typhoon area 中文意思是什麼
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The low latitude systems such as typhoon, etc. affect the rainstorm in plateau through direct and indirect action. the synoptic systems within heavy - hard rainfall stagnated in the most of this area. 4
4 、高原東北部地區大到暴雨的雲圖特徵大都為不同性質雲系的疊置，可為高原及其鄰近地區的暴雨預報提供重要的依據。 -
New breakwaters would be constructed for reprovisioning the anchorage area affected by the reclamation. " the preferred option will accommodate the new prison complex within the existing typhoon shelter. the key advantages are less visual impact on the surrounding areas due to effective screening of the prison facilities by the existing topography, minimal impact on the marine and terrestrial ecology, and minimal impact on tidal flow and water quality
發言人說：按最可取的方案，會在喜靈洲避風塘內進行土地平整，興建新綜合監獄，主要的優勝之處是喜靈洲的地形能有效遮蔽監獄設施，對鄰近地方造成的視覺影響較小，而且對陸上和海洋生態、水質和水流的影響亦輕微。 -
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。 -
Eastern district lies in the northeastern part of hong kong island and covers a total area of about 1, 900 hectares, ranging from causeway bay typhoon shelter in the west to siu sai wan in the east
東區位於港島東北部，面積達1 ， 900公頃，西自銅鑼灣避風塘起，一直向東伸延至小西灣。 -
The reclamation area provides an opportunity for developing a continuous waterfront promenade extending all the way from the new central waterfront west of the planning scheme area to the eastern end of the causeway bay typhoon shelter
填海區提供機會以發展一條海濱長廊，由規劃區以西的新中環海旁一直延展至銅鑼灣避風塘東面盡頭。 -
The total area of eastern district is about 1, 900 hectares. the district lies in the northern part of hong kong island, starting from the causeway bay typhoon shelter in the western side, stretching eastward to victoria park, north point, quarry bay, shau kei wan, chai wan and siu sai wan
東區的總面積約為1 ， 900公頃，位於港島東北部，由西向東伸延的范圍，包括銅鑼灣避風塘、維多利亞公園、北角、 ?魚涌、筲箕灣、柴灣及小西灣。 -
The results show that the weather process occurs because of typhoon trough with cold air, deep upper trough ; the southeast low - jet by typhoon transported large water vapour and great energy of instability to heavy rainfaill area ; cold air, lower convergence and upper divergence by deep upper trough lead to development of the east - ocean low pressure and occurd strong wind
分析結果表明：這次天氣過程是由臺風倒槽和冷空氣及深厚的高空槽共同作用引起的；臺風環流引起的東南低空急流為暴雨區輸送了大量的水汽和不穩定能量；冷空氣的侵入加上深厚的高空槽引起的低空輻合、中高層輻散，促使了東海低壓的劇烈發展，產生了猛烈的大風。 -
In the case of the kwun tong typhoon shelter, improved levels of dissolved oxygen have arisen both because of the epd s ongoing efforts to reduce the discharge of wastewater into it, and because of the government s tolo harbour effluent export scheme, in which relatively clean treated effluent has been piped from the sha tin and tai po sewage treatment works in the tolo harbour area and released near the kwun tong typhoon shelter, raising oxygen levels in the water and improving water flow
另外政府所推行的吐露港污水輸出計劃也使觀塘避風塘的溶解氧逐步提高。吐露港污水輸出計劃是將吐露港區內經沙田及大埔污水處理廠處理過的污水經管道通至觀塘避風塘上游的啟德明渠排放，從而增加了明渠的流量，也提高避風塘的溶解氧水平。 -
The analysis of dry pv shows that the high pv dominate the area of typhoon, the higher is the center value of pv, the stronger is the typhoon. lt is also shown that the most important reason resulting in rainstorm is the cold air ( high pv ) which spreads to south from the upper troposphere or lower stratosphere and transports into the warm air. the joining situation of upper and lower pv area make vortex develop. pv transpotation reduces static stability, which increases the releasing of instability energy and makes rainstorm amplify
對干位渦的分析表明：臺風或臺風環流區為高值位渦區，臺風越強，位渦中心值越大；對流層上部或平流層下部冷空氣（高位渦）的擴散南下與暖濕氣流的交匯是造成特大暴雨的重要原因，因為上游斜壓性的發展使對流層頂發生折疊，平流層與對流層相互作用增強，上下位渦區相接的形勢使低層渦旋發展，上升運動加強，位渦的下傳有效地降低了靜力穩定度，有利於位勢不穩定能量的釋放，使得暴雨增幅。 -
Wearing my rain boots, i continued my journey on motorbike to the most serious disaster area - tingnei. in the lowlands of this area, all one story houses were submerged by water when typhoon xangsane struck formosa last year. this year, typhoon nari pushed the water level above the second story of many houses
穿著長統雨鞋，我繼續騎著摩托車行往嚴重災區碇內，此地較低?的地區，在去年象神臺風來襲時曾水淹至一整層樓高，而今年在納莉臺風的肆虐下，更是水滅二層樓高，已達三樓處。 -
In 2000, typhoon bilis weakened into a low - pressure area over southeastern china after landing
在2000年，臺風碧利絲在中國東南部登陸后，減弱為一低壓區。 -
Myungji - dong village, busan city and gadeokdo island on saturday, september 20, fellow initiates from many korean centers visited the myungji - dong village area of busan city. since myungji - dong village is near the sea, many of its houses and fields were flooded by typhoon maemi
來自許多小中心的同修於9月20日一起探訪釜山市的鳴旨洞，由於該地靠海，許多房屋田園都淹沒了，盡管風沙彌漫，同修們仍然很細心地協助清理道路和田地。 -
The numerical simulation for the pearl river networks in the area of guangzhou is calculated by ecomsed model that is based on the observed data for typhoon no. 9316 in storm surge of the flood season of 1999
摘要利用1999年洪季和9316號臺風風暴潮的實測資料，通過ecomsed數學模型對珠江河網廣州區域進行數值模擬計算。 -
On 23 june 2001, due to subsidence descending motion of the air over a rather broad area ahead of typhoon chebi, heat showers formed over inland guangdong and moved south to affect hong kong in the evening
二零零一年六月二十三日，臺風飛燕前端出現下沉現象較大范圍的空氣下降現象，導致廣東內陸地區產生熱驟雨，並在晚上南移影響香港。 -
On 23 june 2001, due to subsidence ( descending motion of the air over a rather broad area ) ahead of typhoon chebi, heat showers formed over inland guangdong and moved south to affect hong kong in the evening. these heat showers later developed into a northwest - southeast oriented squall line
二零零一年六月二十三日，臺風飛燕前端出現下沉現象（較大范圍的空氣下降現象） ，導致廣東內陸地區產生熱驟雨，並在晚上南移影響香港。這些熱驟雨後來更發展成颮線，從西北延向東南。
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