1) Changjiang diluted water
长江冲淡水
1.
Numerical model simulation of expansion of Changjiang diluted water in summer;
夏季长江冲淡水扩展的数值模拟
2.
Analysis on the path of transportation and diffusion of Changjiang diluted water;
长江冲淡水输运和扩散途径的分析
3.
The main axis of the Changjiang diluted water expands towards the northeast-north after it leaves the mouth (the river discharge in August 2000 is smaller than the long-term average).
采用CTD、多参数环境监测系统 YSI等仪器设备 ,于 2 0 0 0年 8月在长江口外海区对长江冲淡水结构、羽状锋等进行了现场观测。
2) Changjiang River diluted water
长江冲淡水
1.
Based on the remote sensing data of "NOAA-14"in summer 1997 and 1998, It is found that the spreading direction of the Changjiang River diluted water changed in 7~10 days, and pointed out, that it is unreliable for using the traditional oceanographic observation data to explain the mechanism of the spreading direction change of the Changjiang River diluted water.
以 1 997年和 1 998年两个夏季的 6幅“NOAA- 1 4”卫星遥感图像为据 ,反映了长江冲淡水扩展方向的周、旬时段变化。
2.
The monthly salinity and wind data in summers of 1959, 1975～1982 and 1998 were used to analyse and discuss the spreading paths of the Changjiang River diluted water.
利用 1 95 9,1 975 - 1 982年及 1 998年夏季各月黄、东海盐度分布和相应风场资料 ,分析讨论了长江冲淡水夏季的扩展路径。
3) Zhujiang River diluted water
珠江冲淡水
1.
Analysis of Diffuse Route of the Zhujiang River Diluted Water;
珠江冲淡水扩散路径分析
4) Hanjiang River plume
韩江冲淡水
1.
In summer, the major water bodies that influence the area are the Hanjiang River plume, t.
夏季影响本海区的水系主要有韩江冲淡水、上升流、南海水、和黑潮水等。
6) ash sluicing with freshwater
淡水冲灰
补充资料：长江三峡(见长江)
长江三峡(见长江)
Changjiang Sanxia
Changiiang Sanxia长江三峡(Chan幻iang sanxia)见长江。
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