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In addition, antiphase relationship in precipitation changes between the northern Tibetan Plateau (climatically controlled by westerlies) and southern Tibetan Plateau (mainly influenced by Indian monsoon circulation) exists on decadal to centennial timescale.

不仅如此,在分属西风和季风影响区的青藏高原北部和南部,年代际-百年尺度上降水变化也表现出反相位关系。

In the austral summer,wind speed 10 meters above the sea surface turn to the lowest in the whole year.

南极海域夏季为全年风场最弱的季节,在整个40°S以南海域以偏西风为主。2。

Best of all the well-known lyric pieces is Shelley's "Ode to the West Wind"; here Shelley's rhapsodic and declamatory tendencies find a subject perfectly suited to them.

雪莱最著名的抒情诗当属"西风颂",这首诗语气狂热,宜于诵读。

The midlatitude Asian continent can be roughly divided into two distinct climatic regions: the humid easternsouthern part of Asia mainly controlled by monsoon circulation and inland arid Asia (including the coldarid northern Tibetan Plateau) in the western part dominated by the midlatitude westerlies.

中纬度亚洲地区存在主要受季风环流影响的东南部湿润地区和主要受西风环流控制的内陆干旱区(包括青藏高原北部高寒干旱区,简称西风区)。

In the second cycle (late July-late September), precipitation and west wind extend northeastward, precipitation become strong and this time is the most prosperous period of WNPSM.

到了第二循环(7月下旬—9月下旬)季风降水和西风都明显向东向北推进,降水强度增大,是西北太平洋夏季风的强盛时期。

The forecasting of turning typhoon is a difficulty, In this paper, the circulations of six turnning typhoons and their relationship with westerly in 2008 are analysed to get the conclusions below: weather typhoon would turn or not is in close relation to westerly when it betweens continenta1 high and West Pacific subtropical high?

分析了2008年6个东北转向台风的环流形势及其与西风槽等的关系,得出当台风处于大陆高压和西太平洋副热带高压之间的中纬度西风槽前时,其转向与西风槽密切相关的结论。

In China, the west is nipping bise, often reminiscent of dongfeng floating down, a British idea of the west, warm, heralds spring's arrival, will make the earth, but in the spring wind is bone-chilling English culture Middle East wind.

在中国,西风是刺骨的寒风,经常使人联想起离愁别绪,东风则像是英国人心目中的西风,温暖,预示着春天的到来,会使大地春意盎然,而在英语文化中东风才是刺骨寒风。

Also the seasonal variation of mean gedstrophic westerly, and the distribution of extra-long wave at this layer were analyzed.

分析了南半球对流层500hPa平均地转西风随纬度的分布特点,平均地转西风季节变化特点,计算分析了南半球位势高度对纬向平均的偏差,分析了超长波的分布特征。

Along 90°E the easterly wind in mid-upper layer is obviously weakened to the south of the plateau, and the westerly wind in mid-upper layer along 140°E is enhanced to the south of 35°N but it is obviously weakened to the north of 35°N.

利用p-σ九层区域气候模式进行高原隆升对东亚副热带西风急流影响的敏感性试验,分析高原隆升过程中西风急流垂直结构和水平结构的变化,并对其变化的原因进行初步分析。

As a result, a weak indirect cell is formed in high latitudes. By the 36th time step, the model atmosphere accomplishes the transition form one-cell circulation to two-cell circulation. There is a momentum source in the upper subtropical region. During the transition, the"polar westerlies jet"gets weakened and vanishes at the end, while the subtropical westerlies jet gets strengthened. At this two-cell stage, the generation and dissipation of westerly angular momentum do not balance each other, and the atmosphere is still at an unstable state with great surplus of angular momentum generation.

随着模式的运行,直接环流加强,地表东风带制造西风角动量加大,上支气流的加强,同样在科氏力的作用下,在副热带地区形成副热带西风急流,同时所谓的&极地西风激流&向赤道靠拢、减弱,最后消失,这时在整个半球形成了靠赤道的直接环流和靠极地一侧的间接环流,两圈环流形成的过程仅仅需要9个小时左右。

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