wind speed 中文意思是什麼

wind speed 解釋
風速
  • wind : n 1 風；大風，暴風；氣流；【機械工程】壓縮空氣。2 【航海】上風；風向；〈古語〉〈pl 〉方向。3 氣息...
  • speed : n 1 快，迅速。2 速率，速度。3 （汽車的）變速器，排擋。4 （膠片，照相紙）感光速度。5 〈古語〉興隆...
  1. Lying between these high - speed air streams are air streams of lower wind speed

    在這些高速氣流之間，會出現較低速的氣流。
  2. On windy occasions such as the approach of a tropical cyclone, air streams of high wind speed may emerge from mountain gaps

    風吹越山脈在刮大風的時候，例如在熱帶氣旋逼近時，高速氣流會在山峽形成。
  3. Wind speed is the speed of the air flow. it is usually expressed in kilometres per hour or as a force on the beaufort scale

    風速是指空氣的移動速度，一般以公里每小時或蒲福氏風級來表示。
  4. From 1200 utc surface wind direction 150 degree south - southeasterly winds ; wind speed 15 knots ; visibility 10 km or above ; nil significant weather ; broken cloud at 2000 feet and broken cloud at 10000 feet

    由1200utc開始，地面風向為150度東南偏南風，風速15海里小時能見度10公里或以上並無顯著天氣狀況2000尺有疏鬆雲層， 10000尺亦有疏鬆雲層
  5. From 1200 utc surface wind direction 150 degree ( south - southeasterly winds ) ; wind speed 15 knots ; visibility 10 km or above ; nil significant weather ; broken cloud at 2000 feet and broken cloud at 10000 feet

    由1200utc開始，地面風向為150度（東南偏南風） ，風速15海里小時；能見度10公里或以上；並無顯著天氣狀況； 2000尺有疏鬆雲層， 10000尺亦有疏鬆雲層
  6. Temporarily between 0800 utc and 1200 utc surface wind direction 170 degree ( south - southeasterly winds ) ; wind speed 25 knots gusting to 40 knots ; visibility 1000 m in thunderstorm with moderate rain ; scattered cloud at 1000 feet including cumulonimbus cloud and broken cloud at 2000 feet

    在0800utc至1200utc之間，地面風向間中為170度（東南偏南風） ，風速25海里小時，陣風達40海里小時；能見度在雷暴及和緩雨勢中為1000米； 1000尺有零散雲層，包括積雨雲， 2000尺有疏鬆雲層
  7. Based on the field investigations and laboratory examinations, a study of the population of the epiphytic dolichomitriopsis diversformis ( mitt. ) nog. in fanjing mountain reveals that its habitats are different among different host trees, but that there lies the common habitat characteristics of not more than 2m height from the bottoms of host trees trunks, less light, high relative humidity, slow wind speed, slow evaporation speed and long time of remaining humid in middle - lower tree bark ; that it is one dioecious moss species, the morphology is remarkably different between its perichaetium and perigonium, the number of its perichaetia is much more than that of its perigonia, its perigonium is difficult to find out, its sporophyte is upright, its seta is long and thin, its capsule is regular long oval and its calyptra is cucullate

    摘要通過野外調查和室內觀測對貴州省梵凈山樹附生尖葉擬船葉蘚種群的研究表明，其生境因其所附生的樹種不同而有所不同，但具有共同特點：附生在樹干下部距地面2m高的范圍之內，光照弱、濕度大、風速小、蒸發量小、中下部樹皮保持濕潤的持續時間長；其為雌雄異株蘚種，雌、雄器苞形態差異明顯，雌器苞數量多，雄器苞數量少並且難于發現，孢子體直立，蒴柄細長，孢蒴規則長卵形，蒴帽兜形。
  8. Specification for electrical contactor wind speed and wind direction recorder

    電接風向風速計技術條件
  9. It is shown that the error could be rather remarkable in some extreme situations and could be neglected in the others. the variance of parameters inside pixel, contexture of the pixel and the surface wind speed are the controlling factors of the scaling error

    結果表明亞像元狀態和結構是像元尺度誤差的主導因素，風速變化對尺度誤差有明顯的影響，不論何種形式的非均勻性，都須遵循相同的尺度擴展步驟，以達到消除誤差的目的。
  10. At the same time, i discover that the number of the return air inlet has a little influecing and it can be neglected. when there is hot resource at upperside of the room, the hot jet and supply air jet together affecting. at the same lower part heat intensity, a utmost wind speed exist, the supply air speed lower, the more heat intensity on the upside, the less convecting transfer heat, whereas

    對于上部有熱源的條件下，則其對流熱轉移量的變化關系是由熱射流與送風冷射流共同作用影響的，在下部熱源強度相同的條件下，存在一極限風速，在該風速以下，上部熱源強度越大，則對流熱轉移量越小，反之在該風速以上，上部熱源強度越大，則對流熱移量越大。
  11. The thesis focuses on the development of the dynamic simulation model of evaporators, the accomplishment of the stable and dynamic simulation of the parameters of cryogen - side, air - side and how to carry out dynamic simulation on the refrigerating effect of evaporators under different evaporating temperature and the realization of the analyses and calculations of the main parameters, such as, the wind speed of air - side and specific humidity etc, which affect the function of evaporators

    本文重點是對蒸發器建立動態模擬模型，並對製冷劑側和空氣側參數進行穩態和動態模擬，同時對蒸發器在不同蒸發溫度下的製冷量進行了動態模擬，而且對影響蒸發器性能的主要參數（空氣側入口風速、入口含濕量等）進行了分析和計算。
  12. The power curve indicates that doubling the wind speed will lead to an eightfold increase in power

    功率曲線顯示風速加倍將使功率增加8倍。
  13. A one - dimensional oceanic mixed layer model with the m - y level - 2. 5 turbulence closure schemes is employed. the rate of energy loss by breaking waves is estimated by parameterization and incorporated into the model as a source of turbulence kinetic energy ( tke ) by modifying the existing surface boundary condition of tke equation. the velocity field and turbulence energy budget are calculated under different forcing conditions ( the results given below are for a wind speed of 20 m / s. )

    採用一維2 . 5階湍封閉混合層模式，根據參數化方法對波浪破碎導致的能量耗散率進行了估計，通過改變湍動能方程的上邊界條件引入波浪破碎對湍動能生成的影響，計算了不同風應力強迫下的混合層流場結構和湍能量收支（下述給出的結果是取風速為20m s得到的） 。
  14. The exponent p is a function of wind speed, ground roughness, stability, etc.

    指數P是風速、地面不平度、穩定度等的函數。
  15. The variation of wind speed dominates the variation of latent heat flux eventually

    感熱通量的變化主要由海氣溫差的變化主導。
  16. Zhoushan has a northern subtropical monsoon marine climate with clear four seasons ; leading wind directions are southeast wind in summer, northwest wind in winter. with an annual average wind speed of 3. 3m s ; and an average temperature of 15. 6 - 16. 6, and the frost free period reaches 251 - 303 days perannum, annual average sunshine time 1941 - 2257 hours, and the annual preeipitation is 927 - 1620 mm

    舟山屬北亞熱帶南緣季風海洋型氣候，四季分明主導風向，夏季為東南風，冬季為西北風，年平均風速3 . 3米秒年平均氣溫15 . 6 . - 16 . 6 ，冬季最低溫為- 1 ，夏季最高溫度為37無霜期251 - 303天，年日照時數1941 - 2257小時年降雨
  17. A petrel does not dig a burrow where it does because of the average temperature or wind speed on the island but because of how warm or windy it is at that particular spot

    海燕並不會由島上的平均溫度或風速，來決定應該在哪裡挖掘洞穴，而是根據特定地點的暖度與風速而定。
  18. Monthly prevailing wind direction and mean wind speed recorded at the observatory and waglan island between 1971 - 2000

    表7 . 1971 - 2000年在天文臺及橫瀾島觀測之盛行風向及平均風速
  19. Monthly prevailing wind direction and mean wind speed recorded at the observatory and waglan island between 1961 - 1990

    表7 . 1961 - 1990年在天文臺及橫瀾島觀測之盛行風向及平均風速
  20. Among commonly used types are those employing either a propeller or cups for measuring wind speed and a vane for measuring wind direction.

    普通使用的型式是測量風速的葉扇或風杯及測量風向的風標。
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