1)  high pressure
入海高压
1.
Through diagnostic analysis of the 10 ~ 11 scale south gale occurred in the north coast of Zhejiang Province on April 16~17 2003, we find that the high pressure moving to the sea preserved stable and the low pressure developing in the west are the direct reasons.
本文对 2003 年 4 月 16 ~ 17 日发生在浙北沿海的一次 10 ~ 11 级南大风过程进行了诊断分析: 发现入海高压的稳定维持和西面低值系统的发展是造成南大风的直接原因,北面冷空气的动力作用和西南急流引起热力降压作用,使地面增温、增湿、梯度堆积,并引起对流发展,使高空动量下传,有利于南大风的出现。
2)  sea estuary
入海河口
1.
According to data based on inspection research which was carried out from 2003 to 2005,in the area of sea estuary(ZhangJiang Estuary,DongXi Estuary) and the alongshore sea area(DongShan Bay,GongKou Bay),we have done a series of analysis and research on the impacts of the effluents from the coastline estuary to the water eutrophication of the alongshore sea area.
根据2003～2005年对福建省漳州市入海河口(漳江口、东溪口)和近岸海域(东山湾、宫口湾)的监测调查资料,分析研究了入海河口污染物输入对近岸海域水体富营养化的影响,结果表明:河流陆源的有机、氮、磷污染物入海通量越大,所对应的近岸海域海水水质越差,富营养化趋势越明显。
3)  flux
入海通量
1.
Behaviours and flux of bioavailable phosphorus in Jiulongjiang Estuary;
九龙江口生物可利用磷的行为与入海通量
4)  quantity into the sea
入海量
5)  seagoing rivers
入海河流
1.
The variation of runoff module and sediment transportation module in main seagoing rivers of China are analyzed according to the latest 60 years data published in the China Gazette of River Sedimentation by using tendency analysis method and based on the accumulated water-sediment relationship to investigate their historical evolution.
本文利用"中国河流泥沙公报"数据,结合各流域长系列年降水量资料,利用趋势分析和水沙双累计曲线方法相结合分析径流模数和输沙模数的变化,探讨我国主要入海河流水沙的历史变迁。
6)  coastal outfall
入海口
1.
A new type of energy dissipator for coastal outfall of a drainage project;
排水系统入海口新型消能工
参考词条
补充资料：高压线走廊（高压架空线路走廊）
在计算导线最大风偏和安全距离情况下，35kV及以上高压架空电力线路两边导线向外侧延伸一定距离所形成的两条平行线之间的专用通道。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。