查询词典 monsoon

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。

The results show that when the tropical western Pacific is in a warming state in spring, convective activities are intensified around the Philippines. In this case, there is a cyclonic anomaly circulation in the lower troposphere over the South China Sea, and the western Pacific subtropical high shifts eastward, thus, the early onset of the South China Sea summer monsoon can be caused. Moreover, when the tropical western Pacific is also in a warming state, convective activities around the Philippines are also strong in summer, since the western Pacific subtropical high abruptly shifts northward in mid-June and early July during its northward advance in this case, the abrupt northward-shift of the East Asian summer monsoon rainband from South China to the Yangtze River and the Huaihe River valleys is obvious in mid-June and this monsoon rainband again jumps northward from the Yangtze River and the Huaihe River valleys to the Yellow River valley, North China and Northeast China in early July.

分析结果表明：当春季热带西太平洋处于暖状态，菲律宾周围对流活动强，在这种情况下，南海上空对流层下层有气旋性距平环流，西太平洋副热带高压偏东，从而使得南海夏季风爆发早；并且，当夏季热带西太平洋也处于暖状态，菲律宾周围对流活动也很强，在这种情况下，西太平洋副热带高压北进时，在6月中旬和7月初存在明显的突跳，从而使得东亚季风雨带在6月中旬明显由华南北跳到江淮流域，并于7月初由江淮流域北跳到黄河流域、华北和东北地区。

The achievements have been made such as the records revealed by climatic proxies,show the instability of the East Asian monsoon climates and warm phases; a short term warm event and a cold reversal before the termination of the penultimate; cold Henrich fingerprint in lake sediments of the Tibetan Plateau; the instability of oxygen isotope stage 5e and Holocene climates; the spatial variability of East Asian monsoon precipitation during the Younger Dryas and the increased variability of the recent centennial East Asian monsoon precipitation.

发现在倒数第二次冰期结束前一次持续时间非常短暂的气候温暖事件和寒冷回返事件，发现我国青藏高原湖相沉积物中保存了Henrich寒冷事件的烙印、氧同位素阶段5e和全新世的不稳定性，Yonger Dryas东亚季风降水的空间变率以及最近100年东亚季风降水变率增大等。

The results show that:① The onset of the cell of summer monsoon circulation over East Asia is nearly 5 pentads earlier than that over South Asia, while the withdrawing of the summer monsoon from the mainland of China is about 5 pentads later than its withdrawing from Indian continent;② The East Asian summer monsoon undergoes two stages of continuous e...

结果表明：①东亚地区夏季风环流圈的建立比南亚地区夏季风环流圈的建立大约早5个候。

Using the precipitation of the Indian summer monsoon onset process by the method of EOF expansion, the following conclusions can be found. The onset of the monsoon is mainly seen as the augmentation of precipitation and the rapid advance of monsoon rain belt with sudden change in the distribution of its space and time.

用南亚夏季风爆发前后的降水量资料作了经验正交函数分解，分析表明，南亚夏季风的爆发主要体现在降水的突然增加和季风雨带的快速推进上，雨带的时空分布有突变的特点。

The quantificational correlations between summer and winter monsoon intensity reflected by annual monsoon amplitude were the fixed proxy of monsoon variations of dry and humid.

季风年变幅反映的夏季风与冬季风强度的定量组合关系，是季风气候干湿变化的定量代用指标。

east monoon ; barotropic monsoon pattern ; baroclinic monsoon pattern ; mixed monsoon pattern ; thermal difference between continent and ocean,planetary wind belt

典型的由海陆热力差异所引起的季风是印度季风和南海季风，在这些地区冬季盛行东北风，夏季盛行西南风。

The results showed that 9 natural vegetation types were distributed in 6 gradients. Except gradientⅠ, the dominant vegetation types along other gradients were all monsoon evergreen broadleaved forest. Gradient had greater effects on the distribution of seasonal rainforest and temperate coniferous forest, had some effects on the distribution of mountain rainforest, deciduous monsoon threat and river valley savanna forest, had smaller effects on monsoon evergreen broadleaved forest had no effect on warm-hot savanna forest and tropical bamboo forest.

结果表明：9个自然植被类型在6个坡度级均有分布；6个坡度级中除Ⅰ坡度级优势类型是水域外其他坡度级的优势植被类型均是季风常绿阔叶林；坡度对季节雨林和暖温性针叶林的分布影响较大，对山地雨林、落叶季雨林和河谷稀树灌木草丛的分布有一定影响，对季风常绿阔叶林和暖热性稀树灌木草丛的分布影响较小，对暖热性针叶林和热性竹林的分布无影响。

The comparisons of the corresponding time coefficient curve for1983 with those for 1981 and 1982 indicate that the summer monsoon circulation in ElNino years is weak,and the circulation transition from winter monsoon pattern tosummer monsoon pattern is...

其1983年的时间系数曲线与1981、1982年的差异表明，ElNino年夏季风环流弱，且其向北半球夏季型的转变期较正常年推迟。在西太平洋地区它表现为副高北进的滞后，用IAPGCM作的一个相应的数值试验证实了上述结果的正确。

For every one of my New Year resolutions, I have been a backslider for years.

说到我的新年决心，我每年都做

With empathy and focus on a feeling level, we can all relate to the common ground of mutuality of emotions.

有了同情心和感觉上一级的重点，我们都可以涉及到相互的情感共同点。