台湾海峡1999年8月表层温盐的走航式观测  

Underway Measurement of Sea Surface Temperature and Salinity in the Taiwan Straits in August, 1999

作　　者：陈华[1] 胡建宇[1] 潘伟然[1] 曾淦宁[1] 陈照章[1] 贺志刚[1] 张彩云[1] 李虹 

机构地区：[1]厦门大学亚热带海洋研究所,海洋学系厦门361005 [2]福建海洋研究所,厦门361012

出　　处：《海洋通报》2001年第6期25-31,共7页Marine Science Bulletin

基　　金：福建省科技项目(98-Z-179);国家自然科学基金重点项目(编号:49636220)

摘　　要：利用1999年8月台湾海峡的调查资料中走航式温盐仪的资料,对该海区的表层温盐分布进行分析?分析结果表明:调查期间在该海区存在多处上升流和冲淡水?台湾海峡调查海区的上升流区大致可分为两类:(1)海峡西部沿岸上升流区:平潭上升流区?东山上升流区和南澳上升流区;(2)台湾浅滩附近的上升流区?冲淡水主要有九龙江冲淡水?珠江冲淡水和闽江冲淡水,此外还有粤东沿岸水?The distributional features of temperature and salinity in the Taiwan Straits have been analysed based on the data in August ,1999. The characteristics of temperature and salinity are summarized as follows: There are several upwellings and diluted water in the Taiwan Straits. The upwellings are divided into two kinds: those along the western coast of the Taiwan Straits and those around the Taiwan Shoal. There are three kinds of diluted water: diluted water of the Jiulong River, diluted water of the Zhujiang River and diluted water of the Minjiang River.

关 键 词：台湾海峡 上升流 冲淡水 表层温盐分布 1998年 

分 类 号：P731.1[天文地球—海洋科学]