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central north
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  华北中部
     Volcanic Event Strata and Correlation of Coals and Rocks of Taiyuan Formation in Central North China Cyclicity of Volcanic Event Strata and Correlation of Coals and Rocks(Ⅱ)
     华北中部太原组火山事件层与煤岩层对比——火山事件层的旋回性与煤岩层对比(Ⅱ)
短句来源
     Conductivity Structure of Lithosphere in Central North China: Magnetotelluric Study of Yingxian-Shanghe profile
     华北中部岩石圈电性结构——应县—商河剖面大地电磁测深研究
短句来源
     Volcanic Event Strata and Correlation of Coals and Rocks of Taiyuan Formation in Central North China ——Sedimentary Study of Volcanic Event Strata and Their Distribution(I)
     华北中部太原组火山事件层与煤岩层对比——火山事件层的沉积学研究与展布规律(Ⅰ)
短句来源
     CHARACTERRISTIC ANALYSIS ON SANDSTORM IN CENTRAL NORTH CHINA——TAKING LANGFANG AREA AS AN EXAMPLE
     华北中部沙尘暴的特征分析——以廊坊地区为例
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  “central north”译为未确定词的双语例句
     Different Controls over Pb and Nd Isotope Evolution of the Central North Pacific Ocean
     控制北太平洋深水中Pb、Nd同位素演化的不同因素
     Whereas those over the North Atlantic are the equatorial Atlantic (EAL), the Caribbean Sea (CAR), the eastern North Atlantic (ENA), and the central North Atlantic (CNA) patterns.
     而夏季北大西洋SST的主要异常型为赤道大西洋型(EAL),加勒比海型(CAR),东部北大西洋型(ENA)和中部北大西洋型(CNA)。
短句来源
     x) method for four nodules from the Central North Pacific are 0.8, 1.9, 2.9 and 4.3 mm/Ma respectively. The results are in reasonably good agreement with those found in other nodules by other investigators.
     利用~(230)Th_(ex)法测定了中太平洋北部四个锰结核顶侧的生长速率分别为0.8,1.9,2.9和4.3mm/Ma,这些数据接近于世界各大洋锰结核的平均生长速率。
短句来源
     Sedimentary Characteristics and Sources, and Environmental Indications of Late Quaternary in the Central North Yellow Sea
     北黄海中部晚第四纪沉积特征及其物源和环境意义
短句来源
     The results show that SST anomalies in central north Atlantic in winter reflected two basic models,and the interannual and interdecadal variability of second model characteristics that can reflect SST anomalies in the field between 20°N to 50°N in Atlantic in winter has close relation with mean air temperature in China.
     结果表明,冬季北大西洋中部海表温度异常主要表现为2个基本模态,其中反映冬季大西洋20°~50°N区域海表温度异常的第二特征模态,在年际、年代际变化关系上与中国冬季平均气温关系非常密切。
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  相似匹配句对
     QUATERNARY DIATOMS FROM THE NORTH CENTRAL PACIFIC
     中太平洋北部第四系硅藻
短句来源
     ON BONE-ANTLER-HORN TOOLS FROM THE CENTRAL NORTH CHINA
     华北地区旧石器时代的骨、角器
短句来源
     North and south
     专业面粉市场:南强北弱 “金像杯”面包烘焙大赛侧记
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     To the north is Kyushu.
     冲绳海槽北部与日本九州相接。
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     the Central and the Local;
     二是处理好中央与地方的关系;
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  central north
Observations of oceanic temperatures in the upper 400 m revealed an obvious region of the interdecadal signals in the central North Pacific.
      
The thermal anomalies subducted in the central North Pacific east to the dateline only reach 18°N.
      
The convergence between anomalous northerlies from the central North Pacific (not from the East Asian continent) and anomalous southerlies from Northeast Australia favors the persistence of a westerly over the central-eastern Pacific.
      
The general picture is that the anomalously warm (cool) SSTs in the central North Pacific are always accompanied by the anomalously cool (warm) SSTs along the west coast of America and in the central east tropical Pacific with comparable amplitude.
      
Migratory Timing of Humpback Whales (Megaptera novaeangliae) in the Central North Pacific Varies with Age, Sex and Reproductive
      
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The South China Sea is one of the tropical seas with high SST, and its seasonal and non-seasonal variations of SST are both conside-rable.It is found that SST variations of the central-north part of the South China Sea have a significant effect on the sea-air heat exchanges and the atmospheric stability.The central-north part of the South China Sea, as an underlying heat source,is responsible for the long-term weather anomalies.

南海海域是热带海洋高海温地区,海温层季节性变化与年际变化显著。海温变化对海气热量交换和大气层结稳定度均有明显作用。文章分析表明,南海中北部海域是能导致长期天气异常的下垫面热源。 南海海温场与上空温度场、高度与之间存在长周期耦合振荡。南海副高的维持及变化,也与南海海温场热力作用有一定的关系。

Three stages, geosynclinal, platform and diwa, can be singled out in the history of tectonic development of North Xinjiang, Based on the differences in development history and tectonic features, the study area can be divided into three tectonic regions, the Altay, Junggar and Tianshan diwa regions. They were transformed from a post-Hercynian pla- tform.Three factors have controlled the generation and evolution of the diwa regions in North Xinjiang: (1) Inhomogeneity in crustal structure. There is...

Three stages, geosynclinal, platform and diwa, can be singled out in the history of tectonic development of North Xinjiang, Based on the differences in development history and tectonic features, the study area can be divided into three tectonic regions, the Altay, Junggar and Tianshan diwa regions. They were transformed from a post-Hercynian pla- tform.Three factors have controlled the generation and evolution of the diwa regions in North Xinjiang: (1) Inhomogeneity in crustal structure. There is a relatively thin but "stable" Precambrian rigid basement in central North Xinjiang, which is surrounded by thick but weak ancient Hercynian geosynclinal fold belts. Such an inhomogeneity in crustal structure played an decisive role in the generation and evolutionof the diwa regions. (2) Existence and pattern of a "crust-mantle mix-melted layer". This layer is closely related to mantle activity. Its existence has exerted an important influence on tectonism and magmatism in North Xinjiang. (3) Mutual pressure of neighbouring crustal blocks in North Xinjiang. Lateral compression caused by crustal expansion and impedance or active compression of neighbouring crustal blocks have resulted in various folds and fractures and tectonic systems composed of them.The structures formed in North Xinjiang since Early Pleistocene time have resulted from the strong crustal expansion of the Tianshan diwa region and the compression, in a varying degree, of crustal blocks from south and north.

北疆可划分为三个各具不同特征的大地构造发展阶段,即地槽阶段、地台阶段和地洼阶段。根据地质发展史和构造特征的不同,本区现阶段可划分为三个构造区,即阿尔泰地洼区、准噶尔地洼区和天山地洼区。它们是由后海西地台转化而来的地洼区。 控制北疆各地洼区的形成演化的重要因素,一是地壳结构的不均一性:北疆中部存在厚度相对较小,但较为“稳定”的前寒武纪刚性基底,其周围存在厚度大、但较软弱的海西古地槽褶皱带,它对本区地洼区的形成演化起决定作用;二是“壳幔混熔层”的存在和分布状况:“壳幔混熔层”与地幔活动紧密相关,它的存在对北疆地壳运动和岩浆作用有重大影响;三是北疆各相邻壳体的相对推挤作用。由于地壳膨胀造成侧向的挤压作用,加上相邻壳体的阻挡作用或主动的挤压作用,致形成各种褶皱和断裂及由其组成的各种构造系。 北疆早更新世以来所形成的构造,主要是由于天山地洼区地壳的急激膨胀和来自南北方壳体不同程度的挤压作用所造成。

In this paper, Lorenz's moist low-order two-layer quasigeostrophic spectral model with beta-plane geometry[1]was improved.Using the improved model, we have carried out five experiments ex tended ( more than 75-day ) integrations.The model physics are orography, moisture process, time-dependent vertical stability, land surface heat budget, contrast between land and sea, climatic mean distribution of solar radiation absorbed by the land and sea surface in winter and parameterizations of long-wave radiation. From...

In this paper, Lorenz's moist low-order two-layer quasigeostrophic spectral model with beta-plane geometry[1]was improved.Using the improved model, we have carried out five experiments ex tended ( more than 75-day ) integrations.The model physics are orography, moisture process, time-dependent vertical stability, land surface heat budget, contrast between land and sea, climatic mean distribution of solar radiation absorbed by the land and sea surface in winter and parameterizations of long-wave radiation. From these experiments, it seems that the formation of blocking high is related to the nonlinear adjustment between flow fields and diabatic processes with moisture, and the nonlinear interaction of zonal currents and wave components under orographic forcing.Comparing flow patterns of blocking ridges proposed by Charney and Straus[2]from equilibrium state theory, the simulated blocking ridges over the Central North Pacific were much closer to reality.

本文对Lorenz二层准地转β平面低谱湿模式作了改进,并用改进的模式实施了五组积分时间大于75个模式日的试验。模式含有:辐射、感热、水汽相变、水份循环、垂直稳定度的变化、垂直内摩擦、地面摩擦、地形、陆面热量平衡及海陆差异。试验结果表明:地形强迫下基波与谐波的非线性作用以及包括湿过程在内的流场与加热场的非线性调整,与北太平洋阻塞高压的形成,之间存在着密切的联系。模拟出来的北太平洋中部阻塞高压,与Charney和Straus提出的阻塞高压平衡态相比更加接近于实际大气的阻塞现象。

 
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