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1)  West Pacific tropical cyclone
西太平洋热带气旋
1.
Among these the West Pacific tropical cyclone is faster, 3.
3纬度/日,其中西太平洋热带气旋较快,达 3。
2)  tropical cyclone over WNP
西北太平洋热带气旋
3)  northwest pacific tropical cyclone retrieval system
西北太平洋热带气旋检索系统
4)  Western Tropical Pacific Ocean
热带西太平洋
1.
In this paper, the deep casting CTD data collected around the 1986/1987 ENSO event in the western tropical Pacific Ocean(141 165 E,140 100 W)are used to calculate the spatial and temporal variabilities in potential energy relative to different isobaric surfaces in the sea area.
利用1986/1987ENSO事件前后的深水CTD资料,计算了热带西太平洋(141°~165°E,10°N~10°S)相对于不同等压面的势能空间分布和时间变化。
2.
Based on the observed data during 1986-1990,the longitudinal variabilities and vertical distributions of buoyancy frequency in the western tropical Pacific Ocean are analyzed to expound the relation of buoyancy frequency to seawater stability and potential energy of oceanic internal wave.
根据实测资料(1986-1990年),分析了热带西太平洋(165°E,10°N~10°S)浮力频率的垂直分布和经向变化,讨论了浮力频率与海水稳定度和海洋内波位能的关系。
3.
Interannual variability of sea level in the western tropical Pacific Ocean are discussed in this paper,on the basis of the monthly mean sea level during the period of 1975 -1988 provided by TOGA SEA LEVEL CENTER.
根据美国TOGA水位中心所提供的1975—1988年水位月平均资料,分析、讨论了热带西太平洋水位的年际变化特征,特别是与ENSO事件有关的低水位现象。
5)  western tropical Pacific
热带西太平洋
1.
Decadal variations of the subsurface and intermediate waters in the western tropical Pacific derived from Argo and historic data;
基于Argo浮标和历史资料的热带西太平洋次表层与中层水年代变化分析
2.
Simulation of undercurrents in Western Tropical Pacific:(I)Model configuration and validity of results
热带西太平洋潜流模拟:(Ⅰ)模式配置与模拟结果验证
3.
The analyses of the sounding data of the atmosphere obtained from Sino-American joint air-sea interaction studies in the western tropical Pacific revealed that inversion layers occur within the lower atmospheric layer over the western tropical Pacific warm pool area where vertical convection of air prevails.
通过对“中美热带西太平洋海-气联合考察”获得的大气温度探测资料分析,揭示了大气垂直对流旺盛的热带西太平洋暖水区低层大气普遍有逆温层存在的事实,并指出这些逆温层与信风逆温层和季风逆温层的显著区别是逆温层大多很弱、很薄,而且往往有多个逆温层同时存在。
6)  the tropical western SST
热带西太平洋SST
补充资料:太平洋地区标准会议标准(见太平洋地区标准会议)


太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC

Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
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