摘要
“海洋四号”在执行DY95-7和DY95-9航次调查任务期间,在东太平洋我国开辟区做了2个测站的底层海流观测。观测资料分析表明,底层流的流速在1.2~12.0cm/s之间;底层流有月际和日际变化,并发现底层流存在“不活动”期。
Mooring observation of bottom sea current was done at the 2 stations in the China pioneer area of East Pacific Ocean during “Haiyang 4”cruises DY95 7 and DY95 9.This report presents the analyzed and studied results of mooring observation of deep sea bottom current.Data analyses show that:the current velocity is 1 2~12 0 cm/s,among which,velocity 200 m from the seafloor is generally 1 3~12 0 cm/s,and 8 m from the seafloor generally between 1 2 and 10 0 cm/s.Bottom current not only has changes in months,days and low frequency period of 20~30 days,but also has an“unactive”period.In the layer 200 m from the seafloor,the“unactive”period of the current is taking 1 day as the shortest and 6 days as the longest;8 m from the seafloor,the shortest is 1 day and the longest 8 days.The largest velocity occurs in August,and the smallest in July.And the velocity changes most frequently in April and October.Except January and November,all the months see a larger velocity 200 m from the seafloor than that 8 m from it.The direction of the bottom current is nearly opposite in January to that in June.
出处
《海洋地质与第四纪地质》
CAS
CSCD
北大核心
1999年第3期115-120,共6页
Marine Geology & Quaternary Geology
关键词
底层流
流速
流向
东太平洋
海底
锚泊观测
bottom current
current velocity
current direction
the Eastern Pacific Ocean