查询词典 part of a river

Tibet has very complex topography and falls into three geographic parts: the northern part of Tibet known as the North-Tibet Plateau, lies between Kunlun Mountain, Tonglha Mountain and Kangdese Mountain, and Nyainqentanglha Mountain;between Kangdese Mountains and Himalayas;the river valleys which the the Yarlung Tsangpo and its anabranch flow by in the southern part of Tibet and lie between the Gangdise and the Himalaya ranges; the eastern part of Tibet belongs to an area of deep gorges where a series of mountain ranges from east to west criss-crossing mountain ranges running from south to north,and is some parts of the Hengduan mountain range.

在西藏的边远山谷中，一辆老式的苏联卡车翻滚到坡底的河边，车里一个已经怀孕了几个月的女人尽然不死，而她腹中的孩子也没死，那个孩子尽然就是我。"——莫毅，这为神交已久而未谋面的艺术家，其作品在许多展览上令我印象深刻，在筹备此展的过程中认识，相聊甚欢。多年藏区生活塑造了一个率直敏锐的性情汉子，这组拍摄于20年前、却完成于今年的作品以严肃的记实性和抒情的叙事片段，融会艺术家近年的实验手段，呈现了对诸如"脆弱"、"意外"、"真实"和"理想"的记忆。因此20年后的莫毅仍然"想念西藏。

With the middle and lower part of the Pearl River as its center, the Pearl River Culture is a regional culture that has long exerted great impact on the local inhabitants and the regions around.

珠江文化是经过漫长的发展阶段，形成于明清时期，以珠江中下游地区为中心，对当地居民及周边地区乃至全国产生持久而深刻影响的一支地城性文化。

National Emblem: Central shield surface Photo has three cases: the upper part of the national flower water lily; middle for 3 blue bellows, a symbol of the country's Essequibo River, Berbice River, Demerara River the three main rivers and numerous waterfall, rapids; lower for a pheasant, on behalf of the country's rich animal resources.

国徽： 中间的盾面上有三组图案：上部为国花睡莲；中间为三道蓝色波纹，象征该国的埃塞奎博河、伯比斯河、德梅拉拉河三条主要河流及众多的瀑布、激流；下部为一只雉，代表该国丰富的动物资源。

Following implementation of the project for the construction of the shelter-forest system of the Yarlungzangbo River, which is part of the key "three rivers" agricultural development undertaking, a man-made forest belt measuring several hundred km from Xigaze to Zetang on the upper reaches of the Yarlungzangbo River has been formed.

隶属"一江两河"农业开发重点项目的雅鲁藏布江防护林体系建设工程实施后，形成了从上游的日喀则到泽当几百公里的人工林带，成为西藏一道新的亮丽景观，对雅鲁藏布江的水土保持起到了积极的作用。

Combined the geological analysis with analogue modeling experiments,the evolution of the Yinggehai basin could be divided into four main stages:(1) Before 42Ma,controlled by the southeastward extension of the Beibu Gulf basin on the northern continental margin,the Yinggehai basin experienced dextral pull-apart.Bounded by NS-trending Yingxi fault,the transtensional areas mainly are the northwest part and along the eastern boundary of the basin.(2) From 42 to 21Ma,the development of the main rift body in Yinggehai basin was mainly controlled by the southward slip and clockwise rotation of the Indochina block along the Red River fault zone,and the sedimentation was strengthened due to the sinistral transtension.In the east,the subsidence is deepened due to the dextral transtension.(3) From 21 to 10.4Ma,the sinistral movement of the Indochina block slowed down to still.From 21 to 15.5Ma,the northwest part of the basin began to inverse locally because of post-rift thermal subsidence of the whole basin.(4) From 10.4Ma to present,the basin was affected by the dextral movement of the South China block along the Red River fault zone and thermal accident in a new phase at 5Ma.

结合地质分析和物理模拟实验，莺歌海盆地的演化大致可以分为以下4个主要阶段：早期(42 Ma以前)主要受到南海北部陆缘裂解造成的右旋转换伸展作用的影响，但影响范围较小，主要为莺歌海盆地西北部和东部边界。42～21 Ma期间，主要受控于印支地块左行走滑和顺时针旋转作用的影响，莺歌海盆地在此期间发育了主体裂陷体系，东侧受到右旋转换伸展应力场的叠加影响而导致沉降加强；21～10.4 Ma期间，受印支地块逐渐减弱直至停止的左行走滑作用的影响，盆地西北部在21～15.5 Ma期间发生局部反转褶皱，但盆地整体进入以热沉降为主的时期；10.4 Ma以后，盆地受华南地块沿红河断裂右旋走滑作用和5 Ma以后新一期热事件的影响。

Regional tourist cooperation is a significant trend in current development of tourist industry, which shows the initiative of tourist industry. At present, regional tourist cooperation around Pan Pearl River Delta is the hot cooperation region and Yunnan province, as an important part of western China, is going to discuss in this paper about joining the regional cooperation in Pan Pearl River Delta and developing its influence to offer high class ethnic culture tourist services.

区域旅游合作是当前旅游业发展的一种大趋势，是旅游产业做出的一种主动接轨，泛珠三角区域旅游合作是当前热点的话题，作为其中重要的西部组成成员的云南省，如何利用其丰富的民族文化旅游资源，抓住这一区域旅游合作广泛开展的重要机遇，积极参与泛珠三角区域合作，充分发挥作用，推出高品位的民族文化旅游产品，这是本文所要探讨的问题。

The headwater region of the Yellow River is located at the core area of the Three River Natural Reserve, which is in the central-eastern part of the Qinghai-Tibet plateau. The region serves as a protective eco-screen of both China and Southeast Asia.

中文摘要黄河源区位于青藏高原中东部的三江源自然保护区的核心区，是我国和东南亚国家生态系统安全和区域可持续发展的生态屏障。

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。

Then I turned and went down Chesnut-street and part of Walnut-street, eating my roll all the way, and, coming round, found myself again at Market-street wharf, near the boat I came in, to which I went for a draught of the river water; and, being filled with one of my rolls, gave the other two to a woman and her child that came down the river in the boat with us, and were waiting to go further.

m9 {2 M！ i1 k 于是我转个弯，经过栗子街和胡桃街的一段，在路上吃那一卷东西，兜一个圈子，发现我又在市场街码头，离开我刚来时停船处不远，我到那里去喝一点河水，我的三卷中的一卷已塞满我的肚子了，于是就把另外的两个给一个妇人和她的孩子，她是和他们一齐来的，正在等着到更远的地方去。

Then I turned and went down Chestnut-street and part of Walnutstreet, eating my roll all the way, and, coming round, found myself again at Market-street wharf, near the boat I came in , to which I went for a draught of the river water; and, being filled with one of my rolls, gave the other two to a woman and her child that came down the river in the boat with us, and were waiting to go farther.

接着我转身沿粟子大街和核桃大街走着，边走边啃着我的面包圈，突然发现自己又到了市场街的码头，在靠近我来的渡船的地方，我喝了一大口河水，吃了那一个面包圈我就饱了，于是就将另外两个给了和我一同乘船来并等着要继续走的母子二人。

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。