- 更多网络例句与喀拉海相关的网络例句 [注：此内容来源于网络，仅供参考]
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These discoveries provide important new insight into the hydrocarbon potential of the adjacent eastern Barents and Kara seas.
这些发现为加深了解相邻的巴伦支海和喀拉海东部的油气远景提供了新的重要线索。
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These three ductile to ductile-brittle meso-shallow deformational belts made up a complete plate （micro-landmass） condensation zone, indicating that the Kalatongke island arc underthrust, towards northeast to east, the Keketuhai-Qinghe magmatic arc, then a continent-arc collision occurred.
结合区域地质分析，可认为这3个变形带共同组成一个完整的板块聚合变形带，显示喀拉通克岛弧以北东偏东方向俯冲于可可托海-青河陆缘岩浆弧之下，并发生弧-陆碰撞。
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The Yangtze River, with length is about 6380km, is the longest river in China and the third longest river in the world, which rises from Geladangdong Jokul, flows over Qinghai Province, Xizhang Province, Sichuan Province, Chongqing City, Yunna Province, Hubei Province, Hunan Province, Jiangxi Province, An'hui Province, Jingshu Province and Shanghai City and converge into the East China Sea and Huang Sea at last.
长江是我国第一、世界第三大河，绵延6380公里，从喀拉丹东雪山南麓冰川出发，干流先后流经青海、西藏、四川、云南、重庆、湖北、湖南、江西、安徽、江苏和上海等省市，在东海与黄海的交界处入海。
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Thus, Vera's ashes were scattered on Lake Titicaca, in Bolivia, following the ancient traditions of the Aymara Indians; on the river outside the royal palace in Stockholm; on the banks of Choo Praya, in Thailand; at a Shinto temple in Japan; on the icecaps of Antarctica; in the Sahara desert.
因此，浑子的骨灰散落在的喀喀湖，在玻利维亚，继古老的传统的艾马拉印第安人；上河以外的王宫在斯德哥尔摩；对银行的秋秉直海旁，在泰国，在一个神道寺庙在日本；就icecaps的南极洲，在撒哈拉大沙漠。
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A river of central Siberian U.S.S.R. flowing about4, 023 km(2, 500 mi) westward and generally north to the ''.'Kara'.'' Sea through Yenisei Bay, a long estuary.
叶尼塞河苏联西伯利亚中部一河流，流程约4，023公里（2，500英里），向西而且大致向北流经一长海湾叶尼塞湾流入喀拉海
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Flowing about4, 023 km(2, 500 mi) westward and generally north to the Kara Sea through Yenisei Bay, a long estuary.
叶尼塞河苏联西伯利亚中部一河流，流程约4，023公里（2，500英里），向西而且大致向北流经一长海湾叶尼塞湾流入喀拉海
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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。
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Which by their causes, and the water depth can be divided into two parts, one is basically the edge of the continental shelf sea (such as the Kara Sea, Laptev Sea, East Siberian Sea, Chukchi Sea, Beaufort Sea, Baffin Bay, Hudson Bay, etc.); Second, the central part of the Arctic Ocean, all kinds of ice widespread, most of the waters as "permanent ice zone" of biological resources than the poor.
后者按成因和水深又可分为两部分，一是基本上属于大陆架范围的边缘海（如喀拉海、拉普捷夫海、东西伯利亚海、楚科奇海、波弗特海、巴芬湾、哈得孙湾等）；二是北冰洋中央部分，各类浮冰广布，大部海域为&永冰区&，生物资源较贫乏。
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I read recently of an ingenious plan put forward by Russian engineers, for making the White Sea and the northern coasts of Siberia warm, by putting a dam across the Kara Sea.
我最近读到一份俄国工程师提出的独出心裁的计划，说是要筑一条坝穿越喀拉海，使白海和西伯利亚北部沿海变暖。
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Chikmaryov lives in Marresale, an outpost on the Yamal peninsula's north-west coast overlooking the Kara Sea .
契科马耶夫住在位于雅马尔半岛西北海岸的马拉萨尔。从那里可以俯瞰到喀拉海。
- 更多网络解释与喀拉海相关的网络解释 [注：此内容来源于网络，仅供参考]
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Barents：巴伦支(海)
"巴伦支海(Barents)和喀拉(Kara)海域发现大型油田的同时,人们也随之开始担忧灾难性的事故的发生. 装载有石油和液化气的轮船来往于斯堪的那维亚渔业区,将能源运往欧洲和北美. 这片未曾被践踏过的土地很有可能会随着能源工业的发展而被污染.
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Charybdis：卡律布狄斯
同行的赫耳墨斯建议奥德修斯用草药(Moly)去抵抗喀耳刻的魔法. 经过一夜之后,喀耳刻便爱上了奥德修斯,并在未来一年帮助他返回家乡. 喀耳刻建议奥德修斯经由墨西拿海峡返回家乡,但在这个海峡他将会遇上名为卡律布狄斯(Charybdis)的危险漩涡和女海妖斯库拉.
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Heidelberg：海得尔堡
少年时代特尔慈受信义会影响甚深,曾从弗冉克(Frank),立敕尔(Ritschl),拉喀尔(PauldeLagarde)诸名师习心理,逻辑,宗教及哲学等;一八九一年开始写作生活,翌年应聘任波昂(Bonn)大学神学教授,一八九四年任海得尔堡(Heidelberg)大学神学教授,到了
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Indus：印度河
[印度河] (Indus)梵名Sindhu (信度). 乃印度之大河. 发源于西藏高原,流经喜马拉雅山与喀拉昆仑山两山脉之间,流向西南而贯穿喜马拉雅山,右岸交会喀布尔河,左岸汇流旁遮普(梵Pan~ja^b ,五河之意)地方之诸支流,经巴基斯坦而入阿拉伯海.
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Kara Sea：喀拉海
东和东南临鄂毕湾,西濒喀拉海(Kara Sea)及拜达拉茨湾. 长750千米左右,宽约240千米. 面积12.2万平方千米地表平坦,最高点海拔90米. 冬季寒冷,长达8个月. 河流、湖泊众多. 永冻层广布. 南缘为森林苔原带,中部为苔原、草地与灌丛,
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Ob：鄂毕河
(袁树人) 鄂毕河(Ob') 亚洲北部的重要国际河流. 由源出阿尔泰山的比亚河和卡通河汇成. 自南西伯利亚山地曲折向西北流,纵贯西西伯利亚平原,注入北冰洋喀拉海的鄂毕湾. 汇合点以下河长3650公里;以卡通河为源,长4338公里;