1) Subtropical Countercurrent
副热带逆流
1.
Based on the analysis of Sea Surface Height Anomaly(SSHA) from satellite observation,it is proved that the oscillation with period of 70～210 days is dominating in two branches of the eastward countercurrent in Subtropical North Pacific: Subtropical Countercurrent(STCC) and Hawaiian Lee Countercurrent(HLCC).
根据对卫星观测的海平面高度资料的分析,进一步证实了在北太平洋副热带两支向东的流(副热带逆流和夏威夷背风逆流)所在的区域内,海平面高度的70-210天周期振荡是主要的低频变化。
2.
Meso-scale eddies in the region of Subtropical Countercurrent (STCC) in the Northwest-Pacific are active and they are important ocean processes in such area.
中尺度涡在西北太平洋副热带逆流区活动频繁,是该海区的重要海洋过程。
3) subtropical circulation
副热带环流
1.
In addition,it is found that the center of the subtropical circulation will be located on the north of heating area when there is the meridional and vertical shear of the basic flow.
说明即使在线性模式中,洋面副高的形成也不能完全用季风潜热加热来解释;另外,静力稳定度对热强迫的副热带环流的影响也很重要,使热源的强迫作用放大。
4) subtropical cell
副热带经圈环流
1.
The Pacific subtropical cell involves the subtropical subduction and equatorial upwelling.
太平洋副热带经圈环流是太平洋热带和副热带上层海洋进行热交换的桥梁,其变化可以影响太平洋热带和副热带之间的热结构,从而影响全球气候。
5) subtropical westerly jet
副热带西风急流
1.
Sensitive experiments were performed by using a regional climate model with p-σ incorporated coordinate to investigate the impacts of the uplift of the Tibetan Plateau on the East Asian subtropical westerly jet(EAWJ).
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。
2.
They are (1) preparation stage of Subtropical westerly jet (from May to September); (2) Development stage of jet from October to March; (3) the jet disappearing and replacing by west pacific subtropical high from May to September.
我国夏季主雨带的形成 ,是从上一年夏季开始的 ,共经历 3个阶段 :①上一年 5～ 9月副热带西风急流的孕育期 ;② 10～ 3月西风急流发展期 ;③西风急流为西太平洋副热带高压替代期 (本年 5～ 9月 )———主雨带形成。
6) high sky strong wind
高空副热带急流
1.
The result enunciation:In spring high sky strong wind is result in southeast region in Yunnan of one of the important factors of the unsteady la yer knot of atmosphere, the weather system tr.
结果表明,春季高空副热带急流是造成滇东南地区大气不稳定层结的重要因子之一,天气系统触发不稳定大气层结产生强冰雹云,副热带急流具有加强、维持发展的作用。
补充资料：副热带
亚热带。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条