風暴降雨 的英文怎麼說
中文拼音 [fēngbàojiàngyǔ]
風暴降雨
英文
storm rainfall- 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...
- 降 : 降動詞1. (投降) surrender; capitulate 2. (降伏) subdue; vanquish; tame
- 雨 : 雨名詞(從雲層中降向地面的水) rain
- 風暴 : storm; windstorm; tempest
- 降雨 : rainfall降雨持續時間 time of the duration of rainfall; 降雨歷時 rainfall duration; 降雨時數 rainf...
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In this paper, four cases of heavy rainfalls and snowfalls in china are simulated by using mm5. cloud microphysical characteristics and sources of rain, snow and graupel have been particularly studied
運用中尺度非靜力數值模式mm5v3 ,對我國華南前汛期暴雨、梅雨鋒暴雨、北京東風迴流降雪和遼寧寒潮大風雪等四次過程分別進行了模擬研究。Aircrafts fly above and beside the storm clouds and drop tiny silver iodide crystals into them, triggering rainfall.
飛機飛行於風暴雲之上及其周圍,向風暴雲中撒播碘化銀晶粉以激發降雨。But by and by, as said, this evening after sundown, the wind sitting in the west, biggish swollen clouds to be seen as the night increased and the weatherwise poring up at them and some sheet lightnings at first and after, past ten of the clock, one great stroke with a long thunder and in a brace of shakes all scamper pellmell within door for the smoking shower, the men making shelter for their straws with a clout or kerchief, womenfolk skipping off with kirtles catched up soon as the pour came
如前所述,日暮時,風起西空,夜幕降臨后,出現大朵烏雲,翻滾膨脹。喜觀天象者咸望之:惟見一道道閃電,十時許,一聲巨雷,伴以悠長轟鳴,驟雨若煙霧,眾人倉皇遁往家中。暴雨乍下,男子即以布片或手帕遮草帽,女子則撩起裙裾,跳躥而去。The storm sent the temperature down.
暴風雨襲來,氣溫隨之下降。At night the tempest increased in violence
暴風雨隨著黑夜的降臨更加猖狂起來。The analysis of the large - scale synoptic situation shows that strong precipitation is closely related to the explosion of monsoon and the intensification of cross - equatorial flow which bring a lot of vapor and meet with cold masses at the eastern of northwest district on 8th, june causing extremely heavy rainfall ; that subtropical high - level jet at 200hpa, subtropical high at 500hpa and low - level jet at 850hpa are the weather backgrounds favorable to strong precipitation ; that the pattern of eastern highs and western lows and the establishment of a low - level jet and the coupling between upper - and low - level patterns that determine that the rain occurred in the east of the northwest china ( on average, this is the rainy season for the south of china, but not for the northwest china ) ; that water vapor comes from southerly and easterly flow which converge at the eastern of northwest district with convergence mainly in lower levels and pbl ; that the high value of the whole - level apparent heat source < q1 > is near the area of large rainfall in the direction of northeasterly - southwesterly agreeable to shear line very well and the condensation latent heat releasing is main heat source with vertical advection item playing key role in q1 and q2 ; that there is a vertical secondary circulation crossing low - lever jet whose ascending branch is at the area of large rainfall ; that the construction of convection instability and conditional symmetry instability results that there is not only deep thermal instability, but also moisture influx and triggering mechanism of thermal instability causing strong torrential rain
作為對比,本文還對2002年6月24 - 25日發生在北京地區的強地形雨進行了分析,並討論陜南、北京地區兩地暴雨的異同點以及地形作用的共性和個性,為兩地暴雨預報提供有益的參考,得出了一些很有意義的結果: 1大尺度環流背景分析表明: ( 1 ) 「 02 . 6 」強降水與6月上旬越赤道氣流和季風爆發密切相關,攜帶大量水汽的偏南氣流與冷空氣於6月8日交匯在西北地區東部,導致了這次強降水的發生; ( 2 ) 200hpa的副熱帶西風急流、 500hpa副高以及850hpa的低空急流的配置非常有利於本文分析之陜西強降水的發展與維持。大尺度形勢分析表明,東高西低形勢場、低空急流的建立和高低空形勢的配置決定了這場降雨出現在西北地區東部。與暴雨區相聯系,存在一支橫越低空急流的經向垂直環流,暴雨區處于該垂直環流的上升支; ( 3 )偏南和偏東氣流水汽通道在西北地區東部交匯,水汽的輻合積聚主要在對流層低層和行星邊界層內完成; ( 4 )整層的視熱源< q _ 1 >高值區在暴雨區附近呈東北-西南向分佈,與切變線走向非常一致,降水產生的凝結潛熱釋放是強降水區大氣的主要熱源。Winds in severe ocean storms can reach speeds of more than 250 kilometers an hour, up to 50 centimeters of rain can fall
海洋上的強風暴雨能達到每小時250公里的速度,形成50厘米的降雨量。At least three others are missing. forecasters say the storm could drop another 20 inches of rain before heading northwest toward the bahamas
氣象預報顯示在轉向巴哈馬群島西北前,暴風雨還將帶來20英寸(換算成500毫米,特大暴雨了)高( )的降雨。Weather forecasters said early monday the storm was a category four hurricane, with maximum sustained winds of 240 kilometers per hour and possible rainfall of up to 50 centimeters
天氣預報周一清晨表示此次風暴強度為四級,最大持續風力達240千米每小時,降雨達50厘米。Michelle minelli, a forecaster with the national weather service in miami, said the storm was expected to get stronger as it enteredswarmerworm waters of the gulf of mexico
天氣預報說周一早上風暴就已經是一個四級颶風,最大風速每小時240公里,降雨量有可能高達50厘米。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。These are usually inversely related, i. e., high intensity storms are likely to be of short duration and low intensity storms can have a long duration
通常強度與降雨時間的長短成反比,換句話說,高強度的暴風雨很可能會持續較短的時間,而低強度的暴風雨會持續比較長的時間。During the last el nino, in 1997 and 1998, rainfall doubled in california, causing a $ 1 billion in storm damage
在最近即1997至1998年的一次厄爾尼諾中,加尼福利亞降雨加倍,暴風雨造成了10億美元的損失。While the plane did not experience the full force of the storm, the resulting rate of descent of the plane was nonetheless quite phenomenal, exceeding 2, 000 feet per minute ( see figure 11 )
飛機幸未遇上暴雨的主力,但亦以每分鐘超過2000尺(見圖11 )的速度急降!因此,切勿對這類風暴掉以輕心。The bottom image of reflectivity which provides estimation of the rain intensity depicts the hook - shaped characteristic of the storm. this is another typical signature of tornado
下圖為反射率表示估計的降雨強度圖像,顯示出該風暴出現了狀回波,這是卷風另一典型特徵。The bottom image of reflectivity ( which provides estimation of the rain intensity ) depicts the hook - shaped characteristic of the storm. this is another typical signature of tornado
下圖為反射率(表示估計的降雨強度)圖像,顯示出該風暴出現了?狀回波,這是龍卷風另一典型特徵。While it ' s always hot and humid, the southwest monsoon period from may to november see the most rain and storms
盡管那裡終年濕熱,但是降雨和風暴在5月至11月的西南季風期最為頻繁。Each year central american nations such as costa rica receive large amounts of rainfall during the wet season typical of tropical regions. however on january 11, 2005, the limon and caribbean areas along costa ricas atlantic coast experienced more than their usual levels of precipitation as the heaviest storm in forty years struck, causing severe damage and displacing many residents
不過, 2005年1月11日,哥斯大黎加的利蒙省limon及其他位於加勒比海沿岸的地區,卻遭到40年來最嚴重的暴風雨侵襲,驚人的雨勢遠超過往常的降雨量,造成非常嚴重的災害,很多民眾被迫撤離家園。Mediologist meteorologist dennis feltgen of the national hurricane center in miami said the storm will cause heavy rains and possible flooding as it moves over mountainess mountainous areas
位於邁阿密的國家颶風中心的氣象專家d . f .表示暴風將帶來強降雨,在經過山地時可能引發洪災。About 70 % of the total rainfall as heavy downpour in the summer monsoon months and 30 % in winter
夏季季風季節的暴雨占總降雨量的70 % ,冬季佔30 % 。分享友人