印度洋

Further, we investigated the possible impact of SDP on ENSO event in interannual scale by researching the anomalous characteristics of sea temperature, wind, convergence and divergence, total cloud amount, radiation and so on. The results showed that the influence of SDP on ENSO involve not only the process of positive and negative air-sea feedback, but also the interaction between atmospheric circulation over tropical and subtropical, specially the eastward propagation of anomalous zonal wind from the equatorial Indian Ocean to the Pacific Ocean. Otherwise, it also relates, to some extent, to the transition of large-scale climatic mean flow over the Indian Ocean and Pacific Ocean.

进一步，本文通过分析SDP事件前后期海温、高低层风、低层辐合辐散、高空云量和辐射等的变化特征研究了南印度洋偶极型海温异常在ENSO事件中的作用，结果表明：SDP在ENSO事件中的作用不仅涉及海气相互作用的正负反馈过程，还与热带和副热带大气环流之间的相互作用有关，特别是与东南印度洋海温变化所引起的异常纬向风由赤道印度洋向赤道太平洋传播的过程等有十分直接的关系；同时，SDP对ENSO事件的影响在很大程度上还依赖于大尺度平均气流随季节的变换。

Although he speaks of the Far East between the 15th and 18th centuries as a single world-economy, he says it in fact comprised three "gigantic world-economies: Islam, overlooking the Indian Ocean from the Red Sea and the Persian Gulf, and controlling the deserts stretching across Asia from Arabia to China; India, whose influence extended throughout the India Ocean, both east and west of Cape Comorin; and China, at once a great territorial power- striking deep into the heart of Asia-and a maritime force, controlling the seas and countries bordering the Pacific."

尽管他把15到18世纪的远东说成一个"单一的世界经济系统"，但他说实际上这个系统包含了三个"巨大的世界经济系统：伊斯兰系统，它从红海和波斯湾俯瞰印度洋，控制着横跨阿拉伯到中国的中亚沙漠；印度系统，它的影响力遍及科摩林角的东西两面的整个印度洋；还有中国系统，它曾经是一个有着广阔领土的强大势力，直插亚洲心脏——它也是一个海上霸主，控制着太平洋沿岸的海域和国家。"

SEC velocity in South Indian Ocean and SEC, NEC and EUC in Pacific Ocean is decreased, the speed of SECC in Indian Ocean and the speed of SECC, NECC in Pacific Ocean is increased.

ITF通道的封闭使得南印度洋的SEC大大降低，太平洋的SEC、NEC、EUC减小，而印度洋的SECC和太平洋的SECC、NECC有所增大。

Sensitivity experiments were then designed to further investigate such GIP connections.

基于此，设计了赤道太平洋和印度洋海域纬向风应力异常的4组敏感性试验，去研究太平洋和印度洋海气相互作用的联系。

The built carbon cycle model had been used to simulate the surface distributions, vertical distributions and the isogram distributions along the meridian of various chemical species in the Indian Ocean.

把建好的海洋碳模式应用于印度洋区域，模拟得到了印度洋中与碳有关各化学量的表层分布、垂直分布和沿子午线面的等值线分布。

The locations and orientations of the Subantarctic Front, the primary Polar Front and Southern ACC Front in the ACC of the Southeast Indian Ocean can be identified more precisely by the current distribution derived from ADCP data than by hydrographic data, because these fronts are usually accompanied by strong currents, although the speed coinciding with the SACCF is less than that of the SAF and primary PF.

在东南印度洋远离海脊和海台的深海盆以及海脊和海台的走向与ACC主轴平行的海域，高涡动能主要由周期大于90天的变化产生。SAF在东南印度洋没有一致的季节变化。

Tertiary waves are seismically generated acoustic waves that can propagate over great distances in the SOund Fixing And Ranging channel. On 2004/12/26, big Sumatra earthquake ( Mw =9.3) occurs at the Sumatra island. A huge tsunami excited by the energy from the big Sumatra earthquake causes a great lose, thus a lot of scientists from all over the world pay a lot attention to such big Sumatra earthquake.

T-波是由海底地震或者海陆边界俯冲带附近地震激发，并在海洋低速层中传播的声波。2004年12月26日，在印度洋东部印尼苏门答腊岛附近发生 MW =9.3级大地震，其产生的能量在印度洋中激发了巨大的海啸，造成了严重的人员伤亡和财产损失，受到了世界科学家们极大的关注。

When the autumn SST in the Indian Ocean is wormer, winter temperature in China is also higher. When the Indian Ocean Dipole is positive, temperature is high in the Northeast China and low in Southwest China; and the East Asian winter monsoon is weaker.

当印度洋海温一致变化时，中国温度变化也呈一致；当印度洋海温距平偶极振荡时，中国东、西部的冬季气温也出现偶极变化的现象；印度洋海温偶极振荡正位相年时，东亚冬季风偏弱，中国东北部气温偏高。

The results show that the most significant mode of IO SST in recent 50 a is the warming trend at most of the ocean basin and there is abrupt warming in 1976,1986 and 1996 respectively.

自1999年Saji等[1]和Webster等[2]提出&印度洋偶极子&以来，人们对热带印度洋SST变化十分关注，此后开展了很多工作，认为热带印度洋中也存在类似太平洋ENSO的大尺度海

The results obtained revealed that:(1) the Pacific yellowfin has larger ring-radii as well as scale size than the Indian Yellowfin;(2) the specimens from the western Indian have larger value in scale size and ring-radii than those from eastern Indian;(3) there is a significant difference in the estimated growth curves between male and female for the Pacific specimens, but not for the Indian specimens; and (4) it is convinced that there are two yellowfin groups in the Indian Ocean, viz., one concentrates in the western Indian and the other densely distributes in the waters around Sunda Islands and Banda Sea; intermingling of these two groups is supposed to be occurred around 100°E in the season of northern summer.

3李氏现象在太平洋和印度洋都很显著。(4)年轮每年形成二次，时间为2～4月及8～10月。(5)有关成长的parameters如下：太平洋K=0.386 L=174.9 t0=0.05 东印度洋 K=0.278 L=212.7 t0=-0.19 中印度洋 K=0.290 L=215.6 t0=-0.01 西印度洋 K=0.349 L=191.1 t0=0.06 (6)由钓获率的分布、体长组成和其他生物学资料及以往之结果加以综合分析，显示印度洋的黄鳍鲔可分为东、西两个族羣，一为以班达海和小巽他羣岛附近海域为中心的东方羣，另一则以西部印度洋赤道流域为中心的西方羣。此两羣在100°E附近发生混合交流。当北半球的夏天时，此混合交流的现象较为显著。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。