1) Seawater density
海水密度
1.
The calculation method of seawater density by the multi-angle and polarized information was advanced here.
提出一种利用多角度偏振信息计算海水密度的方法,从多角度遥感与偏振光遥感的角度,找出海水的偏振特性与海水密度之间的函数关系,利用海水偏振特性与海水折射率特性对海水密度进行计算,扩展现有遥感应用的领域,同时为海洋基本参数反演开拓新思路。
2.
Using TOPEX/ Poseidon satellite altimeter data, and seawater temperature and salinity estimated from WOA98 model, we calculated sea level height variation caused by seawater density change in multi layers.
基于TOPEX/Poseidon卫星测高资料,采用WOA98海水温度及盐度模型,计算了多层海水密度变化引起的海面高变化。
2) sea water density
海水密度
1.
Striving to get the maximum cargo carrying capacity and to acquire great economic benefit by use of variations of sea water density in harbours is worth considering by captains and ship operators under the circumstances of sailing safely through shallow waters.
我国沿海河口港较多，利用港区的海水密度变化，在保证船舶安全通过浅水区的前提下，争取最大载货量，提高经济效益，值得引起广大船长和驾驶人员重视。
2.
The existent difference between geodetic leveling and tide station is investigated, and this difference comes from the sea level slope, and the sea level slope mechanism caused by ocean current, air pressure and breaking wave is analyzed, the geoid disturbance computed by three dimensional distribution of sea water density is prese.
进一步讨论了大地水准的测量精度 ,指出了大地 (几何 )水准与沿海验潮资料的不符是由于海面的倾斜 ;分析了海面倾斜的机理 ,其中包括海流、海水密度分布、气压、台风引起的破碎波等的作用 ;提出了用海水异常密度的三维分布计算大地水准面的扰动 ,实质上它反映了海面的倾斜 ,该量占大地水准测量结果的 73% ,这进一步说明密度的异常乃是我国沿海海面倾斜的主要原
3) water density
海水相对密度
1.
6, the optimum water density is 1.
6,海水相对密度的适宜范围为1。
4) layer of sharp density gradient
海水密度骤变层
5) salt water density correction
海水密度校正
6) seawater densitometer
海水光密度计
补充资料：海水增养殖(见海水养殖、海水增殖)
海水增养殖(见海水养殖、海水增殖)
marine aquaculture
_一一’‘~’‘以，’日y以.1日乙川髦增养殖(~ne aquacultu祀’见海水养殖·海水
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条