1) Western North Pacific subtropical area
副热带西部海域
2) subtropical sea area
副热带海域
1.
The hydrological data observed by the R/V Ryofu Maru of JMA along 155°E Section in the summers of 1972～1979 and 1989～1990, was used to study the ocean circulation and hydrological characteristics in the northern Pacific subtropical sea area.
根据日本气象厅RyofuMaru调查船于 1 972～ 1 977和 1 989～ 1 990年间夏季在 1 55°E断面观测的水文资料 ,分析了该断面上北太平洋副热带海域 ( 1 8°～ 30°N)的主要水文要素———温度、盐度、密度、溶解氧含量和地转流等的分布特征及其与ENSO现象之间的关系。
3) subtropical circle ocean area
副热带环流海域
1.
The sensible and latent heat fluxes over the subtropical circle ocean area (17***-26***N, 120***-130***E,) are calculated and analyzed by using the conventional meteorological data obtained during the China - Japan Joint Investigation on Subtropical Circulation System from 1995 to 1997.
利用“中日副热带环流合作调查”期间四个航次(1995-1997年)获得的常规气象资料和海表水温资料,计算了副热带环流海域(17°-26°N,120°-130°E)不同季节的感热通量和潜热通量。
4) tropical/subtropical cell
热带/副热带区域
5) SST in subtropical ocean
副热带海洋海温
6) 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。
补充资料：热带
1.赤道两侧南回归线和北回归线之间的地带称"热带"，也叫"回归带"。
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