河口高潮 的英文怎麼說

中文拼音 [hékǒugāocháo]
河口高潮 英文
pororoca
  • 河 : 1 （天然的和人工的大水道） river 2 （指銀河系） the milky way system; the galaxy 3 （特指黃河） t...
  • 口 : Ⅰ名詞1 （人或動物進飲食的器官; 嘴） mouth 2 （容器通外面的地方） mouth; rim 3 （出入通過的地方） ...
  • 高 : Ⅰ形容詞1 （從下向上距離大; 離地面遠） tall; high 2 （在一般標準或平均程度之上; 等級在上的） above...
  • 潮 : 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...
  • 河口 : [地理學] river mouth; stream outlet; estuary; outfall河口地貌 estuarine geomorphy; 河口港 estuary...
  • 高潮 : 1 （最高潮位） high tide; high water; spring tide; flood 2 （事物高度發展的階段; 矛盾發展的頂點）...
  1. Based on 2m contour of surveyed bathymetry from 1976 to 1999 and mean - high - tidal line distracted from remote sensing images acquired by landsat - 5 tm from 1976 to 2000 respectively, quantitative analysis about alluvion and erosion as well as the relationship between accretion of modern yellow river delta and the water and sediment discharge of yellow river is made, and the results indicate the mean - high - tidal level is more effective than 2m contour of the bathymetry. it is found that the accretion of modem yellow river delta is becoming less and less, what ' s more, erosion is even more than alluvion in some recent years. diaokou promontory has been eroded seriously since yellow river changed its course in1976

    以一般高潮線反映現代黃河三角洲沖淤演變時，從1976年黃河改道清水溝流路入海到2000年，整個黃洞三角洲凈造陸201 . 5km ~ 2 ，淤積有逐漸變慢的趨勢，甚至出現凈蝕退的年份；刁口河嘴大量蝕退，蝕退速率開始快速，后來逐漸變慢；清水溝河嘴大量淤積，淤積速率開始迅速，后來逐漸變慢，甚至出現凈蝕退；清水溝河嘴南側到支脈溝一段岸線與刁口河嘴以西到灣灣溝一段岸線基本穩定。
  2. This plan was well designed in accordance with the geographic features of suzhou new district. this area receives the flood of the upper reaches from the grand canal, pased by the flood from the western hills and accepted the local rainstorm run off at the same time. 3

    3 . 《蘇州市長江防洪工程規劃》蘇州境內的長江位於長江河口段，同時受到洪峰、高潮和臺風的影響，尤以三者同時遭遇，危害最大。
  3. 1966 the world ? s first major tidal power station, at the rance estuary in the golfe de st malo in brittany, was opened by president de gaulle

    坐落在法國布列塔尼半島聖馬洛灣朗斯河口處的世界上第一座大型潮汐發電站建成，戴高樂總統出席竣工儀式。
  4. Generally, tidal bore is wave alignment moving upstream estuary, and its surface will break when the wave alignment is strong, which leads to water roll tracing the source. the velocity, which is between small - disturbed wave velocities before tidal bore happens and the one after tidal bore happens, increases with the ratio of tidal bore height to the water depth in wave front

    涌潮一般是向河口上游推進的波列，強度大時，表面破碎，進而發展成溯源推進的水滾，其傳播速度隨涌潮高度與波前水深比值增加，大小介於涌潮前後小擾動波波速之間。
  5. According to the result of physical modeling, the regression equation about the decrement of tidal bore height, the percentage of water - resisting area and the distance away from the upstream bridge site is constructed in this paper, the regression equation can be applied in the impact which bridge has on the tidal bore height in qiangtang esturary

    根據模型試驗結果，建立了涌潮高度的減小值與中潮位橋墩阻水面積百分比和上游離橋址距離的多元回歸方程，可供錢塘江河口建橋對涌潮高度的影響計算參考使用。
  6. Preliminary study on high water level of cao e river, a hilly, fluvial and macro - tidal estuary

    山溪性可沖性強潮河口曹娥江高水位初步研究
  7. In this section the evolution process of the coastline in the bayou area and diaokou bayou area was analysed through overlay analysis of gis. furthermore, the evolution rules and the enfluence factors were also analysed briefly

    在比較兩種基於遙感數據的海岸線提取方法可行性的基礎上，運用一般高潮線法提取海岸線，通過gis疊加分析深入剖析了黃河口地區、釣口河口地區海岸線的演變過程，並簡要分析了海岸線的演變規律及其影響因素。
  8. It is indicated that, because of the strong influence of fluvial carbonates, the pco2 of surface water in the changjiang estuarine area and near the hangzhou bay were obviously higher than the pco2 of air ( especially in summer, autumn and winter ), while the pco2 in the mid east china sea was apparently lower than the atmospheric pco2. it is also shown that the pco2 in the southern east china sea, near the black ( kuroshio ) current, is higher than atmospheric pco2, especially in spring and summer

    東海表層海水的pco :分佈大致有以下幾個特點:有明顯的空間和季節變化;長江口及杭州灣鄰近海域海水pco :明顯高於大氣pcoz ，尤其是在夏、秋、冬季尤為突出，表明有河流碳酸鹽系統的強烈影響;在東海中部有大片區域海水pco :顯著低於大氣pcoz ，在南部靠近黑潮的大片區域里，尤其是春、夏季節，海水的pco :高於大氣pc02 。
  9. When choosing evaluative indexes, we take four aspects of fatalness of sea level rise hazards, vulnerability of land system, socio - economic and ecological vulnerability, and defending ability. we draw the map based on the relief map and the land utilizing map of 1 : 100000 scale, gain altitude values ( range of 1 km 1 km ) and the fundamental data of evaluation in the studied area using the software of mapinfo and socio - economic statistic data

    運用mapinfo軟體和社會經濟統計數據，以盤錦市1 ： 100000地形圖和土地利用圖作為底圖，獲得地面1km 1km范圍高程值以及評估單元基礎數據，並計算出在沒有防護、不同潮位背景、海平面上升不同高度的條件下，遼河三角洲未來海平面上升將淹沒的土地面積、受災人口和經濟損失，以及不同土地利用類型的淹沒面積及相應的經濟價值。
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