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There is a weakness between the subtropical ridge anchored east of the date line and the ridge in the NW Pacific, and LINGLING will traverse the weakness to give a standard recurving pattern.

预料玲玲将会通过在换日线以东的一个副热带高压脊与西北太平洋高压脊间的弱点,从而向北至东北方向移动。

The forecast after t+36 calls for a recurving scenario supported by most numerical models along the western periphery of the ridge.

其后,随著副热带高压脊的东退,米娜将沿它的西部转向北至东北移动。

It is forecast that FAXAI will turn to the northeast soon due to the effect of the westerlies.

预料受西风带的影响,法茜将加速转向东北,沿副热带高压脊西北边移动。

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。

And the westward ISO is usually the low-frequency low and high pressure systems from the Bay of Alaska in northeastern Pacific and the Okhotsk in the northwestern Pacific of mid high latitudes, and the ISO evolving in subtropical easterlies.

进一步分析发现,经向风ISO的纬向传播对应着大气经向型环流系统的移动,向西传影响东亚夏季风区降水的ISO有来自低纬中东太平洋东风流中的低频气旋(如副热带东风带中ISO的演变);也有来自中高纬度阿拉斯加湾及鄂霍次克海一带低频低压和高压(如阻塞高压和东北太平洋高压)的向南向西频散。

The results show that for the global scale characteristics of the vertically integrated vapor flux fields, which is described in terms of the rotational and divergent components of the stationary parts of the vapor field, both GOALS and FGCM--0 can reproduce the subtropical gyres in each hemisphere, the eastward water va- por transport of the mid--latitude westerlies, and the westward vapor transport of equatorial easterlies reasonably, though the precise positions of the gyres simulated by GOALS, and the intensities of the gyre centers in FGCM--0 do not match the observations accurately.

结果表明:(1)对垂直积分的水汽通量场的流函数及其对应的无辐散水汽通量矢量的模拟,三个耦合模式都能够较为合理地再现副热带大洋的涡旋结构、中纬度西风带的东向水汽输送、赤道东风带的西向水汽输送和东亚夏季风水汽输送等行星尺度特征及其季节变化,只是GOALS的涡旋位置、FGCM-0的涡旋中心强度,较之实际略有偏差。

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。

Among these factors the effects of the Atlantic subtropical high on locusts occurrence are mainly caused by ground surface temperature that is affected by the Atlantic subtropical high in autumn and winter when the locusts live through and incubate; Therefore the occurrence, the development and the harmfulness of the locust as well as its amount of eggs and imagos are impacted.

其中大西洋副热带高压对我国东亚飞蝗发生的影响主要是由于影响了秋冬季节蝗卵孵化和越冬期间的地面温度,从而影响了蝗卵基数和蝗卵孵化为成虫的数量,进而影响着我国东亚飞蝗发生、发展、危害情况的变化。

A numerical simulation technique is adopted to draw the surface projection map and its isograms of the pH values in the precipitation over Jiangxi Province.

采用数字模拟技术,绘制了江西省降雨pH值曲面投影图及其等值线图,发现江西省在南昌-鹰潭-临川-吉安-赣州一线形成南北方向的&r&字形的严重酸雨带,并指出这条严重酸雨带的走向与信风环流圈和副热带高压带纬向环流一致。

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。

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