southeast by east
- southeast by east的基本解释
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东南偏东
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There are Hannan block in the northwest and Huangling block in the east. Its extended direction is east-northeast in the northwest area, east-west in the middle area and east-northeast in the southeast area,being a southwestward arc made up of many thrust nappes.
该带西北端受汉南地块限制,东部有黄陵地块的阻挡,其展布方向由西北部的北北东向、中部的近东西向、至东南部的北东东向,呈一向西南凸出的弧形,是由一系列呈向西南突出的巨型逆冲推覆断裂带构成。
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This thesis contains five chapters. Chapter 1 introduces the cause, purpose and value of the thesis and the problems that affect the existence of the east-and-west-facing residence. Chapter 2 analyzes the affecting factors of the facing of residence including the thermo-comfortability, the spiritual and mental state and the ecological environment etc. Chapter 3 analyzes the specific circumstances, under which the east-and-west-facing residence is practicable. For example, in order to enjoy the view, to make good use of the land and to form the endocentric residential area, we can choose the east-and-west-facing residence. Chapter 4 puts forward some measurements, including the planning design, the architecture design and the constitution design, to make the east-and-west-facing residence hot-proof so that we can eliminate the most disadvantageous factor in the south. Chapter 5 gives some examples of the east-and-west-facing residence in the south.
本文分五章,第一章提出本文研究的起因、范围、目的、意义及南方地区东西向住宅存在的问题;第二章分析了影响住宅朝向的各因素(包括热舒适性、精神心理、生态环境等);第三章分析了东西向住宅在一些特定条件下(如景观、地形地貌、小区内聚围合等)在南方地区的适应性;第四章提出了解决南方地区东西向住宅防热的一系列(规划设计、建筑设计、构造设计等)措施,以解决东西向住宅在南方地区存在的最大障碍;第五章列举了南方地区东西向住宅的一些实例;最后在结语中总结了东西向住宅在南方地区存在的现实意义及实用价值,并展望了住宅建设发展的前景。
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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。
- 更多网络解释 与southeast by east相关的网络解释 [注:此内容来源于网络,仅供参考]
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southeast by east:东南偏东
west by south西偏南 | southeast by east东南偏东 | southeast by south东南偏南
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southeast by east:abbr. sebe; 东南偏东
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SE by E =southeast by east:东南偏东
Settlement 沉陷,沉降 | SE by E =southeast by east 东南偏东 | Supporting ring 支承环;垫环