ebb current 中文意思是什麼
ebb current
解釋
落潮流-
The results show that in the case of no wind the oil film moves southwestward along with the tidal current, its area increases and thickness decreases, and the port is not polluted during ebb tide ; a part of the oil film is blocked by the northern jetty, and stays in the port during flood tide
計算結果表明，在靜風情況下，落潮期間油膜隨落潮流向西南方向漂移，面積擴大，厚度減小，港區未受油污的影響；漲潮期間油膜受北導堤的阻擋，部分油污留在港區。 -
In the second place, the ebb was now making - a strong rippling current running westward through the basin, and then south ard and seaward down the straits by which we had entered in the morning
其次，現在正值退潮一道泛著細浪的湍流經過海灣向西流去，然後再穿過我們早晨通過的那個海峽，向南匯入大海。 -
Ebb - current flow structure
落潮流構造 -
The oil film trajectory oscillates back and forth with the ebb and flood current, and its thickness decreases and area increases during the drift process with oscillation due to the diffusion
油膜軌跡隨落潮流和漲潮流來回振蕩，因擴散作用，在往復漂移過程中厚度變小，面積增大。 -
Our enterprises took the opportunity, when our economy was at its lowest ebb, to upgrade their efficiency and rationalise their businesses. that has greatly strengthened the resilience of our economy, and laid a solid foundation for the current upturn
在經濟低潮時，我們的企業積極提升效率，重整業務，大大加強了香港經濟的韌力，為今次經濟復甦奠定穩固的基礎。 -
Influenced by flood dominated current in the flood channels, the characteristics of surface sediments, such as grain size, light and heavy minerals, micro - paleontology and magnetism in the flood channel are very different from those in the ebb channels, this kind differences is the response for complex hydrodynamic in estuary
河口漲潮槽在漲潮優勢流作用下，槽內表層沉積物的粒度、輕重礦物、微體古生物和磁學等特徵不同於落潮槽相應的沉積特徵，體現了沉積物的分佈對河口復雜水動力的響應。 -
Make a comprehensive view of all study results about the flood channel, a model of formation and evolution of the flood channels was proposed. according to this model, not all flood channels formed by ebb channels divided by sand spit develop toward death, some of them may be keeping the current situation or transform to the reserve channel with the change of runoff and sediment concentration from upper reach
用gis方法計算1861 - 2002年新橋水道區域的沖淤變化，可定量表達漲潮槽在不同時間尺度形成演化規律，結合漲潮槽巖芯沉積物垂向的沉積特性變化，可闡明漲潮槽的形成機理與演化過程，並提出不同種類型漲潮槽的形成演化模式。 -
Analyses of the velocity data at no. 14 station of chengjiawu channel for two tidal periods show that the ebb current is strong and that the flood current is weak
摘要陳家塢槽14號站位連續兩個潮次的流速資料表明，該站位的潮流特點為落強漲弱。
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