strong storm 中文意思是什麼

strong storm 解釋
強風暴
  • strong : n 斯特朗〈姓氏〉。adj 1 強壯的，有力的，有膂力的；強健的；鞏固的，堅牢的，堅固的；堅強的（性格等...
  • storm : n 1 暴風雨，暴風雪，大雪雨，大冰雹，狂風暴雨；【海、氣】暴風〈風力十一級〉。2 （政治、社會上的）...
  1. One night, the winds angered, the clouds burst and a strong storm overturned a fishing boat at sea

    一個夜晚，風激怒，雲爆裂，而且一陣強壯的暴風雨在海上推翻一艘漁船。
  2. One night, the winds angered, the clouds burst and a strong storm overturned a fishing boat at sea. the crew in trouble sent out the sos

    一個夜晚，風怒吼，雲翻滾，猛烈的暴風雨打翻了一艘（尚未返航的）魚船無計可施的船員發出了求救信號。
  3. The three - dimensional cloud model with hail - bin microphysics could simulate the characteristics of the severe storm such as life cycle, rainfall distribution and diameter of hail well, and also could produce strong downdraft and wind shear ( downburst )

    而利用三維強冰雹雲模式對此次強風暴的生命史、降水分佈、降雹的大小等要素做了較好的模擬，並能夠模擬出伴隨強風暴過程所產生的強下沉氣流和及地面強風速切變（下擊暴流） 。
  4. The result shows that : the sand - dust storm occured in favorable climate background that is drought and rainless, the tilted trough and mongolia cyclone are the important weather systems that caused the severe sand - dust storm, tilted trough and strong frontal zone caused the mongolia cyclone developed and the clod front strengthened at surface, high jet and ferrel circulation are the main reason that momentum spreaded downward from higher level and frontal zone strengthened on lower level

    結果表明：沙塵暴是在乾旱少雨的有利的氣候背景下產生的。斜壓槽和蒙古氣旋是觸發這次強沙塵暴天氣過程的重要的天氣系統，高空斜壓槽和強鋒區促使了地面蒙古氣旋的發展和冷鋒的加強，誘發沙塵暴天氣。高空急流及其下方的ferrel環流起到了高層動量下傳和加強低層鋒區的重要作用。
  5. Sand - dust storm is a kind of calamitous weather phenomenon, which means that strong breeze draws much sand and dust on the surface into the sky, making air very foul and with visibility lower than 1km

    沙塵暴系指強風把地表大量沙塵捲入到空中，使空氣特別渾濁，水平能見度低於1km的災害性天氣現象，是重要環境問題之一。
  6. On an average a strong gale moves at the rate of40 miles an hour, a storm at about56 and hurricanes at90

    平均來說，八級大風每小時風速達40英里，十一級風暴達56英里，而十二級颶風則達90英里。
  7. And the resuits are as follows : the main hazards in rural area were flood, water - logging, landslide and debris flow, whereas water - logging in cities ; the catastrophe was caused by the natural factors including the heavy rain due to the strong tropical storm, the mountainous terrain conditions in xiangjiang river basin, and the man - made factors including unreasonable project construction, the imperfect disaster warning mechanism, the weak consciousness on disaster prevention and the unperfect disaster risk transfer mechanism etc

    結果表明：農村的主要致災因子是洪水、內澇、滑坡、泥石流，而城市主要為內澇；此次巨災是在強熱帶風暴引發的暴雨、湘江流域中上游多山的地形條件等自然因素，和工程建設不合理、災害預警機制不夠完善、人們防災意識薄弱以及災害風險轉移機制不夠成熟等人為因素的共同作用下導致的。
  8. Although the accuracy in meterological forecast of tropical cyclones has been distinctly improved, it is still a difficult problem confronting masters and anti - typhoon team leaders of the companies how to steer clear of typhoon reasonably and safely in case that the actual resistance to typhoon is strong enough, the sea area wide enough, and the time permitting ; to avoid unreasonable deviation, anchoring for shelter, blindly rushing onto her path, being involved in storm area, even into the the center of typhoon ; under the limitation of the condition of the sea area and time. how to take correct meassures to escape, such as navigating with wind or windward in bias angle, slowing down, anchoring, berthing alongside the warf, mooring to buoy, etc. as early as possible

    盡管氣象部門對熱帶氣旋監測預報的準確率已經比過去有了明顯的提高，然而船舶在海上如何避離臺風，如何做到在本船實際抗風能力允許、海域條件允許、時間也充裕的前提下合理避臺，安全避臺，避免不合理的繞航、 「扎風」 ，避免盲目冒進「搶風頭」 ，更避免被捲入強風區甚至臺風中心；在海域條件受限、時間尷尬的情況下又如何正確採取偏順航、偏頂航、滯航、錨泊、系岸、系浮等抗臺措施和技術，盡快擺脫臺風的影響，仍然是擺在船長和公司防抗臺領導小組面前的一個實實在在的難題。
  9. The initial field of the model is the in situ observational data. combining the observational data by the doppler weather radar, the distribution and evolution of macro - physical as well as micro - physical variations such as wind field structure, radar echo structure, overhang echo, bound weak echo region, strong echo wall, water content, etc. in the storm were analyzed

    利用中國科學院大氣物理研究所建立的完全彈性三維雹雲數值模式，模擬了1996年6月29日發生在北京東北部京冀交界地區的一次強單體雹暴過程，並結合多普勒雷達探測資料，分析了風暴的流場結構，雷達回波結構特徵，含水量場等宏微觀物理量的分佈及其演變。
  10. A strong pacific storm system moved through parts of the far west over the holiday weekend

    美國遠西棉區節后遭遇一股太平洋風暴襲擊。
  11. I heard a gun fire, and supposed the storm had proved too strong for us, and we were firing signals of distress.

    聽到一聲炮響，我認為一定是風暴太猛烈，所以發出遭難求救的信號。
  12. A single triangular sail, of strong canvas, was hoisted as a storm - jib, so as to hold the wind from behind. then they waited

    艙面上只留下一張厚布三角帆代替船頭上的大帆，以便利用背後吹來的大風繼續航行。
  13. The paper analyzes and summarizes the following laws of distinctive sediment yield produced in storm floods of the region based on predecessors ' study : storm is the main dynamic force of erosive sediment yield and storm, flood and sediment exist an inevitable relation ; the flood occurring time is concentrated with high peaks and huge volume, suddenly rising and suddenly falling and has decisive influence to the formation of a major flood peak in the middle yellow river ; the main reasons of concentrated coarse sediment of the river is severe erosive sediment yield, strong sediment transporting capacity and high sediment concentration ; the important influence of frequent or continued storm floods happened in he - long reach especially in coarse sediment concentrated region to the sediment transport of the yellow river and ; along with the increase of harnessing, regional flood trend is becoming smaller but the variation of sediment quantity is not obvious and the reaction of peak discharge and flood runoff of majority tributaries are not sensitive, showing that a general and normal engineering works can not effectively control regional major floods especially the sediment of an extraordinary flood

    摘要在前人研究的基礎上分析總結了該區特有的暴雨洪水產沙規律：暴雨是侵蝕產沙的主要動力，暴雨、洪水、泥沙之間存在著必然的關系；洪水發生時間集中，峰高量大，暴漲暴落，對黃河中游大洪峰的形成具有決定性影響；侵蝕產沙強烈而粗泥沙集中，輸沙能力強，洪水含沙量高，是黃河粗泥沙的集中來源地；河龍區間特別是粗泥沙集中來源區頻繁或連續的暴雨洪水對黃河輸沙有重要影響；隨著治理水平的提高，區域洪水有減小趨勢，但泥沙量變化不明顯，大部分支流的洪峰流量、洪水含水量反應不敏感，說明一般規模和水平的治理工程還不能有效控制區域大洪水特別是特大洪水的泥沙。
  14. [ bbe ] for you have been a strong place for the poor and the crushed in their trouble, a safe place from the storm, a shade from the heat, when the wrath of the cruel ones is like a winter storm

    因為當強暴人催逼人的時候，如同暴風直吹墻壁，你就作貧窮人的保障，作睏乏人急難中的保障，作躲暴風之處，作避炎熱的陰涼。
  15. Surprisingly, the weather report on the evening before the storm said there would be strong winds, but not a hurricane

    令人驚奇的是，風暴發生之前的那個晚上，天氣預報說，將有強風，而沒有颶風。
  16. The results show that the auto - conversion of frozen drops and graupels ( cnfh, cngh ) are the main sources of the hailstones in the strong convective storm studied in the paper, but the contribution of frozen drops is greater than that of graupels. hailstones mainly depend on the processes of collecting supercooled water ( clch, clrh ) to grow. the relatively simple mass continuous equation was used to calculate vertical velocity, and use radial projection relation of dual - doppler radar to retrieve the case ' s three - dimensional wind field

    同時模擬分析了冰雹形成的微物理過程，結果表明，本個例模擬雹雲中，冰雹粒子主要由凍滴和霰轉化（ cnfh ， cngh ）形成，但凍滴對冰雹形成的貢獻要比霰大得多，冰雹含水量中心的發展演變與凍滴含水量中心的發展演變相一致，冰雹主要是通過撞凍過冷水過程（ clch ， clrh ）而進一步長大的。
  17. Several influence factors to result plasma drift in hainan were analyzed. in this paper the characteristics of ionospheric parameters variation were analyzed systematically and some new results in storm - time such as seasonal behaviors were obtained ; it is the first time to investigate the ionospheric drift behavior in hainan and some new results was obtained, the relationships between each two plasma drift velocity components in storm time in hainan were found and the electric filed variation in hainan ionosphere also was obtained ; the results also show that there are big differences of the ionosphere parameters bo and bl obtained from the data with that obtained from the iri - 2001 applied for hainan ; a new phenomena was found during a strong magnetic storm, that a layer with very strong electron density and density grad was found during the recovery phase of the storm, its horizontal scale is beyond 100km and temporal scale is about 2 hours, this phenomena repeated 3 times continuously. a type of negative disturbance in high and low latitude but positive disturbance in east - asia also has been found

    本文較為系統地給出了海南地區電離層的參數變化特徵，特別是得到了一些暴時與以往不同的季節特性；第一次給出了海南地區的電離層等離子體漂移特徵，發現等離子體漂移暴時擾動在三個方向上有內在的聯系，得到了電場變化曲線；研究結果還表明海南電離層的半厚指數和形狀參數等與國際參考電離層iri - 2001存在很大差別；通過對強磁擾動事件期間的參數變化特性分析發現，在磁暴恢復相期間海南地區電離層底部存在一個電子密度非常大的高密度區，高密度區底部電子密度梯度隨高度急劇增加，該區域的水平尺度可達100公里以上時間尺度約為2小時，連續出現過三次，這是一個在海南從來未發現的新現象；研究還發現了暴時東亞地區電離層擾動會出現高低緯負相而中緯正相的現象。
  18. B issue no. 3 or no. 8 signal as the case may be when half or more anemometers in the reference network register or are expected to register strong winds or gale storm force winds and the wind condition is likely to persist

    B發出3號或8號信號的準則為參考風力站網路內半數或以上的測風站錄得或預料錄得強風或烈風暴風，且風勢可能持續
  19. Residents in parts of the midwest will still be digging out today after a strong storm dumped feet of snow

    美國中西部地區的居民今天仍在被暴風雪覆蓋的幾英寸的雪裡被發現。
  20. There is to be strong storm and heavy rain in the coming three days, it is estimated that it will do great damage to shenzhen from tonight to tomorrow

    深圳市今日起3天內將有大到暴雨，今天晚上到明天白天， 「杜鵑」可能對深圳造成嚴重影響。
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