氣旋中心 的英文怎麼說

中文拼音 [qìxuánzhōngxīn]
氣旋中心 英文
center of cyclone
  • 氣 : Ⅰ名詞1 （氣體） gas 2 （空氣） air 3 （氣息） breath 4 （自然界冷熱陰晴等現象） weather 5 （氣味...
  • 旋 : 旋Ⅰ動詞1 （旋轉） whirl 2 （用車床切削或用刀子轉著圈地削） turn sth on a lathe; lathe; pare Ⅱ名詞...
  • 氣旋 : [氣象學] cyclone; low
  1. There are negative latent and sensible heat fluxes in south and east of the cyclone central area after it moved to ocean

    氣旋出海后在氣旋中心區南方和東方存在負潛熱通量和感熱通量區。
  2. Because of the low temperature there, water vapour condenses into small, clear crystals. a layer of glossy cirrus forms which drifts out from the centre of the tropical cyclone because of divergence at that level. so, when the outer edge of a tropical cyclone reaches hong kong, we can see cirrus high in the sky

    熱帶氣旋強烈的上升氣流會把潮濕的空氣帶到近五六千公尺以上的高空，由於溫度很低，水氣結成了透明的小冰粒，形成像絹絲一樣發光的雲彩-捲雲，這些在高層輻散流場區域的捲雲，會從熱帶氣旋中心向外流出，所以當香港還是位於熱帶氣旋邊緣時，我們便已看到那些在熱帶氣旋外圍的捲雲，並稱為臺母。
  3. Information on the nearest approach together with an estimate of the minimum central pressure of each tropical cyclone during its closest approach, the maximum winds at king s park and chek lap kok and waglan island, the minimum mean sea - level pressure recorded at the hong kong observatory and the maximum storm surge ( the excess of the actual water level over that predicted in the tide tables ) recorded at various tide stations in hong kong are included

    資料包括熱帶氣旋最接近香港時的位置及時間和當時估計熱帶氣旋中心附近的最低氣壓、京士柏及赤?角及橫瀾島錄得的最高風速、香港天文臺錄得的最低平均海平面氣壓以及香港各潮汐測量站錄得的最大風暴潮（即實際水位高出潮汐表中預計的部分） 。
  4. Information on the nearest approach together with an estimate of the minimum central pressure of each tropical cyclone during its closest approach, the maximum winds at king s park and waglan island, the minimum mean sea - level pressure recorded at the hong kong observatory and the maximum storm surge the excess, in metres, of the actual water level over that predicted in the tide tables recorded at various tide stations in hong kong are included

    資料包括熱帶氣旋最接近香港時的位置及時間和當時估計熱帶氣旋中心附近的最低氣壓京士柏及橫瀾島錄得的最高風速香港天文臺錄得的最低平均海平面氣壓以及香港各潮汐測量站錄得的最大風暴潮即實際水位高出潮汐表中預計的部分，單位為米。
  5. In the past, whenever a tropical cyclone was centred within the region bounded by 10 - 30 degrees north and 105 - 125 degrees east area shaded in deep green in the figure, the observatory would display the positions and forecast track of the tropical cyclone on its website every 3 hours

    在過去，當熱帶氣旋中心位於北緯10至30度，東經105至125度以內圖中深綠色范圍，天文臺會每三小時在網上發放該熱帶氣旋的位置及預測路徑圖。
  6. Commencing today, for those tropical cyclones centred within the region bounded by 7 - 36 degrees north and 100 - 140 degrees east area shaded in light green in the figure, their positions at 8 a. m. and 8 p. m. and 72 - hour forecast tracks will be made available on the observatory s website at around noon and midnight respectively

    為了更早向市民提供熱帶氣旋的資料，從今天開始，當熱帶氣旋中心位於北緯7至36度，東經100至140度以內圖中淺綠色范圍，天文臺會在每天約中午及午夜在網上發放該熱帶氣旋分別在上午八時及晚上八時的觀測位置及72小時的預測路徑圖。
  7. If the cyclone s centre comes closer to hong kong, winds will increase and rain can become heavy and widespread

    若熱帶氣旋中心移近本港，風力便會增強，廣泛地區可能會有大雨。
  8. If the centre of the tropical cyclone comes closer to hong kong, winds will increase and rain may become heavy and widespread

    若熱帶氣旋中心移近本港，風力便會增強，廣泛地區可能會有大雨。
  9. Generally under 300hpa the subsidence zone of the potential vorticity lies above cyclone at the violent stage of the development of the cyclone, however, the center of cyclone still lies near the potential vorticity of large value above 300hpa

    氣旋強烈發展期，一般300hpa以下，位渦的下沉區在氣旋的上空， 300hpa以上氣旋中心仍位於大值位渦後部。
  10. This paper discuss the effect of roughness coefficient on the tropical cyclone landfalling process using a idealized tc model developed from psu / ncar mm5 in the condition of quiescence and f - plane atmosphere. in order to understand the different influences of land and sea surfaces in the tc landfalling process, two kind of experiments had been designed : one for settled tc, the other for movable tc, and each kind consists four tests. the result indicates that the distribution of wind, precipitation, warm core and intensity of tropical cyclone has been changed obviously due to the effect of difference between the land and sea

    本文利用bogus技術在psu / ncarmm5中加入了理想熱帶氣旋初始渦旋，在f -平面和無環境流場的理想情況下，設計了兩組靜態和動態試驗，通過控制試驗和不同粗糙度的登陸試驗，分別從空間和時間上探討了理想熱帶氣旋的登陸規律和分佈特徵，特別研究了邊界層中熱帶氣旋中心區域風場的垂直細致結構，並初步分析了其物理機制。
  11. The high - resolution image captured on 16 july 2004 shows vividly the appearance of kompasu, including the dense cloud cover near its centre and the outer cloud bands

    在2004年7月16日拍攝到的高解像度圖像，清晰顯示出圓規的外觀，包括接近氣旋中心的稠密雲區及外圍雲帶。
  12. Obviously silicon effect is observed in the transition stage. ( 2 ) thermal decomposition of bamboo is mainly concerned with radicals from the decomposition of hemicellulose, cellulose, and lignin in bamboo. ( 3 ) moisture and the carbonized atmosphere have effects on the properties and relaxation mechanism of spin centers

    （ 3 ）竹炭中的水分和炭化氣氛對自旋中心的性質和弛豫機制都產生了比較明顯的影響，並且在不同的炭化階段產生的影響不同。
  13. During the passage of tornadoes or waterspouts, the direct impact of very strong winds and the difference in pressure between the interior and outside of a building can shatter weak structures, and even blow away trees and vehicles

    渦旋中心附近的氣壓非常低，並且風力強大。卷風經過時，單薄的建築物可能會抵受不住強大風力及室內室外的氣壓差而損毀，樹木及汽車等會被吹起。
  14. During the passage of tornadoes or waterspouts, the direct impact of very strong winds and the difference in pressure between the interior and outside of a building can shatter weak structures, and even blow away trees and vehicles. there have been reports of small boats capsizing in nearby waters on encountering waterspouts

    渦旋中心附近的氣壓非常低，並且風力強大。龍卷風經過時，單薄的建築物可能會抵受不住強大風力及室內室外的氣壓差而損毀，樹木及汽車等會被吹起。在海上曾經有小型船隻遇到水龍卷而沉沒。
  15. The principal contributions of this dissertation are : 1. a high fidelity and real - time rotor wake inflow model was built up. based on peters - he finite states wake theory, a new influence coefficient matrix for high speed flight was derived, the modified wake model is better suitable for the flight state with a large wake skew angle

    本模型以peters - he有限狀態尾跡理論為基礎，修正了大尾跡傾斜角時的誘導速度影響系數矩陣，並結合了王氏渦流理論，導出了旋翼誘導速度垂向分量和旋轉分量的表達式，可計算平尾、尾槳和垂尾氣動中心處誘導速度各分量。
  16. The main conclusions show as following : 1 the effects of propagating vortex rossby waves on tc intensity change are relative closely to the position, the size and intensity of the initial disturbance

    主要結果可歸納如下： 1渦旋rossby波傳播對熱帶氣旋強度變化的影響，與初始擾動相對渦旋中心的位置、初始擾動尺度大小及強度等關系密切。
  17. The intensity is given in terms of the maximum sustained wind speed near the centre of a tropical cyclone

    強度以接近熱帶氣旋中心的最高持續風速來表達。
  18. E. in addition, information on the intensity of tropical cyclone in terms of the maximum sustained wind speed near its centre will also be provided

    此外，亦會提供接近熱帶氣旋中心的最高持續風速以表達熱帶氣旋的強度。
  19. In this publication, tropical cyclones are classified into the following four categories according to the maximum sustained surface winds near their centres

    本年報根據熱帶氣旋中心附近的最高持續地面風速，把熱帶氣旋分為以下四個級別：
  20. The action that weak cold air penetrated into the tropical cyclone made the low pressure become vortex potential instability, and finally turned into kinetic energy. the results were that the center pressure of low became lower, the wind velocity around the cyclone was stronger and the precipitation became more

    冷空氣在中低層的滲透主要使大氣斜壓作用加強，使不穩定能量的積聚並最終釋放；還造成臺風渦旋位勢不穩定，使熱帶氣旋中心氣壓降低，周圍風力加大，因而產生更大的降水。
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