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太平洋

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Central Pacific seismic belt which is the world's longest seismic zone, the West Bank from the Americas north, along the Aleutian Islands, the Kuril Islands south, as Japan, China to the South Pacific islands, the Pacific surround week, the release of energy accounted for 80 percent.

其中环太平洋地震带是世界最长的地震带,从美洲西岸北上,沿阿留申群岛、千岛群岛南下,经日本、中国到南太平洋诸岛,环绕太平洋一周,释放能量占80%。

Circum-Pacific seismic belt volcanoes, including the eastern Pacific, North America and South America's western mountains, as well as South and North America between the Caribbean - Antilles region, the western edge of the Pacific, the Aleutian Islands, Kamchatka Peninsula, the Kuril Islands, south through Japan, the Philippines, New Zealand and so on until a series of islands and island.

太平洋火山地震带,包括太平洋东面、北美洲和南美洲的西部山地,以及南、北美之间的加勒比—安的列斯地区,太平洋西部边缘的阿留申群岛、堪察加半岛、千岛群岛,向南经日本、菲律宾,直到新西兰等一系列群岛和岛屿。

The results show that corresponding to the positive / negative phase of interdecadal modes of the North Pacific SST, the anomalous patterns of the atmospheric circulation and climate in positive phase are opposite to that in negative phase, it indicates an important impact of these interdec...

其结果极为清楚地表明,对应北太平洋SST的年代际模的正、负位相,大气环流和气候异常的形势都近乎相反,充分说明SST年代际模的重要作用;由于北太平洋SST的两个年代际模有十分相近的水平结构特征,它们对大气环流和气候的影响也有十分相似的特征;北太平洋海温年代际模对大气环流的影响在中高纬度地区呈正压结构特征,而在热带地区的响应主要有斜压结构特征。

The Western Pacific subduction zone in the northeast part of China is located at boundary of the Eurasia and the Western Pacific plate.

中国东北西太平洋俯冲带位于欧亚板块与西太平洋板块的交界部位,西太平洋板块在日本海沟以约29°的角度俯冲到欧亚大陆下。

W is taken as the boundary of the East Pacific Ocean and West Pacific Ocean.

太平洋的总量为17.8GW,而西太平洋为40.6GW,两者差异较大(以160°W作为东、西太平洋分界线)。

In the light of sea regions where El Nino events occurred, ENSO events are separated into two categories- the equatorial Pacific warming and the mid-Pacific counterpart, which exert influence directly on a WPSH through a Walker circulation asymmetrical zonally, in such a way that there an El Nino year- a weak Walker circulation- a more intense and southward WPSH-late onset of South-China sea summer monsoon - a more southward and vigorous summer WPSH- the mid-lower valleys of the Yangtze river hit by flood.

上述两种类型的ENSO均可直接通过纬向非对称的Walker环流直接对西太平洋副高产生影响,表现为:El Nino年—Walker环流弱—西太平洋副高偏强、偏南—南海夏季风爆发晚-夏季西太平洋副高偏南、偏强—长江中下游涝。

PA-457 was not just another Taxol, the anticancer drug that required the controersial felling of rare yew trees until a semisynthetic substitute was found. Panacos did not need a steady source of Taiwanese herbs. Betulinic acid could be extracted from ubiquitous plane and birch trees, and a subsequent processing step yielded the desired molecule.

PA-457不像抗癌药物太平洋紫杉醇:在太平洋紫杉醇的合成代替品出现前,砍伐罕见的太平洋紫杉一直引发争议;Panacos并不需要有稳定供应的台湾药草,桦木酸能从普遍存在的悬铃树和桦树中提炼,并且只要一个后续处理步骤,就可以制造出所需的分子。

The results are shown as below.1 Tectono-thermal evolution: The history of the Songliao basin is divides into four stages, high-temperature doming and extension, high-temperature rifting, low-temperature depression, and low-temperature shrinkage. Numerical simulation of mechanical process shows that the basin appeared in the early- to late- Jurassic as a result of rapid low-angle subduction of the Pacific plate towards the northwest, of movement of the Siberian block towards the southeast, of many other influences such as internal thermal stress in the mantle, gravitational force, stress of phase transition, etc. Both the Pacific plate and the Siberian block slowed down in the early Cretaceous, and almost stopped in the middle Cretaceous with the rapid decrease of abnormal heat in the mantle below.

盆地构造热演化力源机制数值模拟研究表明:早、中侏罗世至晚侏罗世晚期,盆地演化主要是太平洋块体向北西方向以低角度快速俯冲和西伯利亚块体向东南俯冲共同作用的结果,同时也与地幔内部热力、重力、相变力以及地球自转及公转速度变化效应和上覆块体绝对运动的作用有关;早白垩世早期至早白垩世中期,来自东部太平洋块体俯冲作用的减弱,而这一时期影响盆地演化的主要力源是地幔内部热力、重力、相变力以及地球自转及公转速度变化效应和来自西伯利亚块体俯冲作用;进入早白垩世晚期至晚白垩世早期,由于双重俯冲带中西侧俯冲作用带基本停止活动,而本区地幔热能的快速衰减则控制盆地的构造热演化;晚白垩世晚期以后,太平洋块体活动加强和地幔热运动是影响盆地演化的主要动力。

It is justified that during the stronger winter monsoon, the westerlies are intensified over the equatorial western Pacific and the in situ SSTA is positive, while and the easterlies are intensified over the equatorial eastern Pacific and the SSTA is negative because of the air-sea interaction over the Northern Pacific.

证明由于北太平洋的上的海—气相互作用,强东亚冬季风期间,赤道西太平洋西风加强,SST为正异常;赤道东太平洋东风加强,SST为负异常。

Northwest Pacific STH should be seen as two part, the west Pacific STH and mid-Pacific STH due to their marked difference in horizontal and vertical structure.

1不论是从水平环流上还是从垂直结构上,都应将西北太平洋副高分为中太平洋副高和西太平洋副高,它们具有显著不同的特征。

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