溫帶風暴 的英文怎麼說
中文拼音 [wēndàifēngbào]
溫帶風暴
英文
extratropical storm- 溫 : Ⅰ形容詞(不冷不熱) warm; lukewarm; hot; gentle; mild Ⅱ名詞1 (溫度) temperature 2 (瘟) acute ...
- 風 : Ⅰ名詞1 (空氣流動) wind 2 (風氣; 風俗) practice; atmosphere; custom 3 (景象) scene; view 4 ...
- 暴 : Ⅰ形容詞1 (突然而且猛烈) sudden and violent 2 (兇狠; 殘酷) harsh and tyrannical; cruel; fierce...
- 溫帶 : temperate zone
- 風暴 : storm; windstorm; tempest
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Nock - ten weakened into a severe tropical storm that night and became an extratropical cyclone the next morning
洛坦于當晚減弱為一強烈熱帶風暴,翌日早上變成一溫帶氣旋。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) 。On the morning of 21 may, it weakened into a severe tropical storm and became an extratropical cyclone the same day. on 6 june,
到了五月二十一日早上,海貝思減弱為一個強烈熱帶風暴,並在同日變為一個溫帶氣旋。The fifth is the observation in reality of a predicted link between increased sea - surface temperatures and the frequency of the most intense categories of hurricane, typhoon and tropical storm
第五,觀察資料顯示:海洋表面溫度的持續上升和最高級別颶風、臺風以及熱帶風暴的發生頻率之間存在著可預測關系。Chaba weakened into a severe tropical storm over the sea of japan on the morning of 31 august and became an extratropical cyclone over hokkaido that afternoon
暹芭於八月三十一日早上在日本海減弱為一強烈熱帶風暴,當天下午在北海道變成溫帶氣旋。Theresearchers also examined whether the recovery was sufficient to makethe protected areas more resilient to storms and changes intemperature, but the results were not statistically significant
研究人員也檢驗了魚群數量的恢復是否足以令保護區更有效地抵禦暴風雨的侵襲和溫度變化帶來的影響,但檢驗結果未達到統計上的顯著水平。Songda weakened into a severe tropical storm over the sea of japan on the early morning of 8 september and skirted the southwestern coast of hokkaido before becoming an extratropical cyclone
桑達於九月八日清晨在日本海減弱為強烈熱帶風暴,在擦過北海道西南沿岸后,變成溫帶氣旋。China is one of the countries which are harmed by storm surge both tropical and temperate cyclones, the disaster of storm surge can occure every seasons and from south to north in china ' s coastal area. based on the analysis of the features of temporal and spatial changes of storm surge disaster in the recent 50 years, this paper focuses on the frequency changes of historical records in recent 500 years and measured data in recent 50 years of storm surge disaster and the relationships between storm frequency change and climate fluctuation. meanwhlie, the effects of future increase in the frequency of tropical cyclones landing or affecting china and relative sea level rise with global warming on storm surge disaster of china ' s coastal area also discussed. the results show that, in recent 500 years, there are direct relationships between storm frequency change and climate fluctuation, i. e., high global mean temperature correspond with high storm frequency and low mean temperature correspond with low storm frequency. storm surge disaster in china ' s coastal area will be exacerbated with global warming
中國是全球少數幾個同時受臺風風暴潮和溫帶風暴潮危害的國家之一,風暴潮災一年四季,從南到北均可發生.本文基於中國沿海近50年風暴潮災時間變化和空間分佈特點的分析,著重探討了近500年全國及長江、黃河、珠江三角洲的歷史記錄和近50年實測風暴潮災發生頻次的變化及其與氣候波動的關系,並對未來全球變化背景下,中國沿海風暴潮災的變化趨向進行了討論.結果表明:近500年來,中國沿海的風暴潮災在氣溫較高的偏暖時段比氣溫較低的偏冷時段明顯增多.近50年實測臺風暴潮災的變化也是如此,而溫帶風暴湖的變化則與此相反.未來全球變化引起的登陸影響中國的熱帶氣旋頻次增加和相對海平面的上升,均將導致風暴潮災呈加重的趨向Wildfires driven by winds and high temperatures burned out of control saturday in the san bernardino mountains, triggering firestorms that destroyed more than 200 homes in foothill suburbs and forced the evacuation of thousands of residents from san bernardino to rancho cucamonga
在強風和高溫的推動下,周六發生在聖貝納迪諾縣大山的瘋狂大火目前已經變得無法控制,大規模風暴性大火已經摧毀了郊區山腳一帶200多戶家園,當地上千居民被迫從聖貝納迪諾緊急撤離到蘭喬?庫卡蒙加It made landfall in the same evening about 100 km south of wenzhou. sinlaku weakened into a severe tropical storm after making landfall and became an area of low pressure over jiangxi province on 8 september
它在九月七日加速趨向浙江省,同日傍晚在溫州以南約100公里處登陸。森垃克在登陸后迅速減弱為一個強烈熱帶風暴,于次日在江西省減弱為一個低壓區。A severe rainstorm over liaoning occurring from august 19th to 21st in 1997 by a landing northward tropical cyclone ( 9711 ) was simulated by mm5 non - hydrostatic model. through comparing the simulate results with the real weather, the different layer synoptic - scale circulation, height field, temperature field and precipitation were successfully reappeared. the main synoptic background in the case was as follow
使用psu ncarmm5v3非靜力模式,對1997年登陸北上的11號臺風, 8月20日夜間在遼寧登陸前後,給遼寧帶來的大范圍大暴雨進行了數值模擬,並通過模擬的高、中、低空形勢場(高度場、溫度場) ,降雨量以及降雨強度與實況進行對比分析,是一次比較成功模擬,基本再現了遼寧大暴雨過程物理量場變化的全貌。Sudal further weakened into a tropical storm on 16 april and became an extratropical cyclone the same day
蘇特在四月十六日進一步減弱為一個熱帶風暴,同日變為一個溫帶氣旋。In the next four days, phanfone kept moving northwestwards over the pacific. on 18 august, phanfone turned abruptly to the northeast. it weakened into a severe tropical storm on 20 august and became an extratropical cyclone the same night
它于隨后四天繼續在太平洋上向西北推進,在八月十八日突然轉向東北,在八月二十日減弱為一個強烈熱帶風暴,同日晚上轉變為一個溫帶氣旋。On 10 july, it weakened into a severe tropical storm and skirted to the south of tokyo. chataan then moved along the east coast of japan and became an extratropical cyclone on 11 july
七月十日,它減弱為一個強烈熱帶風暴,並在東京以南掠過,隨后沿著日本東岸移動,在七月十一日變成一個溫帶氣旋。On 20 august, megi weakened into a severe tropical storm and crossed the northern coast of honshu, japan. it became an extratropical cyclone that afternoon
?魚在八月二十日減弱為一強烈熱帶風暴,並橫過日本本州北岸,同日下午變成溫帶氣旋。The seed for hurricane formation is a cluster of thunderstorms over warm tropical waters
颶風形成的原因是由於雷暴聚集在溫暖的熱帶水面之上。In history, storm surges associated with a typhoon in 1937 and typhoon wanda in 1962 caused severe flooding to widespread areas in the new territories
歷史上,一九三七年的一個臺風及一九六二年的臺風溫黛所引發的風暴潮都曾經為新界廣泛地區帶來嚴重水浸。Traversing the seas between honshu and ogasawara islands, kirogi weakened into a tropical storm in the early morning of 19 october and became an extratropical cyclone later that day
它於十月十九日清晨在本州和小笠原群島之間的海面減弱為熱帶風暴,隨后變成溫帶氣旋。After passing just to the east of iwo jima and ogasawara islands, tingting began to track northeastwards on 1 july. it weakened into a severe tropical storm early next morning, and became an extratropical cyclone over the pacific on 4 july
婷婷于硫磺島及小笠原群島以東附近掠過后,在七月一日開始轉向東北移動,翌日清晨減弱為一強烈熱帶風暴,七月四日在太平洋上變成一個溫帶氣旋。On 7 august, meranti weakened into a severe tropical storm as it turned northward. it eventually became an extratropical cyclone on 9 august. on 8 august,
莫蘭蒂於八月七日減弱為一強烈熱帶風暴並轉向北移動,最終在八月九日變成溫帶氣旋。分享友人