季风的

基本解释 (translations)

monsoonal

与季风的相关的网络例句 [注：此内容来源于网络，仅供参考]

Lying in the North Hemispheric Subtropical High, the middle reaches of the Yangtze, as a key passage of the East Asian monsoon, is climatologically characterized by the energy exchange between the trade wind and westerlies as well as water-vapor convergence of the Southeast and Southwest monsoons.

长江中游地处北半球副热带，是东亚季风的必经之地。副热带附近东风与西风之间的能量交换和东南季风与西南季风的水汽辐合造就了该区环境的过渡带特征，使它灵敏地响应气候的变化。

The relationships between wind field at low level and convection activities over the South China Sea are investigated based on pentad wind and OLR data from NCEP. The onset time and intensity of SCS summer monsoon are determined by area-averaged zonal wind component over central and south SCS. So we possess long-term time sequence of SCS summer monsoon activities for the period of 1949～1998. Interannual and interdecadal variations are examined by using this time series.

利用NCEP风场资料和候平均向外长波辐射资料分析了南海区域低层风场与对流活动的关系，在此基础上，采用南海中南部的纬向风平均值来定义南海夏季风的爆发，确定了长序列（1949～1998）的南海夏季风爆发日期和强度指数，并研究南海夏季风活动的年际和年代际变化特征。

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。

Precipitation in Heilongjiang Province of China increased slightly from 1960 to 2000. Adopting the method proposed by Arthur N. Samel, we separated monsoon rainband rain and calculated the initial and final date of monsoon rainband of each year and each station.

为了分析黑龙江省夏季季风的变化规律和夏季季风与年降水之间关系的变化，采用Samel发明的方法，用逐日降雨量数据计算每一年夏季季风到达、离开、停留在黑龙江省的时间。

Based on NCEP/NCAR reanalysis data, the structure and variation of Tropical Easterly Jet and its relationship with the distribution of rainfall in Asia and Africa are analyzed. In addition, the Asian summer monsoon indices are reappraised and the secular variation of monsoon is studied.

本文主要是用NCEP/NCAR再分析资料研究了热带东风急流的结构，多尺度变化特征及其与亚非季风降水的关系，并且在此基础上重新评估亚洲夏季风指数及研究季风的长期变化，最后比较了NCEP/NCAR与ERA-40再分析资料的差异。

E. , approximately four months; 2 the active periods occur much longer than the non-active periods; the main climatic characteristics of the non-active periods, compared with the active periods, is weaker monsoon with westerlies at 850-hPa and easterlies at 200-hPa on the deviation fields of circulations over the SCS (active time minus non-active time); it is warmer in the active periods than in the non-active periods at lower and upper levels; 3 in most circumstances, the low frequency vibrations of the summer monsoon and its rainfall are quite in phase.

2其中活跃期出现时间要比非活跃期长的多。与活跃期相比非活跃期主要气候特征表现为季风的减弱，在环流的偏差场上在南海上空850hPa上为西风，200hPa上为东风，活跃期高低空都比非活跃期要暖一些。(3)在多数情况下夏季风和夏季风降水的30-60天的低频振荡比较一致。

For the climatic characteristics of the onset of the SCS summer monsoon, results reveal: 1 the SCS summer monsoon brusts at the 4th pentad in May; 2 the onset of the SCS summer monsoon is closely related to the southwesterly monsoon over the eastern Bay of Bengal, as induced by the intensification and eastward advancement of the latter; 3 the rainy season of the SCS summer monsoon bursts after the onset of the SCS summer monsoon basically; and 4 the atmospheric circulations exhibit rapid changes at different heights over the SCS and its adjacent districts, during the establishment peroid of the SCS summer monsoon, these include: i in lower troposphere, the southward expansion and deepening of the Indo-Burma trough; ii in middle troposphere, the rapid easterward retreat of the western Pacific subtropicl high form the SCS region, iii in upper troposphere, the fast radiation of the easterlies form the center of the SCS region to the whole of it apparently.

对于南海夏季风建立的气候特征，研究发现：(1)南海夏季风的建立具有爆发性，爆发的时间是5月第4候。(2)南海夏季风的建立与孟加拉湾东部西南季风有密切的关系，是孟加拉湾西南季风发展和东移的结果。(3)南海的夏季风雨季基本上是随着夏季风建立而建立的。(4)在南海夏季风建立期间，南海及其邻近地区高低空环流都有急速的变化，在对流层低层表现为印缅槽的南扩和加深，在对流层中层表现为西太平洋副热带高压迅速东移撤出南海地区，在对流层高层最明显的变化是东风带迅速地从南海中部向北扩展到整个南海地区。

We also calculate annual monsoon Intensity index and Front Location Index by averaging the indices of 18 pentads in summer. The results show that the summer rainfalls in China have tight relation not only to the intensity of Monsoon, but also to the location of Monsoon. When Monsoon is strong and in North, excessive rainfalls in North and few in South; when Monsoon is weak and in North, few in China all over; when Monsoon is strong and in South, excessive in China all over; when Monsoon is weak and in South, excessive in South and few in North.

还计算了夏季18个候平均得到的逐年季风强度和季风位置，结果表明中国夏季降水的形势不仅和季风强度密切相关，还和当年季风的位置有着紧密的联系，季风偏强偏北时，降水北多南少；季风偏弱偏北时，全国少雨；季风偏强偏南时，全国多雨；季风偏弱偏南，降水南多北少。

Asian summer monsoon, one of the earth′s most energetic weather events, undoubtedly plays a key role in the variability of the general circulation. In this paper, through both calculation for the correlation coefficients between the monsoon indices and the geopotential height and the anomalous composite of the strong or weak ASM pentads, it is shown that the activity of the ASM...

本文通过夏季风指数与北半球环流的相关计算以及强、弱季风候北半球环流异常合成的分析发现，亚洲夏季风的活动会激发北半球夏季大气环流遥相关型，其主要相关中心均出现在季风区的下游地区，即从亚洲经太平洋至北美洲一带，除了表现出正负中心交替出现的波列状结构外，该遥相关型在太平洋地区还表现为一对南北向的偶极子异常型，我们将这一遥相关型称为亚洲太平洋北美型

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。

与季风的相关的网络解释 [注：此内容来源于网络，仅供参考]

monsoon climate：季风气候

季风气候(monsoon climate) 由于海陆热力差异或行星风带随季节移动而引起的大范围地区的盛行风随季节而改变的现象,称季风. 季风气候受季风支配地区的气候. 最主要特征是一年中随同季风的旋转,降水发生明显的季节变化,东亚与南亚为两个典型的季风气候区,

currents：洋流

开始讲洋流(currents)有三种:水平,上升和下降. 主要讲上升洋流(upwelling current)的成因是季风(prevail),季风的形成是因为海洋与陆地上空的气压不同(有题),导致空气由海洋吹向陆地,而季风带动海洋表面的海水,将海水吹向海岸(有题),海水碰触到海岸后会转向沿着岸际向北或...

currents：流

开始讲洋流(currents)有三种:水平,上升和下降. 主要讲上升洋流(upwelling current)的成因是季风(prevail),季风的形成是因为海洋与陆地上空的气压不同(有题),导致空气由海洋吹向陆地,而季风带动海洋表面的海水,将海水吹向海岸(有题),海水碰触到海岸后会转向沿着岸际向北或...

etesian：例年的/季节风的

eternize /使永恒/使不变/使不朽/ | etesian /例年的/季节风的/ | etesians /地中海季风/

monsoon forest：季雨林 / 季风林

美洲雨林,非洲雨林 中国热带雨林:3个群系组,12个群系 (2) 红树林(Mangrove):东方群系,西方群系,中国的红树林 (3) 季雨林(季风林)(Monsoon forest):不确切而多争议的类型 (4) 常绿阔叶林(Evergreen broad-leaved forest):除欧洲外,

moustache f：髭,小胡子,猫狮鼠等的胡须

3826 mousson f. 季风,信风,季风转换期 NULL NULL | 3827 moustache f. 髭,小胡子,猫狮鼠等的胡须 NULL NULL | 3828 moustique m. 蛟,小孩,矮小的人 NULL NULL

Eulalia speciosa：金茅

海拔1000米以下的各种酸性灰化红黄壤上,画眉草(Eragrostispilosa)、金茅(Eulalia speciosa)、拟金茅(Eulaliopsis binata)等为主的山地草坡. 由于本地区受到两洋季风的影响,加之特殊的河谷地貌,热带种属沿河谷向北分布,

Monsoons：季风

这样,使不同压力差的地区产生了趋于平衡的空气流动,形成了风. 自然界常见的几种风包括热带气旋(tropicalcyclone)、台风(typhoons)、飓风(hurricanes)、季风(monsoons)和龙卷风(tornadoes)等,下面分别进行介绍.

the giant saguaros, one of the biggest of all cacti：巨大的弁庆柱 -- 一种世界上最大的仙人掌

When the summer monsoon blows in,|当夏季季风吹来... | the giant saguaros, one of the biggest of all cacti,|巨大的弁庆柱 -- 一种世界上最大的仙人掌 | are ready to take full advantage of it.|准备充分利用雨...

Magna Graecia：大希腊

两三千年前,古希腊人就是通过这片丝绒般安谧的大海航向意大利南部、西西里岛,建立起一个个"大希腊"(Magna Graecia)殖民城邦的. 整个夏季,爱琴海处于干爽的季风的拂照之下. 通常在每天下午达到最大风速,傍晚时衰减. 但偶尔也有例外,