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South China Sea相关的网络例句

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与 South China Sea 相关的网络例句 [注:此内容来源于网络,仅供参考]

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 study shows that in various continental downfaulted basins in eastern China,the China East Sea basin of the southeast sea region and the continental shelf—Qiongdongnan basin and Zhujiangkou basin—of the northern South China Sea,CO2 in CO2 reservoirs and CO2-rich oil/gas reservoirs is of typical volcanic mantle-derived type and that its migration and concentration is mainly controlled by mantle-derived volcanism and gas-conducting distribution of deep basement faults connected with the gas source at depth. CO2 is mainly sourced from substantial amount of CO2 associated with mantle-derived volcanism at the deep level of the crust. CO2 in the CO2 reservoirs and CO2-rich oil/gas reservoirs in the Yinggehai basin on the continental shelf of the northern South China Sea is of crust origin and crust-mantle mixing origin and mainly controlled by local,layer-by-layer and zone-by-zone,multiple intrusion of late hydrothermal fluids in mud diapir areas and physico-chemical processes of very thick Pliocene-Miocene marine calcareous sandstone and mudstone.

研究表明,中国东部陆上诸断陷盆地与东南沿海海域的东海盆地及南海北部大陆架琼东南盆地和珠江口盆地CO2气藏及高含CO2油气藏中,CO2均属典型的火山幔源型成因,其运聚富集主要受控于幔源型火山活动与沟通深部气源的基底深大断裂的导气配置作用,CO2气源主要来自地壳深部幔源火山活动伴生的大量CO2;南海北部大陆架西区莺歌海盆地CO2气藏及含CO2油气藏中的CO2,属于壳源型及壳幔混合型成因,主要受控于泥底辟热流体晚期分层分块多期的局部上侵活动与沉积巨厚海相含钙砂泥岩的物理化学作用,其运聚分布具多期和分层分区的特点。

The results show that when the tropical western Pacific is in a warming state in spring, convective activities are intensified around the Philippines. In this case, there is a cyclonic anomaly circulation in the lower troposphere over the South China Sea, and the western Pacific subtropical high shifts eastward, thus, the early onset of the South China Sea summer monsoon can be caused. Moreover, when the tropical western Pacific is also in a warming state, convective activities around the Philippines are also strong in summer, since the western Pacific subtropical high abruptly shifts northward in mid-June and early July during its northward advance in this case, the abrupt northward-shift of the East Asian summer monsoon rainband from South China to the Yangtze River and the Huaihe River valleys is obvious in mid-June and this monsoon rainband again jumps northward from the Yangtze River and the Huaihe River valleys to the Yellow River valley, North China and Northeast China in early July.

分析结果表明:当春季热带西太平洋处于暖状态,菲律宾周围对流活动强,在这种情况下,南海上空对流层下层有气旋性距平环流,西太平洋副热带高压偏东,从而使得南海夏季风爆发早;并且,当夏季热带西太平洋也处于暖状态,菲律宾周围对流活动也很强,在这种情况下,西太平洋副热带高压北进时,在6月中旬和7月初存在明显的突跳,从而使得东亚季风雨带在6月中旬明显由华南北跳到江淮流域,并于7月初由江淮流域北跳到黄河流域、华北和东北地区。

Our diplomacy should be tough, and the Ministry of Foreign Affairs or the military or have some influence as long as the government officials have a tough talk about it, then, Viet Nam and other countries will converge immediately, if, as mentioned below;"the South China Sea 12 nautical miles from land other than all the islands, reef sand, the dark beaches, all of China since ancient times, in view of the present annex are around the small country, has listed the common set of 2002's "Declaration on the Conduct of Parties in the South China Sea" as a matter of time in China is' to seek regional peace, we have rice to eat 'principle, and now it appears that the statement has been declared null and void, if necessary, China is determined to force to take the necessary measures to protect China's sovereignty."

我们的外交应该强硬了,外交部也好,军方也好,只要有一定影响的官员出来讲那么一句强硬的话,越南等国马上会收敛的,如果像下面讲的;"南海离陆地12海里以外的所有岛屿、礁沙、暗滩,古来就是中国所有,鉴于目前均被周围小国鲸吞,竟将2002年共同定立的《南海各方行为宣言》视为儿戏,当时中国是本着'寻求地区和平,有饭大家吃'的原则,现在看来,该宣言已废止,中国决心必要时采取必要的武力措施,保卫中国的主权"。

This is an important position on the route of the South China Sea Temple, a port in ancient times, the terminal is outside the vast ocean - the South China Sea, the South China Sea is actually part of the mainland Southeast Asia and around the Pacific, the sea also bear linked to the Pacific, to the Indian Ocean.

处于这条航线重要位置上的南海神庙,在古代有码头,码头外面又是茫茫的大海——南海,南海实际是太平洋靠近东南亚大陆部分,大海又紧连着太平洋,通往印度洋。

This paper analyzes the developmental trends of Southeast Asian countries' policies towards the South China Sea issue in post cold war period from three levels: conflicting countries in the South China Sea disputes; non-conflicting countries in the South China Sea disputes; ASEAN countries.

本文主要从南海争端方国家、非南海争端方国家、东盟3个层次分析了冷战后东南亚国家南海政策的发展动向。

It is reported that this is the 11th summer fishing ban imposedy by China in the South China Sea. Experts say that in the past,Vietnam did not voice opposition to China's operation of fishing ban. Its highlighted opposition is associated with the complication of recent deputes on the South China sea.

据了解,这已经是中国第11次实行南海伏季休渔,有专家表示越南过去从未对中国休渔提出过异议,这次高调反对中国休渔与近期的南海问题复杂化有关。

In the paper, Professor Zhao's historical course engaged in coral reef study and academic results are reviewed: he established the representative section for geological research on Quaternary coral reef, developed engineering geology research on coral reef, elaborated systematically landform development rules of coral reef in the South China Sea, uncovered certain paleo-oceanographical conditions and the new tectonic movement features, studied the historical climate recorded by lagoon of coral reef in the South China Sea and marine geography of coral reef for the first time, investigated comprehensively the only fringing reef of the seacoast of South China continent on western shore of Xuwen County, summarized initially the history of modern coral reef research in China.

文中回顾其从事珊瑚礁研究的历程,并评述其珊瑚礁研究的学术成果:建立了我国第四纪珊瑚礁地质研究的典型剖面;开拓了我国珊瑚礁工程地质研究;系统论述了南海珊瑚礁地貌发展规律,揭示了某些古海洋学状况和新构造运动性质;首次研究了南海珊瑚礁潟湖沉积记录的历史气候;首次进行了我国珊瑚礁区综合海洋地理学研究;较全面开展华南大陆沿岸唯一岸礁徐闻西岸珊瑚礁调查研究;初步总结了我国现代珊瑚礁研究史。

The northern side is the white ream sea, a gram of the 鄂霍 sea, Japanese sea, Yellow sea, the east the china sea and south china sea; go toward the south is the huge east India islands to be divided into the ocean Su pulls the 威 west sea, the Java sea and Timor sea;Became the coralline sea and tower 斯曼 sea again in Australia.

北面是白令海,鄂霍次克海,日本海,黄海,东中国海和南中国海;往南是巨大的东印度群岛把大洋分成了苏拉威西海,爪哇海和帝汶海;在澳洲又形成了珊瑚海和塔斯曼海。

In the northeast part of the South China Sea the high salinity water comes from the Philippine Sea, therefore, biologic productivity was high and there was rich organic matter in sediments during the periods of oxygen-isotopes 2, 4 and 6. In these periods the sedimentation rate was very high, so there were very good material conditions for formation of gas hydrate. In addition, from the end of Miocene to present, the Philippine Sea plate collided with Asian plate in Taiwan area, extruding the northeast part of the South China Sea along northwest direction. The extruding force made fluid in the sediments very active, and this is very good for the formation of gas hydrate.

南海冻北部,在氧同位素2、4、6期,由于菲律宾海的高盐度海水的注入,使这里的生物生产率特别高,陆坡上沉积了丰富的有机物质,加上此期间该处的沉积速率高,为天然气水合物的生成提供了物质条件;另外,自中新世末以来,由于菲律宾海板块与欧亚板块在台湾地区发生碰撞,对南海北部产生北西向挤压,加快了流体在沉积物中的活动,为天然气水合物的生成提供了良好的构造环境。

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