查询词典 sea-beaten

Merged altimetry sea level anomaly data over China seas for more than 14 years is analyzed using the Empirical Orthogonal Function method. The spatial and temporal characteristics of sea level variability over Yellow Sea, East China Sea and South China Sea are presented, respectively.

用经验正交函数分析方法，对中国近海14年多的测高海平面同化格网资料进行分析，给出了黄海、东海和南海各海平面变化主要主成分的空间变化和时间变化特征。

The SSTA of February and August in 1998 had two peaks, while the wind speed reached its maximum minus anomalies in January and August. In order to find the circulation anomaly in the South China Sea, the circulation of 19952000 had been calculated by the ECOM hydrodynamic numerical model. The elevation and circulation of January and August in 1998 indicated that there were great anomaly of elevation and circulation after this El Nio event.(1)In January, the whole South China Sea had positive sea level anomaly and anticyclonic velocity anomaly, so the cyclonic circulation was weaker than normal.(2) In August, the South China Sea had positive sea level anomaly, especially stronger in the east of Vietnam, and cyclonic velocity anomaly in south, anticyclonic velocity in north, especially strong in the east of Vietnam. So the cyclonic gyre in the north and the anticyclonic gyre in the south were both weaker than normal, and an anticyclonic gyre appeared in the east of Vietnam.

为研究南海环流在1997/1998年的异常变化，利用ECOM水动力模型计算了1995—2000年的南海环流场，分析了1998年1月和8月南海水位和环流的异常分布，二者均存在显著的异常：①1月，整个南海海盆为正的水位异常，流场为反气旋异常环流，冬季控制整个南海海盆的气旋式环流减弱；②8月，南海海盆水位为正异常，特别是越南东部海区出现较强的正水位异常，南海南部的高水位中心扩大北移；异常流场表现为南部为气旋式异常环流，北部为反气旋的异常环流，且在越南东部海区形成非常强的反气旋异常环流中心，使得控制南海南部的反气旋环流和北部的气旋环流均减弱。

The Asian Mediterranean consists of several interconnected maritime basins: the Sea of Japan, the Yellow Sea, the South China Sea, the Sulu Sea, and the Celebes Sea.

亚洲的地中海含括几个相连的海域：日本海、黄海、南中国海、苏禄海、西里伯斯海。

From the sea ice motion data extracted from the MODIS and AVHRR images, it is found that the sea ice motion in the Bohai Sea is effected not only by prevailing winds but also by topographic steering, ocean currents and internal ice stresses. The extracted sea ice drift is similar to observed ice drift, and can clearly show the sea ice drift in the Marginal Ice Zone especially. It can compensate for the limitation of the local or single station observation.

利用MODIS和NOAA/AVHRR资料获取的渤海冰速资料的综合分析显示：渤海海冰运动，除受盛行风控制外，还受到复杂的海岸地形、流和冰内应力的共同作用，所得到的大范围海冰运动规律和多年历史观测资料分析结果基本一致，并清楚地显示了冰边缘带海冰运动的特征，弥补了局地、单站海冰观测的局限性。

The method of this study is:first,delaminate the sea ice data of the MODIS to two parts,one is the sea ice distributing,and the other is the sea ice temperature;then synthesize the data of sea ice distributing;and,count the sea ice extent on real time;at last,distill the surface temperature of the sea ice.

本文利用中分辨率成像光谱仪(Moderate Resolution Imaging Spectroradiometer，即MODIS)的海冰数据，监测中山站附近区域海冰的季节性的消融与冻结情况及海冰表面温度的变化。

Vermes, The Dead Sea Scrolls in English; A. Dupont-Sommer, The Jewish Sect of Qumran and the Essenes; M. Burrows, the Dead Sea Scrolls; FF Bruce, Second Thoughts on the Dead Sea Scrolls; WS LaSor, The Dead Sea Scrolls and the NT; R. deVaux, Archaeology and the Dead Sea Scrolls; JH Charlesworth,"The Origin and Subsequent History of the Authors of the Dead Sea Scrolls: Four Transitional Phases among the Qumran Essenes," RQum 10:213-33; CD Ginsburg, The Essenes.

杜邦，索默，犹太人教的昆兰和爱色尼；先生伯罗斯，死海古卷；法郎布鲁斯，第二思考死海古卷；是LaSor ，该死海古卷和NT ；河deVaux ，考古学与死海古卷；家查尔斯沃思说：&起源和更强的历史作者的死海古卷：四过渡阶段之间的昆兰爱色尼&， RQum 10：213 - 33 ；裁谈会金斯伯格，在爱色尼。

In this paper, researches on the characteristics of ice status in the Bohai Sea, the remote sensing methods of sea-ice resource reserves in the Bohai Sea, the characteristics of sea-ice reserves as a freshwater resource, the collecting schemes of sea-ice, the desalinizing techniques of sea-ice, etc. are made and the conclusions are as follows

本文从渤海各海区的冰情特征、渤海海冰资源储量遥感测量方法、海冰作为淡水资源的储量特征研究、海冰采集方案、海冰淡化技术等方面开展了研究工作，并得到以下结论。

With the developing of sea ice researches, more new scientific questions are raised, such as the interaction between sea ice and the other factors of global climate system, the seasonal and regional distributions of Polar sea ice thickness, Polar sea ice boundary and area changing trend, sea ice growth, melt and its influencing factors, the role of the polynya and sea/air interactions.

海冰和全球气候系统其它要素之间的相互作用问题、极地海冰的厚度季节性区域性分布问题、极地海冰边界及范围变化趋势问题、生消关键过程及其影响因素问题、冰间湖的作用以及海气相互作用等将是未来重要的研究方向。

Sea story ---------Olive tree is small, I am very few to the sea understanding, only knew that the sea is very big, the sea water is very blue, marine has sea Europe, sea Europe is the white.

小的时候，我对海了解很少，只知道大海很大，海水很蓝，海上有海欧，海欧是白色的。

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。

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。