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The japanese were busy absorbing western influences at the time , and this is reflected in the building s east - west architectural melange

由于当时的日本受西风影响甚大,因此这一座温泉浴场采东洋和西洋混合的建筑形式。

North of subtropical zone prevails midlatitude westerly wind, and its south easterly wind.

副热带的北侧为中纬度西风气流,南侧盛行热带东风气流,副热带高压是联结中低纬度天气和气候系统的纽带。

In summary, moisture variability in ACA and northern Tibetan Plateau has showed major difference from monsoon evolution on various timescales in the Holocene. It is thus proposed that there is a westerlydominated climate model in midlatitude Asia during the modern interglacial period.

据此我们提出,亚洲中部西风带控制区在现代间冰期从数千年到年代际的各个时间尺度上均存在不同于季风区的湿度变化模式,称之为现代间冰期气候变化的西风模式。

Before the occurrence of ENSO, due to the anticyclonic anomaly in midlatitude of the South Indian Ocean, the anticyclonic anomaly over Australia tends to be enhanced through the dispersion of Rossby wave; In the meantime, the equatorial convergence of the southerly anomaly off the east of Australia and the northerly anomaly in the Philippine excite the onsets of the westerly anomaly in the equatorial western Pacific and the occurrence of ENSO.

在ENSO发生前,南印度洋中纬度为反气旋异常,并通过Rossby波的频散作用加强了澳大利亚附近的反气旋异常;同时,澳大利亚东部沿海的南风异常与菲律宾附近的北风异常在赤道辐合,促进了赤道西太平洋西风异常的爆发和其后ENSO的发生。

The seasonal evolution, precipitation, convection, low-level west wind and SST all have a trend of spreading northeastward.

西北太平洋夏季风的季节演变,降水、对流、西风和海温都有向东向北扩展的趋势。

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。

A trough is traversing to the north of KUJIRA and it is expected that KUJIRA will be steered northeastward in the northwestern periphery of the subtropical ridge.

一道西风槽正於鲸鱼北面横过,预料鲸鱼将沿副热带高压脊的的西北部向东北移动。

At pentad 31 or 32 and after monsoon onsets, precipitation, convection, low-level west wind and SST extend northeastward, and at nearly pentad 41 they arrive at the most northeast zone quickly, and then their intensities decrease, but they still have a trend of extending eastward.

在31或32候(6月初)季风爆发后降水、对流、西风和海温开始向东向北扩展,在41候(7月下旬)左右时都迅速达到最北地区,之后强度减弱,但仍有向东扩展的趋势。

Affected by the enhanced weakness in the subtropical ridge brought by the passage of Tropical Cyclone Matmo and the active southwest monsoon, it moved northeastwards.

初时它受到被热带气旋麦德姆和西风槽扩大的副热带高压脊弱点及活跃西南季候风的影响,该热带低气压初时向东北移动。

The ridge east of SINLAKU is expected to extend westward to allow a short-term northwesterly track, after which it will be eroded by a passing mid-latitude trough to provide room for recurvature.

森垃克东面的副高将继续西伸并令森垃克向西北移动。预计一道西风槽将於 36 至 48 小时后到来,令该副高东退,所做成的空隙将会容许森垃克作出转向。

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The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

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