摘要
温度、盐度观测资料的误差分析结果表明:浅海区温、盐的观测误差冬季较小,分别约为0.4℃和0.2;夏季较大,在跃层附近层次由定深偏差所引起的温、盐观测误差分量分别可达1.32℃和0.11.温、盐的资料误差更大,夏季跃层处温、盐的日替代资料误差分别可达2.62℃和0.17.作者还就造成观测误差、资料误差的原因作了分析,对合理使用历史调查资料提出意见.
The errors on the observational data of temperature (T) and salinity (S) in the shallow seas are analyzed. The results show that: the TS observational errors are smaller in winter with the values of about 0.4℃ and 0.2 respectively, but greater in summer, and especially in the thermocline layers, where the TS observational error components caused by depth deviation can reach 1.32℃ and 0.11, respectively. The TS data errors are much greater, e.g. in the summertime thermocline layers, where the TS daily substituting data errors can come up to 2.62℃ and 0.17, respectively. The reasons for the observational error and data error have also been analysed,and the suggestions for using such data have been proposed.
出处
《厦门大学学报(自然科学版)》
CAS
CSCD
北大核心
1997年第1期100-105,共6页
Journal of Xiamen University:Natural Science
关键词
海洋
误差
温度
盐度
观测资料
浅海
Error, Temperature, Salinity, Observational data, Shallow seas