大亚湾海水温度的时空分布  

Temporal and spacial distribution of water temperature in Daya Bay

作　　者：曾刚[1] 许金殿[1] 张炳楷[1] 

机构地区：[1]国家海洋局第三海洋研究所,厦门361005

出　　处：《台湾海峡》1991年第2期110-116,共7页Journal of Oceanography In Taiwan Strait

摘　　要：本文根据1987年1～12月逐月的水文实测资料,利用统计方法,详细地分析了大亚湾海水温度的时空分布和年、日变化特征以及影响水温变化的主要因子,文内还指出了本海域常见的两种不同类型的水温日变化的特征。In this paper, we use statistical method to analyse the distribution and variation of water temperature in Daya Bay China.It is pointed out that seasonal variation of water temperature in this region is quite significant. The minimum temperature in winter is lower than 16℃, and the summer maximum is higher than 31℃. It is suggested that the increase of solar radiation and the influence of the South China Sea warm water are the main factors for the seasonal rising of water temperature,and the decrease of solar radiation and the influence of the northeast cold air flow are the main factors for seasonal temperature falling. Two different types of daily temperature variation feature are discussed.

关 键 词：海水 温度 时空分布 大亚湾海 

分 类 号：P731.11[天文地球—海洋科学]