潮汐區域 的英文怎麼說

中文拼音 [cháo]
潮汐區域 英文
tidal region
  • : Ⅰ名詞1 (潮汐; 潮水) tide 2 (比喻大規模的社會變動或運動發展的起伏形勢) (social) upsurge; cur...
  • : 名詞(夜間的潮) tide during the night; nighttide
  • : 區名詞(姓氏) a surname
  • : 名詞(在一定疆界內的地方; 疆域) land within certain boundaries; territory; region
  • 潮汐 : morning and evening tides; tide潮汐電站 tidal power station
  1. A similar deposit at the mouth of a tidal inlet, caused by tidal currents

    三角洲海灣入口處三角形沉澱,由形成
  2. Study achievement appears as following aspects : ( 1 ) yellow river estuary gate river flow and tide flow mixed area is not keep standing deposition status, on special income water and sediment conditions, boundary conditions and oceanic power conditions, this area may on the scour status ; ( 2 ) observed from estuary sediment deposition distributing process : delta and sea offing area sediment deposition vary trend is similar, each part sediment deposition scale varies as wave shape ; ( 3 ) on estuary gate, affect the sediment deposition factors, primary factors are tide prop, the gate widens gradually, estuary gate have branches, brine induced flocculation. this paper study the estuary gate widen, estuary gate have branches to affect the river channel deposition in quantity ; ( 4 ) based on field measured data, for the first time, deduce the estuary sediment deposition and distributing regress formula which can estimate estuary different areas sediment deposition volume ; ( 5 ) this subject demonstrate the estuary delta coastline dynamic balance conception, build the relationship between the estuary income sediment with deposition land area, draw the following important conclusion : when estuary years - averaged income sediment keeps at 345 million tons, the delta coastline may on the dynamic balance status. ( 6 ) this subject firstly brings up estuary sediment optimized control conception, and has the primary study on the macroscopically optimized control conception method

    研究認為: ( 1 )黃河河口口門逕流潮汐區域並非持續保持淤積狀態,在特定的來水來沙、邊界條件和海洋動力條件下,該可以處于沖刷狀態; ( 2 )從河口泥沙沉積分配的過程來看:三角洲與濱海泥沙的沉積變化趨勢是基本一致的,各部位的泥沙沉積比例變化基本呈波動狀態,且三角洲與濱海泥沙的沉積比例與來沙量密切相關,基本成正比關系; ( 3 )在口門處,影響泥沙沉淤的因素主要集中在頂托、口門逐漸加寬、河口門分汊、鹽水造成絮凝等,本報告主要對口門加寬,口門西妥理工大學工程碩士專業學位論文分漢對河道淤積的影響進行了定量分析: (一扣根據實測資料首次建立了河贖流路泥沙沉積分配的回歸計算式,據此可以預估計算河口不同泥沙的沉淤量; 、 5 )本項研究首次論證了河口三角洲岸線動態平衡的概念,並建立了黃河河口來沙量與造陸面積的相關關系,得出了當河口多年平均來沙量維持在3 . 45億t時其河口三角洲岸線則可能處于動態平衡狀態的重要結論; 『 6 )本項研究首次提出了河口泥沙優化調控的概念,並對其宏觀優化調控模式進行了初步探討。
  3. Following the launch of topex / poseidon in 1992, there has been considerable improvement in the accuracy of the global tidal models

    Topex / poseidon的發射極大地促進了大洋模型研究的進展,但大洋模型在淺海精度比較差。
  4. This has been further complicated by undisinfected effluent discharged from stage 1 of the harbour area treatment scheme hats since late 2001. though the scheme has brought about general improvement in the harbour s water quality, particularly the eastern side, the discharge is released from a tunnelled outfall from the stonecutters island sewage treatment works, situated around eight kilometers from many of the beaches. tides and currents have resulted in the hats discharge affecting beach water quality in the tsuen wan district

    此外,凈化海港計劃第一期工程已於2001年底完成,該計劃雖能為海港整體水質帶來顯著的改善,特別是東面水,但昂船洲污水處理廠尚未設置消毒設備,而海底排污渠口則距離荃灣多個泳灘僅約8公里,處理后的污水往往隨和海流進入荃灣水,影響內泳灘水質。
  5. The quality factor is about 9543, which, compared with those determined based on the tidal gravity observations in the previous studies, more closes to those obtained by using the vlbi data. the complex resonance strength is ( - 6. 10x10 - 4, - 0. 01x10 - 4 )

    以武漢臺超導重力儀觀測資料為例,研究了海負荷對fcn共振參數擬合的影響和重力觀測中近周日共振的性特徵。
  6. Wetlands exist between water territory and land and always flooded by tides and inundation. normally we can divide them into coastal wetland and inland wetland. taijiang ecology belongs to coastal wetland that created by the ocean tides

    濕地存在於水與陸之間的交會地帶,經常或間歇的被、洪水淹沒的土地,一般可分為沿海濕地與內陸濕地。
  7. But, in some other water areas such as the narrow - deep tide channel, narrow - deep valley reservoir and narrow - deep estuary area, the vertical varies of parameters such as the velocity, temperature and concentration is far greater than that in the horizontal direction, so the two - dimension vertical numerical simulation technique should be adopted in these areas

    而在另外一些水,如窄深通道、窄深型河谷水庫如三峽、窄深河口地,有關參量(如流速、溫度、濃度等)的垂向變化要比水平橫向的變化為大,應採用垂向二維水流水質數值模擬技術。
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