height of the tide 中文意思是什麼

height of the tide 解釋
潮高
  • height : n 1 高，高度；身高；海拔。2 〈常 pl 〉高地，山丘。3 高貴，卓越。4 絕頂，頂點；【聖經】天。5 〈罕...
  • of : OF ＝Old French 古法語。
  • the : 〈代表用法〉…那樣的東西，…那種東西。1 〈用單數普通名詞代表它的一類時（所謂代表的單數）〉 （a） 〈...
  • tide : n 1 潮，潮汐，漲潮時。2 消長，盛衰。3 潮流，趨勢，傾向，形勢，時機，機運。4 【礦山】班，十二個鐘...
  1. In hong kong, most storm surges would have a height of 0. 5 to 1. 0 metre. in extreme conditions, the water level could exceed the tide level by more than three metres, bringing sea flooding to coastal low lying areas

    香港出現的風暴潮高度一般在0 . 5至1 . 0米之間，但在極端情況下，風暴潮可以高達三米以上，引致沿海低?地區受海水淹浸。
  2. Based on systematical study of each constituent of iss, the foundation, computation and precision analysis of the models of geoid, sea surface topography, mean sea surface and ocean tide are mainly discussed ; the conceive of mean sea surface height model and ocean tidal model suitable to chinese near sea and its neighborhood is provided ; two kinds of iss model are derived out

    本文在系統研究瞬時海面高各組成要素的基礎上，主要討論了大地水準面模型、海面地形模型、平均海平面模型和海洋潮汐模型的建立、計算以及精度評價等問題；提出了建立適於我國近海及鄰域平均海平面模型和海洋潮汐模型的設想；綜合得出了兩種瞬時海面高模型，並進行了精度估計，編制了相應的軟體。
  3. However, the application of global tidal model to the study of shallow sea tides is much worse in the accuracy. tidal signal in topex / poseidon altimetric data is the largest contributor to sea surface height variability and accounts for more than 80 % of the signal variance. so it is urgent to develop tide model in the shallow area wi th high accuracy

    潮汐是高度計資料海面變化中最大的成份，占總變化80以上，伴隨著衛星高度計資料在海洋研究中的廣泛應用，發展基於衛星高度計資料的高精度淺海潮汐模型成為進一步利用高度計資料研究其它物理海洋問題的基礎。
  4. A severe earthquake is expected to generate or has generated a tsunami. if the tsunami persists, it would reach hong kong within 3 hours, and the height of the tsunami may exceed 0. 5 metre above the normal tide level

    猛烈地震預計會產生或已產生海嘯。若海嘯持續，將會在3小時以內到達香港，而海嘯高度可能會超過正常潮水高度0 . 5米。
  5. In fact, the transformation and unification of the local height datums have relations to the mean sea level variation at the shore where the tide gauges are located

    局部高程基準的轉換與統一，不得不涉及沿海各主要驗潮站平均海平面的變化。
  6. First, the defmation and status of height datums is introduced and some problems on the local height datums established by the mean sea level, which is defined by the tide gauge data, are discussed. then the research progresses in recent years are analysed

    首先介紹了高程基準的定義與現狀，指出了用驗潮站長期平均海平面建立局部高程基準所存在的問題；分析了當今國內外高程基準的研究現狀；進一步明確了我國高程基準現代化的必要性。
  7. Then the origin vertical shift of cnhd85 with respect to whd is calculated from geopotentials. and the systematic difference and its distribution of cnhd85 is analyzed from the difference of height anomalies. at last, the systematic difference of the mean sea level at qingdao tide gauge is further testified from the sea surface topography model

    然後基於位理論方法求出了1985國家高程基準點的垂直偏差，基於高程異常差分析了1985國家高程基準的系統差及其分佈規律，最後基於海面地形模型進一步揭示了青島驗潮站平均海平面的系統差。
  8. If the tsunami persists, it would reach hong kong within 3 hours, and the height of the tsunami may exceed 0. 5 metre above the normal tide level

    若海嘯持續，將會在3小時以內到達香港，而海嘯高度可能會超過正常潮水高度0 . 5米。
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