1) Circulation in the Tropical Western Pacific
热带西太平洋环流
1.
Dynamic Structure of Ocean Circulation in the Tropical Western Pacific Ocean and Its Simulation;
热带西太平洋环流动力结构分析与模拟
2) 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。
3) 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。
4) the tropical western SST
热带西太平洋SST
5) western tropical South Pacific
热带西南太平洋
1.
The western tropical South Pacific, where there is an evident decadal variability, is the key region of the ENSO decadal variability.
结果表明,热带西南太平洋不仅是年代际信号的显著区,同时也有可能是影响ENSO循环十年际变化的关键区。
6) tropical western Pacific
热带西太平洋
1.
Using monthly mean National Center for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis data for the period 1958-1996, based on a new circulation index in the tropical western Pacific region, this paper investigates extreme winter circulation conditions in the northwestern Pacific and their evolution.
利用月平均的NCEP/NCAR再分析资料(1958-1996),基于一个新的冬季热带西太平区域环流指数,研究了冬季热带西太平洋环流的极端异常及其随时间的演变。
2.
In order to study the effects of SST anomaly in tropical western Pacific during winter and spring on the early summer monsoon in East Asia, a set of numerical experiments is conducted using OSU AGCM.
用ＯＳＵ的两层大气环流模式进行了热带西太平洋冬春海温异常对东亚初夏（５月）季风环流影响的数值试验。
3.
1, an analysis is made on the atmosphere-ocean heat exchange over the Tropical Western Pacific.
根据执行ＴＯＧＡ／ＣＯＡＲＥ研究计划在热带西太平洋进行考察的结果，对调查海区海－气界面热量交换进行了分析。
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。
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