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- East Asia subtropical westerly jet 东亚副热带西风急流
- East Asian Subtropical Westerly Jet (EAWJ) 东亚副热带西风急流
- East Asian subtropical westerly jet 东亚副热带西风急流
- Summertime atmospheric circulation in Subtropical westerly jet 副热带西风急流
- The Characteristics of the Coupling Variation Between the Subtropical Westerly Jet and the Surface Heating Fields over East Asia 东亚副热带西风急流与地表加热场的耦合变化特征
- Impact of the Position Abnormalities of East Asian Subtropical Westerly Jet on Summer Precipitation in Middle-Lower Reaches of Yangtze River 东亚副热带西风急流位置异常对长江中下游夏季降水的影响
- subtropical westerlies jet in winter 冬季副热带西风急流
- subtropical westerly jet 副热带西风急流
- The late northward-shift of upper westerly jet and the subtropical high is the main reason for the late onset of Meiyu in 2005. 东亚副热带高空西风急流和西太平洋副热带高压向北突跳偏晚是江淮流域2005年入梅偏晚的主要原因。
- The results show that the late northward-jumping of the subtropical high is caused by the exceptional deep trough of East Asia, the East Asian subtropical upper westerly jet and the weak ITCZ. 结果表明，入梅前，东亚大槽发展强盛，ITCZ偏弱以及东亚副热带高空西风急流强劲少动导致西太平洋副热带高压北抬偏晚。
- Subtropical upper-tropospheric westerly jet 对流层上层西风急流
- In addition, cyclone activities have good relations with tropospheric baroclinity, westerly jet, and sea surface temperature (SST) gradient. 研究还表明，气旋活动的变化与对流层斜压性、急流以及北大西洋涛动、海温梯度等因素有关。
- The evolution and enhancement of occluded frontal circulation in upper-level westerly jet and lower-level southerly jet are discussed by using a dry primitive equation model. 利用原始方程模式探讨了高空西风急流和低空南风急流中锢囚锋环流的演变和增强机制。
- The results show that there is a good consistency between the low -frequency variations of the westerly jet (and its relevant front zone) over the Northern China and Australian summer monsoon. 结果表明,我国北部上空的西风急流(及相应的锋区)与澳大利亚的夏季风的低频变化有很好的一致性。
- In middle latitudes the high value of PKE locates in the core area of westerly jet or its downstream area, while the low value of PKE lies in the upstream area of the westerly jet. 在中纬度,PKE的高值区位于西风急流中心或其下游,而PKE的低值区则位于急流中心的上游。
- The strong westerly jet in the upper troposphere is linked to the Mongolia cyclone and frontogenesis at low level which can cause strong wind and further provides the dynamic factor for the increased DWF in Beijing. 春季对流层高层的东亚西风急流增强能使低空的蒙古气旋加强和锋生;从而引起地面大风;为沙尘天气频次的增加提供动力条件.
- Relationships Between Perturbation Kinetic Energy Anomaly Along East Asian Westerly Jet and Subtropical High in Summer 夏季东亚西风急流扰动异常与副热带高压关系研究
- The flier is flying a new-type jet plane on trial. 飞行员正在驾驶一架新式喷气机作试验飞行。
- The signpost points in a westerly direction. 路标指向西。
- Location and intensity changes of the westerly jet 急流中心位置和强度变化
