1) 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。
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 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) Western North Pacific subtropical area
副热带西部海域
5) 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。
6) subtropic gyre zone
副热带环流区
1.
A preliminary study on ecology of phytoplankton in the subtropic gyre zone during the spring of 1996;
1996年春季副热带环流区浮游植物生态的初步研究
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