Making use of the energy dissipation function of the step , the measure which takes step as curve jet flow is proposed 四川大学硕士学位论文利用阶梯的消能作用，提出把阶梯作为弯道急流的一种控制措施。
On a 200 - hpa map , regions with wind speed exceeding 150 km per hour are highlighted with colours to mark the location of jet stream 在200百帕斯卡的高空急流图中，风速大于每小时150公里的区域会涂上不同的颜色，以清楚标示高空急流的位置。
The black thick lines with wind barbs indicate the location of jet streams and their maximum speeds , while the dash lines outline possible cat areas 图中有风羽的黑色粗线显示高空急流的位置及最大风速，而虚线则描绘出有可能出现晴空湍流的区域。
But when the baroclinicity of low level vortex was strengthened and when warm air came into being , all the rain belts lay in the left and the front of southeast low level jet 当低涡的斜压性加大，出现暖空气的作用时，暴雨区均出现于西南风急流的左前方。
Results show that there are two activity centers of llsw in southwest of china locating in south china and northeast china respectively which are also the a ctivity c enters o f llj 结果表明：中国有两个西南低层大风活动中心，它们也是低空急流的活动中心，分别位于华南地区和东北地区。
So they will fear the name of the lord from the west and his glory from the rising of the sun , for he will come like a rushing stream which the wind of the lord drives 赛59 : 19如此、人从日落之处、必敬畏耶和华的名从日出之地、也必敬畏他的荣耀因为仇敌好像急流的河水冲来、是耶和华之气所驱逐的。
Further more , the sst warming twice in one year in the northern indian ocean , the mixed layer deepening in the central arabian sea during summer , as well as the equator jet occurred only in transient seasons are all noteworthy 不仅如此，北印度洋sst在一年有两次增暖、夏季风期间阿拉伯海中部混合层的加深，以及季风转换其间赤道急流的存在等也是季节变化尺度上引人注目的现象。
Carved from work , days of independence blue jade carvings into a cliff of humans , the foliage is more lifelike sculpture , river rapids and the boat downstream , the figure depicts the age lifelike , a relaxed mood on the heart 作品精雕而成,天蓝色的独玉巧雕成一株崖上的青松，枝叶的雕刻更显得逼真，江中急流的小舟顺水而下,岁人物的刻画栩栩如生,一种意境悠然上心头.充满了生机勃勃的景象。
The results show that unbalance force of atmospheric motion and the coupling reaction among convective cloud cluster and moisture frontal zone and low level jet lead to the continuation of strong convergence in low layer and the maintenance of torrential rain 分析结果发现，大气运动非平衡强迫、凝结降水的非均匀分布与强烈垂直风切变的耦合作用、 “湿度锋”与低空急流的耦合相互作用通过促进低空辐合流的维持，导致了对流云团和暴雨天气的持续。
