In this paper,decadal variability of global mean sea level is analyzed over one century using the datasets of global ocean tide measurement data from permanent service for mean sea level(PSMSL).
对全球潮汐测量资料的长期变化趋势分析后,得出在过去一个世纪里全球海平面呈现一个整体上升的趋势,在北大西洋和太平洋西部,海平面出现了近40 mm/a的上升量。
coast and geodetic tide station
海岸与大地潮汐测量站
OBSERVATIONS AND RESULTS OF TIDAL GRAVITY PARAMETERS OF LANZHOU (1959-1989)
兰州地区(1959—1989)重力潮汐参数的测量与结果
Analysis of tidal control of super-large shipping route measurement in Bohai Sea
渤海超大型船舶航路测量潮汐控制分析研究
EVALUATION OF DATA QUALITY AND REFLECTING EARTHQUAKE ABILITY OF TILT TIDE DEFORMATION OBSERVATION AT MACHENG SEISMOSTATION
麻城台倾斜潮汐形变观测资料质量与映震效能评定
STUDY OF TIDAL GRAVITY OBSERVATIONS OBTAINED AT STATIONS ZHONGSHAN AND CHANGCHENG, ANTARCTIC
南极中山和长城站重力潮汐观测研究
THE TIDAL EFFECT ON THE OBSERVATION WITH ASTROLABE AT SHANGHAI
上海天文台等高仪观测中的潮汐效应
Study on flow and sediment fluxes for tide-influenced lakes
受潮汐影响的镇江内湖水沙通量研究
A surveyor's mark made on a stationary object of previously determined position and elevation and used as a reference point in tidal observations and surveys.
水准点在事先确定了位置和高度的固定物体上的测量标记，用作潮汐观察与测量的参照点
Loading Effects of the Ocean Tides on the Tidal Gravity Observations at Zhongshan Station in the Antarctic
南极中山站重力潮汐观测的海潮负荷效应
Measurement and Control System of Hydraulic Tidal Model for Lang The Sluice, Viet Nam
越南良地水闸水工潮汐模型的测控系统
THE TIDAL EFFECT ON THE TIME AND LATITUDE OBSERVATION OF SHANGHAI OBSERVATORY
上海天文台天文时纬观测中的潮汐影响
Study on Tidal Model Derived from Satellite Altimetry Data;
由卫星测高资料确定海洋潮汐模型的研究
Method of Earthquake Monitoring by Nontidal Variation of Gravity Direction
利用重力方向的非潮汐变化监测地震的方法
ANALYSIS ON TIDAL PARAMETERS AND STABILITY OF DIGITAL DEFORMATION OBSERVATION IN XINJIANG
新疆数字化形变观测的潮汐参数及稳定性分析
Study on Ecology of Denitrobactcria in Jiulong River Estuary
九龙江口反硝化菌群数量的潮汐、季节、昼夜变化
or or relating to or caused by tides.
属于潮汐，关于或由潮汐引起。
A channel in which a tidal current runs.
潮汐水道潮汐流在其中流动的水道
In contrast to the simple observations of the tides, tidal current studies are difficult and expensive.
与潮汐的简单观测不大相同，潮流研究的难度既大、费用也巨。