摘要
青岛验潮站平均海面在过去60年中,一般呈现上升趋势,相对海面上升速率约为1.7毫米/年。相反,在1954—1984年间相对海面以1.5毫米/年的速率下降。本文探讨了相对海面变化的各种可能的原因。
Mean annual sea levels at the Tide-gauge Station of Qingdao exhibit a general rise of relative sea level at a rake of about 1.7mm/year during the past 60 years. In contrast, the relative sea level was sinking at a rate of about 1.5mm/year during the period of 1954—1984. The various possible causes of the above relative sea level change were investigated in this paper.
出处
《海洋科学进展》
CAS
CSCD
1989年第1期14-17,共4页
Advances in Marine Science
基金
国家自然科学基金