warm cyclone 中文意思是什麼
warm cyclone
解釋
暖氣旋-
Winter brings cool, dry weather with many bright days, while during the summer - the monsoon season, the weather is warm and humid, and rainstorms can be expected. between july and september is the most likely time for typhoons. there are five levels of tropical cyclone warning starting with 1 ( the lowest and least intense ) through 3, 8, 9 to 10 ( the highest and most critical )
香港的冬季大部份是乾爽涼快的晴天；夏季則屬季侯風季節，天氣溫暖潮濕，時有暴風雨， 7月至9月期間為香港的臺風季節，熱帶氣旋分為5級，由1級（最低程度及風力最弱）開始，然後可遞升至3 、 8 、 9及10級（最高程度及風力最強） 。 -
The occurrence of cirrocumulus clouds indicates the distant presence of a convergent zone such as a pressure tough or a cyclone in lower levels ; or a frontal zone where cold air meets moist warm air. vigorous convection and lifting motion bring water vapour up in the sky where the water vapour sublimes into ice crystals, forming the high clouds
卷積雲的出現顯示遠處地方低層有一強輻合帶如低壓槽或氣旋或鋒面即暖濕空氣碰到冷氣團，向上爬升的交界面形成，強烈的對流和抬升運動將水汽帶到高空，在那裡水汽直接升華變為冰晶而形成高層雲。 -
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。 -
The circulation in bohai sea and yellow sea is basically of cyclone shape comprising the coastal currents and the yellow sea warm current. besides the real circulation simulation, numerical experiments were done to study the dynamic mechanism
另外，在真實環流模擬的基礎上，本文又進行了一些數值實驗，以考察各動力因子對冬季東中國海環流的影響。
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