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欧亚大陆

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Eurasia comprises the whole of the northern part of the European and asiatic land-mass, from Portugal to the Bering strait

欧亚国占欧亚大陆的整个北部,从葡萄牙到白令海峡。

Eurasia is home to most of the world's politically assertive and dynamic states...

欧亚大陆集中了世界大多数政治上自信而充满活力的国家,历史上所有问鼎世界的超级大国都源于欧亚大陆

During the four years study on the project, we develop a dynamical forecast model that describing the subtropical ridge surface. A new theory on the role of the land-sea thermal difference on the formation of the Subtropical High is advanced. It is concluded that in the summer subtropics over each continent and its adjacent ocean LO, SE, CO, and a double-dominant heating from west to east compose a LOSECOD heating quadruplet. The influence of the Eurasia continent on SH varies according to the seasonal variation. From the ideal numerical simulation it is shown the important role of the Eaiuan continent and the huge topography on the mechanism of formation and mantanence of the SH during the summer. It is verified by the numerical simulation that the extension of the subtropical continent into the tropics greatly enhances the " East Asian monsoon". Through the Rossby energy dissipation theory it is verified that the deep latent convective heating induces the onset of the South China Sea monsoon over the Bay of Bengal. The relationship and mechanism between the precipitaiton over the East Asia and the Subtropicla high is illustrated by the data. It is also found the close phase lock between the east-west shift of the SH and the disturbence of the east wind belt over the tropical troposphere. The interaction between the structure and activity feature of the SH and the Meiyu over the Yangtze-Huaihe river valley is revealed from the data. The numerical simulation verified the impact of the different SH pattern on the path of the typhoon.

本项目的研究发展了描述副热带高压脊面变化的动力模型,提出了夏季副热带地区四叶型非绝热加热分布型及相应环流拼图的创新理论;明确了大陆尺度的海陆热力差异在副热带高压形成中的作用;指出欧亚地形对副热带高压和气候的影响随季节变化而变化,通过数值试验证明春季青藏高原的感热加热对亚洲夏季风的爆发地点起了"锚定"的作用,进一步证实了副热带高压断裂和亚洲夏季风的最早爆发地点发生在孟加拉湾东岸;利用Rossby波能量频散理论证明了孟加拉湾深对流潜热释放诱导南海季风爆发的机制;揭示了东亚季风降水的季节内变化与西太副高的关系及机理;揭示了西太副高与东西风带中扰动之间的相互作用过程,指出西太副高的东西活动与热带对流层上空东风带扰动和中纬度西风带扰动的移动和锁相密切相关;研究了夏季淮河流域梅雨期间副高结构和活动特征及其与江淮暴雨的相互作用;验证了不同副热带高压形态对台风路径的不同影响;通过数值试验证明了欧亚大陆和青藏高原等大地形对副热带高压形成和维持的重要作用。

The results show that the present convergence rate of the India plate is 21.8 mm/a with a dipping 8.1°to the north. This is in good agreement with various geologic predictions of 18mm/a in past 2~3 million year implying a stable convergence rate of the India plate in a very long duration.

本文 结果与从地质推断的在过去2~3Ma时期内,印度板块向欧亚大陆俯冲速率平均为18mm/a,有较好的一致性,表明在较长时间内,印度板块向欧亚大陆俯冲的速率仍然是稳定的。

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。

The main results are listed as following: 1. Phylogeographic study on Croomia The relationships and distribution of cpDNA haplotypes suggested that Croomia had been widely distributed in ancient eastern Asian and northern American; the origin and distribution center of Croomia were concentrated on the mountains comprised Mt.

Croomia亲缘地理学根据叶绿体DNA(trnL-F、atpB-rbcL)单倍型的关系和分布推测,Croomia在古欧亚大陆和古北美大陆有着较广泛的分布;我国的黄山和天目山一带是Croomia的分布、起源中心,其散布路线是从中国大陆到日本,再到美洲古大陆;北美种群与东亚种群分离较早;东亚种的分化时间比较晚。

The collision of Indian plate and Euro-sian plate affects Fujian and its neighbouring sea region by several blocks side-ransferring in China continent.The obduction and jam of Philippines-ea plate to Taiwan southeast margin of Euro-sia continent also affects this region. The jointly affection still exists today. The former is stronger than the latter while the velocity field of the former is homogeneous and the one of the latte is not homogeneous.

印度板块对欧亚板块的碰撞通过中国大陆内部各块体间的侧向传递和菲律宾海板块对台湾欧亚大陆东南沿的仰冲与挤压,同时作用到福建及其邻近海域此种联合作用现今仍在继续进行中,前者的影响比后者更强烈,但前者形成的速率场均匀,而后者不均匀。

The "unsampled pig herd" theory was suggested by Smith and his colleagues, who concluded that "the progenitor of the S-OIV epidemic originated in pigs", and the "long unsampled history observed for every segment" of the S-OIV genome "suggests that the reassortment of Eurasian and North American swine lineages may not have occurred recently, and it is possible that this single reassortant lineage has been cryptically circulating rather than two distinct lineages of swine flu", and that "Movement of live pigs between Eurasia and North America seems to have facilitated the mixing of diverse swine influenzas, leading to the multiple reassortment events associated with the genesis of the S-OIV strain."

&无取样猪群&论,由Smith和他的同事提出,断定&流行猪源流感病毒的祖辈起源于猪&,猪源流感病毒基因上&观察到的每一个基因片断长期无样本历史&表明,&欧亚族和北美族猪流感病毒重配可能没有在最近发生,也许这种重配病毒已经神秘传播,而不是两个不同族猪流感病毒&,而且&在欧亚大陆与北美之间的生猪运输似乎促进了不同的猪流感病毒混合,导致了和猪源流感病毒毒株基因关联的多重配事件。&

The "unsampled pig herd" theory was suggested by Smith and his colleagues who concluded that "the progenitor of the S-OIV epidemic originated in pigs" and the "long unsampled history observed for every segment" of the S-OIV genome "suggests that the reassortment of Eurasian and North American swine lineages may not have occurred recently and it is possible that this single reassortant lineage has been cryptically circulating rather than two distinct lineages of swine flu" and that "Movement of live pigs between Eurasia and North America seems to have facilitated the mixing of diverse swine influenzas leading to the multiple reassortment events associated with the genesis of the S-OIV strain."

&无取样猪群&论,由Smith和他的同事提出,断定&流行猪源流感病毒的祖辈起源于猪&,猪源流感病毒基因上&观察到的每一个基因片断长期无样本历史&表明,&欧亚族和北美族猪流感病毒重配可能没有在最近发生,也许这种重配病毒已经神秘传播,而不是两个不同族猪流感病毒&,而且&在欧亚大陆与北美之间的生猪运输好像促进了不同的猪流感病毒混合,导致了和猪源流感病毒毒株基因关联的多重配事件。&

During the four years study on the project, we develop a dynamical forecast model that describing the subtropical ridge surface. A new theory on the role of the land-sea thermal difference on the formation of the Subtropical High is advanced. It is concluded that in the summer subtropics over each continent and its adjacent ocean LO, SE, CO, and a double-dominant heating from west to east compose a LOSECOD heating quadruplet. The influence of the Eurasia continent on SH varies according to the seasonal variation. From the ideal numerical simulation it is shown the important role of the Eaiuan continent and the huge topography on the mechanism of formation and mantanence of the SH during the summer. It is verified by the numerical simulation that the extension of the subtropical continent into the tropics greatly enhances the " East Asian monsoon". Through the Rossby energy dissipation theory it is verified that the deep latent convective heating induces the onset of the South China Sea monsoon over the Bay of Bengal. The relationship and mechanism between the precipitaiton over the East Asia and the Subtropicla high is illustrated by the data. It is also found the close phase lock between the east-west shift of the SH and the disturbence of the east wind belt over the tropical troposphere. The interaction between the structure and activity feature of the SH and the Meiyu over the Yangtze-Huaihe river valley is revealed from the data. The numerical simulation verified the impact of the different SH pattern on the path of the typhoon.

本项目的研究发展了描述副热带高压脊面变化的动力模型,提出了夏季副热带地区四叶型非绝热加热分布型及相应环流拼图的创新理论;明确了大陆尺度的海陆热力差异在副热带高压形成中的作用;指出欧亚地形对副热带高压和气候的影响随季节变化而变化,通过数值试验证明春季青藏高原的感热加热对亚洲夏季风的爆发地点起了&锚定&的作用,进一步证实了副热带高压断裂和亚洲夏季风的最早爆发地点发生在孟加拉湾东岸;利用Rossby波能量频散理论证明了孟加拉湾深对流潜热释放诱导南海季风爆发的机制;揭示了东亚季风降水的季节内变化与西太副高的关系及机理;揭示了西太副高与东西风带中扰动之间的相互作用过程,指出西太副高的东西活动与热带对流层上空东风带扰动和中纬度西风带扰动的移动和锁相密切相关;研究了夏季淮河流域梅雨期间副高结构和活动特征及其与江淮暴雨的相互作用;验证了不同副热带高压形态对台风路径的不同影响;通过数值试验证明了欧亚大陆和青藏高原等大地形对副热带高压形成和维持的重要作用。

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