ocean depth 中文意思是什麼

ocean depth 解釋
大洋深度
  • ocean : n 1 洋，大海；（有別于內海的）外洋。 ★ 英國用 sea 的地方，美國常用 ocean 如：spend some weeks by ...
  • depth : n. 1. 深；深度。2. （色澤的）濃度；（聲音的）低沉；（感情等的）深厚，深沉，深刻。3. 進深。4. 〈常 pl. 〉深處；深淵，深海，海。5. 正中，當中。6. 深奧，奧妙。
  1. By physiognomy feature, it could be divided into three types of thermal structure : positive dome model, negative collapse model and border dome core collapse model. based on the depth degree or magma - thermal influenced, it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model, superficial volcano eruption hydro - thermalism and hypabyssal intrusive model, thermal anticline ( thermal dome ) model, mid - deep intrusive model, deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure. there are many interaction system could be induced into a systematic thermal interaction, include : ocean - continent system, basin - mountain interaction, superficial and mid - deep crust - mantle interaction, crust - mantle commingle interaction, vertical thermal interaction ( delamination ) etc.

    依據地貌形態分為三類：正向穹窿型、負向塌陷型、邊隆核陷型：依據巖漿-熱力作用影響的深淺程度或深度分為五類： （古）地熱異常群集區、表淺層火山噴發-熱液活動與淺成侵入型、熱力背斜（熱穹窿） 、中深層侵入型、深部地幔（地殼）熱柱型；提出了熱力構造作用空間分佈的理想模式，將洋陸系統、盆山作用、淺表與中深部殼幔作用、殼幔混合、垂向熱力作用（拆沉）等納入一個整體統一的熱力作用系統中，為盆地動力學研究打開了一個新窗口；研討了熱力構造研究方法。
  2. They pined in depth of ocean shadow, gold by the beerpull, bronze by maraschino, thoughtful all two, mina kennedy, 4 lismore terrace, drumcondra with idolores, a queen, dolores, silent

    她們在海洋的陰影深處苦苦地戀慕著105 ，金發女侍守在啤酒泵柄旁，褐發女侍挨著野櫻桃酒兩個人都陷入沉思。
  3. In this paper, features of decadal variability and the possible mechanism of sea - air system in the pacific are investigated by using upper - ocean temperature, heat storage and wind stress data, the main results are as follows : the most pronounce decadal sign exists at about 160 meter in depth in the western pacific. there are significant decadal abrupt changes in temperature from surface to deep in the subsurface at about 1980. with different depth in the subsurface, there exist 4 types of abrupt change modes, their generation is closely related to the decadal sign which originates from the east of north pacific and propagates along the south - west subduct ion route

    研究表明，太平洋次表層海溫最強的年代際信號在熱帶西太平洋約160m深處，此信號在1980年前後從上至下，先後經歷了一次顯著的年代際突變過程，而且隨深度的不同存在著四種不同的空間突變模態，這四種模態的形成與北太平洋海溫異常的西南潛沉路徑有著密切的聯系。
  4. Wellspring of the joy of living, ocean depth of happy rest

    榮光歸于愛咱的主，洗咱罪過無暇疵，
  5. It is a rock of almost conical form, which looks as though it had been thrust up by volcanic force from the depth to the surface of the ocean

    它像是一塊圓椎形的大巖石，似乎是某次海底火山爆發把它推到海面上來的。
  6. Results rectify that matched field processing based on ray travel time delay is insensitive to the mismatch of sound speed proflle, although the mismatch of ocean bottom depth and receiver location is bad to matched field processing, different forms of cost fimctions could decline the sensitivity

    計算結果表明，基於聲傳播時延的匹配場定位對聲速分佈失配是不敏感的。雖然接收基陣位置傾斜和海洋深度誤差對匹配場處理影響較大，但只要選擇適當的代價函數，可以得到克服。
  7. In the ocean, the velocity of sound varies with the temperature, salinity, and depth of the water.

    在海洋中，音速隨著水的溫度、鹽分和深度而變化。
  8. This creature lives in the depth of the ocean

    這種生物生活在海洋深處。
  9. The correlation analysi s between sst and sea surface height, heat content and depth of thermocline also shows the important role of ocean dynamic processes in some regions, besides the influence of heat exchange between air and sea

    Sst與海表面高度、熱含量、溫躍層深度等的相關分析也表明，在某些區域，除受海洋-大氣之間熱交換的影響外，海洋動力過程對sst的影響也占重要地位。
  10. Under these fimctions, mismatch of ocean depth, receiver location and sound speed profile have been simulated respectively

    文中運用該函數分別對海底深度、接收基陣位置和聲速分佈三種失配情況進行計算機模擬研究。
  11. Different results specify that the first kind of cost function is sensitive to the mismatch of ocean depth and receiver location, but is insensitive to sound speed profile ' s % $ jai8x9 @ t $ m & z mismatch and has high accuracy of depth localizaion ; the second kind of cost fimction is insensitive to all three kinds of mismatch, but its resolution of depth is very low ln order to overcome the cost function ' s sensitivity to mismatch, improvemedt of the accuracy of time delay estimation and model calculation may be adopted, when both conditions are reached, the sensitivity wiil be greatly reduced and the resolution of range and depth will be improved at the same time

    模擬結果表明，第一類代價函數對海底深度和基陣傾斜失配是敏感的，對聲速失配卻不敏感，並且能夠獲得較高的深度定位精度；第二類代價函數對三種失配都不敏感，只是深度解析度較低。為了克服代價函數對失配的敏感性，可採用提高時延估計精度和模型計算精度的方法。當兩個條件滿足時，敏感性得到極大的抑制並獲得了較高的距離和深度估計精度。
  12. The migration results of the synthetic and ocean field datasets show that this method is correct and effective. several prestack depth migration methods are proposed and unified to the synthetic source record migration method. these methods include plane wave migration with fourier finite difference ( ffd ) extrapolator, maximum energy plane wave migration and prestack migration with phase encoding of areal shot records

    通過對本文提出的平面波傅立葉有限差分疊前深度偏移方法、最大能量面炮記錄疊前深度偏移方法和相位編碼面炮記錄疊前深度偏移方法的研究，試算和對比，提出了合成震源三原則，根據這些原則，提出了合成震源概念和合成震源記錄疊前深度偏移方法。
  13. In the middle of the atlantic ocean, with a salinity of 3. 2 %, a vlf signal will penetrate down to a depth of 10 - 20 meter, barely periscope - depth for a modern large scale submarine

    在大西洋中部，海水的鹽度為3 . 2 % ，甚低頻無線電信號可以穿透到海面下10 ~ 20米的深度，幾乎就是現代大型潛艇的潛望鏡深度。
  14. According to the laminar flow or ocean current to confirm the depth of floater and the elasticity of raft body

    依據平流或海流大小剎入漂深度，確定筏身松緊程度。
  15. Most deep ocean basins range in depth from about 4 to 6 kilometers, with some narrow trenches near pacific ocean basin margins dropping to as low as 11 km below sea level

    大多數海盆在深度上從4公里到6公里左右，在太平洋附近海盆邊緣有些狹窄海溝可以陡降到海平面以下11公里處。
  16. In linear potential theory regime, a problem on the oscillations of the harbours of arbitrary shape and constant depth in open ocean was analyzed

    摘要利用線性勢流理論對定常水深且置於廣闊海域中的任意形狀港灣在入射波作用下的港內振動進行了研究。
  17. Discover the real depth and cold of the bottom of the ocean and get back

    發現真正的深度和大海的底部寒冷而且回來。
  18. This method is a novel, simple method calculating the ocean wave force on floater. you can find the rule between ocean wave force and time at any moment, and get the biggest ocean wave force on floater if you give the actual instance of the sea, the geometrical dimension of the floater and the depth of the floater in the water

    這種計算方法是一種新穎的計算漂浮體上波浪力的簡單方法，在計算波浪力的過程中，只需要給出實際海況，浮子幾何大小，以及浮子吃水深度就可以求得波浪力隨時間的變化規律，並可求得浮子所受的最大波浪力。
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