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The westerly has blowd every night,from the Mountain Valley Zhenyuan to Sand River,pine recite bamboo rhyme,valley song mountain cry,at the old time strange westerly is called "nine wells westerly".

西风每夜从此起,自山谷真源至沙河、松吟竹韵、谷应山鸣,古时候把这股奇怪的西风称为《九井西风》。

The circulation features in the westerlies, especially, distribution and variation of the upper–level westerlies play an important role in controlling the different tracks.

西风环流,尤其是中、高纬度高层西风的分布及其变化对于形成不同类型的台风路径亦起了很重要的作用。

The above variation trend suggests that effect of the westerly is increasing.

变化趋势表明西风的作用在加强。

In the Little Ice Age, correspond to the prevalence of the westerly but it is not synchronous.

的小冰期同位素偏负和纹层厚度增加对应西风的强盛,但存在一定的相位差。

The difference may be associated with the variability of zonal wind in the middle and high latitudes.

这种差异可能跟中高纬度纬向西风的自身变化有关。

In the lower level of the troposphere, the center of the cross-equatorial flows is located at 925hPa other than 850hPa while it is at 150hPa instead of 200hPa in the upper level. The CEFs in the Eastern Hemisphere show monsoonal features while they are characterized by the trade wind in the Western Hemisphere.

低层的索马里和南海越赤道气流对南海夏季风的爆发有至关重要的作用,在南海夏季风爆发前2候,索马里急流有一次迅速的增强,这一增强有利于加速孟加拉湾地区西风的向东扩展,并使控制在南海的西太平洋副高东撤;同时,南海越赤道气流的迅速增强也加速副高的北上,共同促使南海夏季风全面爆发。

However, the direction of the new Westerlies, and the location of land masses and known volcanic regions, and thus the direction of the heaviest ash fall, can be easily gauged.

然而,新出现的西风的方向和陆地的位置,以及已知的火山区,还有火山灰降落最重的区域是可以很容易地计算出来的。

On the contrary, the opposite pattern occurs when the AACEF is stronger.(3) On interannual timescale, the changes in the SH Ferrel cell lead to the anti-phase variation of the subtropical high and the circumpolar low, i. e., the Antarctic oscillation .

研究发现,当夏季南极涛动偏强时,南极极涡和高纬度的西风急流强度都偏强,但中低纬度西风急流的强度偏弱;反之,当南极涛动偏弱时,南极极涡和高纬度西风急流强度将偏弱,中低纬度西风急流强度将偏强。

Yesterday evening I saw a boat going up the river at full sail, driven by the west wind.

昨天黄昏时分,我看见一艘满帆的船,在西风的吹送下逆流而上。

The further composite analysis suggests that in the positive first mode SST anomalies years, the main body of the Aleutian low in winter season shifts southwestwards, then, the positive atmospheric temperature anomalies at the lower level and negative westerly wind anomalies at the upper level occur in northeast Asia to the west coast of North American.

进一步的合成分析表明,在第1种耦合型SST正异常年里,冬季阿留申低压主体位置偏西南,从东北亚到北美西海岸的西北-东南向带状区域内是低层大气温度正异常区和高层西风负异常区,西风负异常中心位于西风急流出口处的北太平洋中东部,而西风急流主体区的风速变化很小。

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