东东北

词组短语

east-northeast

与东东北相关的网络例句 [注：此内容来源于网络，仅供参考]

In Alaska, though, the first pass of the ground motions triggered a swarm of small earthquakes near Mount Wrangell, a volcano about 330 km east-northeast of Anchorage and more than 11,000 km from Sumatra.

在阿拉斯加，虽然第一通的震动，触发了一场铺天盖地的小地震山附近wrangell ，火山约330公里东-东北锚地和超过11000公里，从苏门答腊。

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。

FIRST-LIGHT VISIBLE IMAGES ALONG WITH RECENT AMSU AND QUIKSCAT DATA SHOW THE CIRCULATION IS ELONGATED EAST-NORTHEAST TO WEST-SOUTHWEST.

第一轻有形的图像随着最近amsu和quikscat数据显示，流通是长东-东北至西-西南地区。

Land-sea heating, monsoon circulation, eastern Pacific trade wind and the slow seasonal shift of NE Pacific SST form winter to summer bihemispherically- all in joint action give rise to the enhancement of the Walker circulation that will travel east-and northward (west-and southward); the intensification of the maintained eastern Pacific Hadley circulation and north America-Alatantic Walker circulation zonally is responsible dominantly for the zonal/meridional movement of the WPSH in the winter-to-summer (or summer-to-winter) shift and its combination with the north American subtropical high.

海陆加热、季风环流、东太平洋信风以及东北太平洋海表温度由冬向夏关于赤道南北季节转换的迟缓性等综合作用导致的纬向Walker环流的加强东移和北抬、持续的东太平洋Hadley环流和北美—大西洋纬向Walker环流的加强是西太平洋副高由冬向夏产生东西、南北移动及其与北美副高合并的主要原因。

Based on the settings and geological and geochemical characteristics of granitoids of different orogenic belts (exemplified by orogenic granitoids in Altay, East Kunlun, Yanshan in North China, Northeast China and Nanling in South China), the relationships between granitoids and continental crustal growth are discussed, and five modes of continental crustal growth in the continent of China are proposed;they are as follows:(1)the Altay mode of continental growth is that the material and heat of the Paleozoic convertive mantle formed on the background of the Paleo-Asian Ocean were input into the Paleozoic continent and mixed with the materials of the upper crust;(2) the East Kunlun mode is that the basement of the Proterozoic orogenic belt was reworked by the heat input and materials of the Paleozoic-early Mesozoic convective mantle formed on the background of TTG continental crust of the Proterozoic orogenic belt;(3) the Northeast China style is that the Phanerozoic continental crust was reworked by the heat input and materials from the convective mantle formed on the background of the Yanshanian Central Asian orogenic belt;(4) the Yanshan mode is that the Archean basement was reworked by the heat input and materials from the Yanshanian convective mantle;and (5) the Nanling mode is that in South China what was input by the Yanshanian convective mantle into the continent was mainly heat and subordinately materials and the crustal material recycle was the dominant mode for the continental growth (showing zero continental growth).

根据不同造山带花岗岩的形成背景，地质地球化学特征差异，以阿尔泰，东昆仑，华北燕山，东北和南岭造山带花岗岩为例讨论花岗岩与大陆地壳生长的关系，区分出中国大陆的5种大陆地壳生长方式：阿尔泰式是古亚洲洋背景上形成的古生代对流地幔物质，热输入和上地壳混合为主的方式；东昆仑式是元古代造山带TTG陆壳背景基础上古生代—早中生代对流地幔物质和热输入，改造元古宙造山带基底的方式；东北式是燕山期中亚造山带背景上对流地幔物质和热输入改造显生宙陆壳的生长方式；燕山式是燕山期对流地幔物质和热输入改造太古宙基底的方式；南岭式燕山期对流地幔输入大陆的是以热为主，物质为辅，大陆地壳生长是以陆壳物质再循环为主的生长方式。

According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.

由于BOM没有考虑透射太阳辐射的物理过程，研究表明透射太阳辐射对北冰洋的能量收支起到重要作用，因此在BOM模式中引入了对透射太阳辐射的处理；通过对不同水道反照率的数值试验表明海冰厚度对水道反照率的敏感性不强，可能与海冰区水道面积占的比率很小有关；而模式模拟的北极海冰夏季&过度融化&主要源于NCEP再分析资料提供了偏大的太阳短波辐射；对北极海冰的气候变率进行了模拟研究，结果表明：模拟的海冰厚度变化与潜艇探测的海冰吃深度变化具有一致性；模拟和观测的亚欧大陆沿海的年内最大海冰厚度有很好的相关；模拟的海冰移速与长期平均的卫星反演的海冰移速具有相同的速度分布特征；模拟的各个海区海冰面积的变化趋势与卫星反演资料分析的结果基本一致；模拟与观测的主要海洋分区的海冰密集度具有很好的相关：弗瑞姆海峡的海冰体积和面积的输送涉及到海冰密集度、厚度和移动速度，是判断模式模拟能力的一个综合的指标，模式模拟的结果与卫星反演或重建的面积输送、体积输送具有很好的一致性；(5)分析了模拟的北极海冰厚度的气候变率及气候平均表层海流场，结果表明：北极海冰的总体积有显著减少的趋势，北极海冰总体积的变化具有10a际尺度振荡的特点，存在18-20a和12-13a两个主周期；北极海冰的平均厚度在各个海区的变化趋势不同，在巴伦支—喀拉海和巴芬湾—拉布拉多海地区海冰厚度有显著的增加趋势，而其它海区存在减少的趋势；通过对模拟的气候平均表层海流的分析表明，北极河流流量超前弗瑞姆海峡海冰流量7-10年的特征时间尺度与表层海流的气候分布存在着必然联系：(6)利用模拟结果以及中国降水、气温和热带关键区SST资料，讨论了北极各海区海冰平均厚度与中国降水、气温以及热带关键区SST的关系，结果表明：在北极中心海区和楚科奇—波弗特海海冰厚度偏大，在巴伦支—喀拉海以及巴芬湾—拉布拉多海海冰厚度偏小，则中国降水在华南地区、青藏高原和东北北部降水偏少，反之相反；在北极中心海区、东西伯利亚海、楚科奇—波弗特海以及格陵兰海海冰厚度偏小，在巴芬湾—拉布拉多海海冰厚度偏大，则在中国东北地区、高原南部地区和海南岛附近气温偏低，反之相反；另外，北极楚科奇—波弗特海和巴芬湾—拉布拉多海海冰厚度偏大时，在热带中东太平洋海温偏高，而在热带东南印度洋海温偏低。

The Taiwan mountain system and Island of Taiwan northeast - southwest moves towards parallel, the vertical stroke lies middle the Island of Taiwan 偏东 the position, forms east the main island the multi- sierras, middle the multi- knolls, west the multi- plains terrain characteristic.

台湾山系与台湾岛的东北——西南走向平行，竖卧于台湾岛中部偏东位置，形成本岛东部多山脉、中部多丘陵、西部多平原的地形特征。

The direction or point on the mariner's compass halfway between due north and northeast, or22=30 east of due north .

东北偏北水手罗盘上的方向或点，正北和东北中间，或正北偏东22＝30？

The direction or point on the mariner's compass halfway between due east and northeast, or67=30 east of due north .

东北偏东航海罗盘上的一个方向或点，位于正东与东北的中间点，或正北以东67＝30&&

The direction or point on the mariner's compass halfway between due east and northeast, or67=30?ast of due north.

东北偏东航海罗盘上的一个方向或点，位于正东与东北的中间点，或正北以东67＝30&&

与东东北相关的网络解释 [注：此内容来源于网络，仅供参考]

east-northeast：东北偏东

east 东方 | east-northeast 东北偏东 | east-southeast 东南东

east-northeast：东北东

easness 容易度 | east-northeast 东北东 | east-southeast 东南东

east-southeast：东南偏东

northeast东北 | east-southeast东南偏东 | east-northeast东北偏东

NE：东北

二十八、风向:风吹来的风向,气象上常用十六个方位和静风表示,即北(N),东北偏北(NNE),东北(NE),东北偏东(ENE),东(E),东南偏东(ESE),东南(SE),东南偏南(SSE),南(S),西南偏南(SSE),西南(SW),西南偏西(WSW),西(W),西北偏西(WNW),

NNE：东北偏北

二十八、风向:风吹来的风向,气象上常用十六个方位和静风表示,即北(N),东北偏北(NNE),东北(NE),东北偏东(ENE),东(E),东南偏东(ESE),东南(SE),东南偏南(SSE),南(S),西南偏南(SSE),西南(SW),西南偏西(WSW),西(W),西北偏西(WNW),

North East by East：东北偏东

north dilution of precision 北向精度系数 | North East by East 东北偏东 | North East by North 东北偏北

northeast by east：东北偏东

north-south 北-南 | northeast by east 东北偏东 | northeast by north 东北偏北

Northeastern Angkor：(吴哥东北面的寺庙)

East Mebon(东梅奔/东美朋/东梅蓬) | Northeastern Angkor(吴哥东北面的寺庙) | Preah Khan(圣剑寺/宝剑寺)

ene：东北偏东

二十八、风向:风吹来的风向,气象上常用十六个方位和静风表示,即北(N),东北偏北(NNE),东北(NE),东北偏东(ENE),东(E),东南偏东(ESE),东南(SE),东南偏南(SSE),南(S),西南偏南(SSE),西南(SW),西南偏西(WSW),西(W),西北偏西(WNW),

ESE：东南偏东

二十八、风向:风吹来的风向,气象上常用十六个方位和静风表示,即北(N),东北偏北(NNE),东北(NE),东北偏东(ENE),东(E),东南偏东(ESE),东南(SE),东南偏南(SSE),南(S),西南偏南(SSE),西南(SW),西南偏西(WSW),西(W),西北偏西(WNW),