (3)the common and different characteristics between the NAFTA dominated by the United States and the East Asia Area Cooperation.
     (3)美国主导的北美自由贸易区与东亚区域合作的共性与差异。
短句来源
  东亚地区上空
     Using the Singular Value Decomposition (SVD) technique, the relationship between the surface heating field in QinghaiXizang Plateau and 500 hPa geopotential height field of East Asia area and spring air temperature field of SichuanChongqing area and its forming anomalous causes of are studied.
     应用奇异值分解(SVD)技术,研究了青藏高原地面加热场与东亚地区上空500hPa高度场及其东侧川渝地区春季气温场的时空联系和冷暖异常成因。
短句来源
  “east asia area”译为未确定词的双语例句
     If the surface heating field in QinghaiXizang Plateau in winter is strong(weak), the 500 hPa geopotential height field over East Asia area is high (low), and the air temperature of SichuanChongqing area is also high (low) in next spring.
     冬季高原地面加热场强度偏强(弱),则后期春季东亚上空500hPa高度场偏高(低),川渝地区春季气温偏高(低);
短句来源
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  east asia area
Genetic algorithm-finite element method (GA-FEM) is applied to the study of tectonic stress field of part of East Asia area.
      


The structure of simultaneous physical retrieval method published recently by W. L. Smith and H. M. Woolf is analyzed. The experiment of multi-orbit retrieval and mosaic using polar orbit meteorological satellite data over East-Asia area is made The dependence of retrieval accuracy upon different initial guess profiles is studied.

对Smith和Woolf近期发表的同步物理反演法进行了结构分析,并对东亚地区的卫星资料进行了多轨道反演拼图试验,同时用不同的初始估计廓线对反演精度的依赖性进行了研究。

The paleomagnetic study of the strata of Ordivician to Upper Tertiary, conducted in the seven areas along the section from Koktokay to Mori, Hami and Aksay where about 1 500 specimens were sampled from 320 sites,reveals the following main results: (1) The paleomagnetic pole paths of North Junggar and East Junggar were set up , and the Junggar Ocean was therefore, concluded to be formed during Devonian - Carboniferous and closed during Permian. The two pieces,united together during early Paleozoic...

The paleomagnetic study of the strata of Ordivician to Upper Tertiary, conducted in the seven areas along the section from Koktokay to Mori, Hami and Aksay where about 1 500 specimens were sampled from 320 sites,reveals the following main results: (1) The paleomagnetic pole paths of North Junggar and East Junggar were set up , and the Junggar Ocean was therefore, concluded to be formed during Devonian - Carboniferous and closed during Permian. The two pieces,united together during early Paleozoic at a latitude of ±30°S,and in Devonian were seperated into many parts with a long distance away from each other up to 1 000km. The rapid northward migration up to a latitude of 20°-30°N occured during the late stage of early Paleozoic to early stage of late Paleozoic. (2)The locality of paleomagnetic poles from Qijiaojing,Sha Quanzi and Liuyuan of Carboniferous to Permian was obtained. The Liuyuan and Sha Quanzi areas,utterly different from Junggar area, have an approximate paleomagnetic pole locality with Ili Block, Tacheng Block, Tu-Ha Block, Erdus Block and North China Block . It revealed that these blocks were an isolated intermediate terrane be-ween North Continent and South Continent. (3)The southward migration of East Asia area since Paleozoic was further supported by plaeomagnetic study of late Paleozoic to early Tertiary in the eastern and northern Xinjiang. (4)Junggar Block was located at a latitude of 30° - 50°N during late Paleozoic,and Junggar Ocean was pulled apart approximately eastwest-ward. The relative migration, if occurred, was less than 1 500km in the direction of south to north . (5)The structural evolution of Junggar Block followed the evolution model of North Continent,implying Junggar Block was once a part of North Continent.

沿富蕴—二台—苏古泉—七角井—沙泉子—柳园—阿克塞对奥陶系—上第三系进行古地磁研究,主要获得以下成果:(1)建立了北准噶尔地片和东准噶尔地片极移曲线,认为准噶尔洋形成于泥盆纪—石炭纪,在二叠纪闭合。这两个地片在早古生代是一个统一的构造单元,位于30°S左右,泥盆纪拉开距离达1000km,其北边的地片位移于20°—30°N左右,早古生代晚期到晚古生代早期是地块快速北向移动时期;(2)获得了七角井、沙泉子和柳园地区石炭、二叠纪古地磁极位置及古纬度,其中的柳园、沙泉子地区极点位置明显与准噶尔不一致,而与哈萨克斯坦西天山(伊犁地块)、塔城地块、吐哈地块、鄂尔多斯地块及华北地块等古地磁极接近,说明这些地块在晚古生代已处于南、北大陆之间,成为独立的中间地体;(3)通过新疆东部和北部晚古生代到早第三纪古地磁研究,进一步证明了东亚地区从中生代开始南向移动的存在;(4)准噶尔地块在晚古生代处于30°—35°N的古纬度区,准噶尔洋主要为近EW向拉开,如果存在SN向移动,其相对移动距离也不会超过1500km。(b)从晚古生代以来的北方大陆块体构造演化模式来看,准噶尔地块大致遵循了北方大陆块体统一的构造演化规律,说明准噶尔地块是北方...

沿富蕴—二台—苏古泉—七角井—沙泉子—柳园—阿克塞对奥陶系—上第三系进行古地磁研究,主要获得以下成果:(1)建立了北准噶尔地片和东准噶尔地片极移曲线,认为准噶尔洋形成于泥盆纪—石炭纪,在二叠纪闭合。这两个地片在早古生代是一个统一的构造单元,位于30°S左右,泥盆纪拉开距离达1000km,其北边的地片位移于20°—30°N左右,早古生代晚期到晚古生代早期是地块快速北向移动时期;(2)获得了七角井、沙泉子和柳园地区石炭、二叠纪古地磁极位置及古纬度,其中的柳园、沙泉子地区极点位置明显与准噶尔不一致,而与哈萨克斯坦西天山(伊犁地块)、塔城地块、吐哈地块、鄂尔多斯地块及华北地块等古地磁极接近,说明这些地块在晚古生代已处于南、北大陆之间,成为独立的中间地体;(3)通过新疆东部和北部晚古生代到早第三纪古地磁研究,进一步证明了东亚地区从中生代开始南向移动的存在;(4)准噶尔地块在晚古生代处于30°—35°N的古纬度区,准噶尔洋主要为近EW向拉开,如果存在SN向移动,其相对移动距离也不会超过1500km。(b)从晚古生代以来的北方大陆块体构造演化模式来看,准噶尔地块大致遵循了北方大陆块体统一的构造演化规律,说明准噶尔地块是北方大陆的组成部分。

In this paper, the remote respone between the cumulus convective precipitation over the South China sea as well as the tropical wed-pacific and the subtropical high' s shift over the East-Asia in summer, is studied. The results show that this remote respone is achieved by the dynamic process of a kind of large scale slowly varying wave train, excited in the tropical regions, propagating towards the subtropical East- Asia areas. Through this mechanism, the tropical environmental...

In this paper, the remote respone between the cumulus convective precipitation over the South China sea as well as the tropical wed-pacific and the subtropical high' s shift over the East-Asia in summer, is studied. The results show that this remote respone is achieved by the dynamic process of a kind of large scale slowly varying wave train, excited in the tropical regions, propagating towards the subtropical East- Asia areas. Through this mechanism, the tropical environmental factors(thermal forcing and circulation patterns) will induce the intensity and position of subtropical high over the East-Asia being difference.

论证了夏季南海及热带西太平洋地区的积云对流活动与东亚上空副热带高 压活动之间的遥相关关系。结果表明,这种遥相关作用是通过上述热带地区积云对流 活动激发出的天气尺度以上的准定常波列向东亚副热带上空的传播过程来实现的。通过这种机制,上述热带地区的热力强迫和环流构型等环境场因子的变化将导致东亚上空副热带高压强度和位置的差异。

 
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