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。
英文短句/例句
1.Study of Mesoscale Eddies in the Subtropical Ocean of the Northwest-Pacific and Adjacent Area;西北太平洋副热带逆流区及其邻近海域中尺度涡研究
2.THE SPECTRA ANALYSES OF THE SUBTROPICAL GENERAL CIRCULATION AT 100 MB IN THE PLUM RAIN梅雨期间100毫巴副热带环流的谱分析
3.The seasonal,interannual and interdecadal variations of the intensity of different subtropical upper jet-stream centers副热带高空急流各中心强度时间变化及分析
4.calm zone of Capricorn南半球副热带无风带
5.calm zone of Cancer北半球副热带无风带
6.A Numerical Study of the Effect of Anomalous Surface Heating in the Kuroshio Current Region in Winter on the East Asian Subtropical Westerly Jet冬季黑潮暖流区加热异常对东亚副热带西风急流影响的数值研究
7.The subtropical monsoonal circulation is associated with the Southerlies from the subtropical South Asia and the northern upper Easterlies;副热带季风环流与源于南亚副热带地区的偏南风,北支高空东风相联系;
8.STRUCTURES OF A THERMAL CONVECTIVE PRECIPITATION SYSTEM HAPPENED IN CONTROLLING OF THE WESTERN SUBTROPICAL PACIFIC HIGH西太平洋副热带高压下热对流降水结构特征的个例分析
9.Relationship between Date of Abrupt Change of the East Asian Subtropical Westerly Jet and East Asian Circulation Anomaly in Early-Middle Summer初夏至盛夏东亚副热带西风急流突变早晚与东亚环流异常的关系
10.sub-tropical dry climate副热带冬季乾旱气候
11.THE INFLUENCE OF EDDY VISCOSITY ON THE SUBTROPICAL PLANETARY-SCALE CIRCULATION IN SUMMER涡旋粘性对于夏季副热带准定常行星尺度环流的影响
12.THE RELATIONSHIP BETWEEN GENERAL CIRCULATION OF THE SOUTHERN HEMISPHERE AND THE MEDIUM RANGE ACTIVITIES OF WEST PACIFIC SUBTROPICAL HIGH AND TYPHOON GROUP南半球环流与西太平洋副热带高压和台风群中期活动的关系
13.The Analysis of the Variations of the East Asian Subtropical Westerly Jet from Early Summer to Midsummer and Its Anomalies初夏至盛夏东亚副热带西风急流变化及其异常分析
14.Relationship between the East Asia Subtropical Westerly Jet Anomaly and Summer Precipitation over Eastern China中国东部夏季降水与同期东亚副热带急流年代际异常的关系
15.Stationary Response of the Subtropical Circulation to Latent Heating in a Linear Quasigeostrophic Model.Ⅰ:Basic Quality and Characteristic Analysis线性准地转模型中副热带环流对潜热加热的定常响应 Ⅰ.基本性质及特征分析
16.Location Variation of the East Asia Subtropical Westerly Jet and Its Effect on the Summer Precipitation Anomaly over Eastern China东亚副热带西风急流位置变化及其对中国东部夏季降水异常分布的影响
17.Features of the East Asian Tropical and Subtropical Summer Monsoons and Their Relations to the Thermal Forcing;东亚热带—副热带季风活动特征及其与热力强迫的关系
18.Relationship of Land-Sea Thermodynamic Anomaly and East Asian Summer Subtropic Monsoon;海陆热状况异常与东亚夏季副热带季风的关联
相关短句/例句
Subtropical jet副热带急流
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。
延伸阅读
副热带亚热带。
