diurnal current 中文意思是什麼

diurnal current 解釋
全日潮流
  • diurnal : adj 1 每日的；【天文學】周日的。2 晝間的，白天的 （opp nocturnal）。3 【植物；植物學】（花、葉等...
  • current : adj. 1. 通用的，流行的。2. 現在的，現時的，當時的。3. 流暢的；草寫的。n. 1. 水流；氣流；電流。2. 思潮，潮流；趨勢，傾向。3. 進行，過程。
  1. Using the split steps finite element method, the varied - boundary two - dimensional numerical model of diurnal tide and tidal current in the luoyuan bay is constructed

    摘要採用不規則三角形網格的分步雜交法，建立羅源灣海域二維變邊界全日潮汐和潮流數值模型。
  2. The diurnal constituents at some of the crossover points and all of the semi - diurnal constituents at all of the crossover points as well as 16 tidal gauge data are assimilated in the ocean model, this is because the assimilation of the diurnal constituents at some crossover points make the result worse. the improvement is 36 % for m2, 54 % for s2, 42 % for k, 30 % for 01 compared with the results of dynamic model without assimilation. in the stratified ocean, mixing controls the intensity of the ocean current

    為了克服交叉點上全日分潮精度較低的局限，文中主要將半日分潮同化進模式中，而全日分潮只在部分交叉點上進行了同化，同時同化了沿岸16個驗潮站的調和常數，同化高度計資料和沿岸資料后， m _ 2 、 s _ 2 、 k _ 1 、 o _ 1四個主要分潮的結果精度分別提高36 、 48 、 20 、 12 。
  3. After validating the good agreement between simulated results and observed ones, the characteristics and the distribution rules of tides and tidal currents in the whole seas near to zhejiang are thoroughly analyzed, mainly based on the simulated results, combining with the observed conclusion. the co - tidal and co - range charts, co - current charts, types of tides and tidal currents, distribution of maximum possible tidal range and maximum possible tidal current, phenomenon of diurnal inequality, moving modes of tidal currents, tidal ellipses, distribution of tidal residual currents and the vertical structure of tidal currents and residual currents are investigated respectively. and thereout we draw a series of meaningful conclusions as follows, the main of these are : 1

    在驗證模擬與實測符合良好的基礎上，本文以模擬計算結果為主，結合實測資料的分析結論，對整個浙江近海的潮汐、潮流特徵和分佈規律作了全面、深入的探討，分別對各主要分潮的潮汐同潮圖、潮流同潮圖、潮汐性質、潮流性質、最大可能潮差分佈、潮汐日不等現象、最大可能流速分佈、潮流的運動形式、潮流橢圓、余流分佈以及潮流和余流的垂向結構等進行了研究，並由此得到了一系列有意義的結論。
  4. The diurnal change of cg lightning is obvious, and it generally takes on bi - peak and bi - valley pattern. the two peak values occur at 15 : 00 and 03 : 00 respectively, whereas the two valley values occur at 09 : 00 and 22 : 00respectively. the mean current of positive cg lightning is slightly bigger than that of negative one

    閃電的發生也有明顯的日變化，總體呈雙峰雙谷形式， 15時和03時為兩個峰值，兩個谷值分別出現在9時和22時。
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