風向常變的 的英文怎麼說
中文拼音 [fēngxiàngchángbiànde]
風向常變的
英文
choppy-
It was not often that she could turn her eyes on mr. darcy himself ; but, whenever she did catch a glimpse, she saw an expression of general complaisance, and in all that he said she heard an accent so far removed from hauteur or disdain of his companions, as convinced her that the improvement of manners which she had yesterday witnessed, however temporary its existence might prove, had at least outlived one day
她雖然不能常常向達西先生顧盼,可是她只消隨時瞥他一眼,就看見他臉上總是那麼親切,她聽他談吐之間既沒有絲毫的高傲習氣,也沒有半點蔑視她親戚的意味,於是她心裏不由得想道:昨天親眼看到他作風大有改進,那即使是一時的改變,至少也保持到了今天。It is found that the anomalous sea ice area over the southwest part of the sea of okhotsk, together with the associated northern pacific sst anomaly, can exert crucial influence on the variability in the vigor and nw - se extension ( contraction ) of the pacific storm track, while the sea ice area anomalies over the area of northeastern part of the sea of okhotsk and the gulf of shelikhow, together with its associated north pacific ssta, mainly impact the strength and south - north movement of the storm track
結果發現:冬季鄂霍次克海西南部海區海冰面積異常與北大平洋海溫異常共同作用對北大平洋風暴軸在西北東南方向的伸縮及強度的年際變化有重要影響;鄂霍次克海東北部及舍列霍夫海海區海冰面積異常與海溫異常的共同作用主要影響風暴軸的南北位移和強弱。If a decadal positive temperature anomaly occurs in the eastern tropical pacific, the atmospheric response excites a anticyclonic wind stress anomaly in the east of australia, which will lead to generate a negative temperature anomaly in the western tropical south pacific
當熱帶東太平洋的海溫為暖異常,它將激發澳大利亞的東部沿岸的大氣產生反氣旋性風應力異常,在這種風場的作用,下方海水向四周輻散,導致熱帶西南太平洋的溫躍層變淺,產生負的溫度異常。She is as in a field a silken tent at midday when the sunny summer breeze has dried the dew and all its ropes relent, so that in guys it gently sways at ease, and its supporting central cedar pole, that is its pinnacle to heavenward and signifies the sureness of the soul, seems to owe naught to any single cord, but strictly held by none, is loosely bound by countless silken ties of love and thought to everything on earth the compass round, and only by one ' s going slightly taut in the capriciousness of summer air is of the slightest bondage made aware
她如田野中的一頂絲綢帳篷在夏日的中午,微風吹乾了她上面的露珠也吹柔了懸掛的細繩她悠然自得地擺動支撐她的雪松樹干透過她的頂端直上雲霄見證了她靈魂的存在看上去,她不被任何單一的繩索束縛只被無數愛和思想的絲繩牽動沿著指南針方向,聯系萬物在夏日變換無常的微風中只有受到些微的阻礙時她才意識到一絲的牽伴。As a result, we find that in winter when the kuroshio is cooler than the normal, at following summer, the continental cyclone deepen and the east asia monsoon strengthen, that the mid - latitude blocking high weaken and zonal circulation develop, the east asia teleconnection of " - + - " is stired up, so that subtropical high weaken and diminish, and tend to east north, tropical monsoon trough strengthen and mei - yu front weaken, and tend to north, meanwhile south asia high weaken and diminish, and tend to eastvnorth, is easy to form eastern region type
結果發現當黑潮海溫冷異常時,後期夏季大陸熱低壓加深,東亞夏季風偏強。中緯度阻塞高壓減弱,東亞地區緯向環流發展,在東亞-西太平洋地區激發「 - + - 」的東亞遙相關型,從而西太平洋副高強度偏弱,面積偏小,位置偏東、偏北,東亞梅雨鋒也偏弱,季風槽則變強,位置偏北。同時南亞高壓偏弱,位置偏北、偏東,易形成東部型。The well correlation times persist for about six months and the incidence level is reach or pass 0. 01. the meridional wind field which persistly impacting on sst in kuroshio region is near the west tropical pacafic. the result also behave as distinctly positive correlativity. afterwards we investigate the relationship between sst in kuroshio region and ninoc, 4 region and integrate the front conclusion. as a resultjt display that the sst in kuroshio region persists for positive relevance during the course of el - nino and inversely during the course of la - nina. subsequentl y the synthetic fields of kuroshio region ' s ssta in el - nino and la - nina years have proved the front outcome
對與黑潮海溫異常變化關系密切的風場關鍵區及兩者的相互關系研究表明:黑潮本身的風場和其源地北赤道流海域的風場異常對黑潮海溫的影響僅限於同期及海溫滯后1到2個月,而能持續影響黑潮海溫異常的經向風場的關鍵區出現在赤道西太平洋( 140 - 160e , 5s - 5n ) ,緯向的關鍵區則在赤道中太平洋( 160e - 150w , 5s - 5n ) ,且緯向關鍵區的強度和范圍均大於經向,兩者對黑潮海溫的影響均能持續六個月左右。Apart from direct strokes, people can also get hurt by electric shock when using or in contact with conductors or electrical appliances which come under the influence of these strokes. squalls or violent gusts often occur with thunderstorms
除直接電殛外,接觸受雷電影響的導體或電器,亦會因電震而受傷。雷暴中常出現狂風或猛烈陣風,風速驟然增強或風向突然改變。By using ncep / ncar reanalysis data of height and wind, the inter - monthly lpac map, the climate lapc map, inter - annual anomaly map and mean variance map of monthly wind field of 850 and 500hpa and monthly height field of 850, 500, 150, 30hpa are calculated in a globe - belt area, which situates between 30 s and 75 n, from december 1957 to december 1997, according them we analysis the rule of the season transfer and anomaly of nh mean circulation. the results show that the climate map of lapc can describe the seasonal transfer process of large scale circulation better. the advance process of summer circulation establish is form south to north at the middle and lower level of the troposphere, that is reflected primly in the inter - monthly wind and pressure map of lapc ; at lower lever of stratosphere, the establish process is simulate to that of troposphere, and reflect of process of that the south asia high toward plateau ; at middle stratosphere the summer circulation establish begins at middle and high latitude initially, and then transmits to low latitude gradually, while the seasonal variability in mid - stratosphere is stronger than it in troposphere and low - stratosphere
利用ncep ncar再分析高度場和風場資料,計算了30 s 75 n球帶區域1957年12月至1997年12月逐月850 、 500hpa風場及850 、 500 、 150 、 30hpa高度場月際局地型相似系數圖、多年平均圖(即氣候lpac圖) 、年際異常圖及均方差圖,在此基礎上,分析了北半球平均環流季節轉換及其異常的規律。分析表明,氣候局地型相似系數圖較好地給出了大尺度環流季節轉換發生的過程:在對流層中、下部,風、壓場月際局地型相似系數圖清楚地反映了夏季型環流建立由南向北的推進過程;低平流層夏季型環流的建立與對流層接近,其中,南亞高壓上高原過程有明顯反映:中平流層,夏季型環流的建立明顯表現為從中、高緯度開始,逐步向低緯傳播的特徵,且變化較對流層和低平流層明顯。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。Upon above advantage, we can realise that the airboat is very suitalbe for every advertising company and enterprises, low cost, high efficiency, it brings the commercial advertising from the groung to the sky, from the static to moving, from silence to soundable, the shape of streamline is adopted to have very good ability of anti winding, stable flying and agility, it can take off vertically, forwarding or backwarding, presenting a fully new carrier to advertising circles, becoming a focus of people in the world
綜合以上的優點不難看出,遙控飛艇非常的適用於各廣告公司,各種企業購買使用,成本低,見效快,它將商業廣告從地面發展到空中,由靜態變為動態,由無聲變有聲,遙控飛艇採用流線外型,氣動性能好,抗風能力強,飛行平穩,機動靈活,可垂直起落,俯沖爬升,前進後退,空中懸停,拋撒資料,施放彩色煙霧,空中攝影攝像等,向廣告界展示了一個新穎的廣告載體。But these processes have also brought risks, most notably in the volatility of large capital flows, to the extent that many small and open economies have found it difficult to cope, even though their macroeconomic policies may have been largely free of mistakes
但這個過程亦同時帶來風險,尤其是當規模大而且變化無常的資金流向出現時,許多小規模的開放型經濟體系,即使向來在宏觀經濟政策上沒有重大失誤,也覺得難以招架。( 4 ) in summer, tropic west pacific ssta decadal change infect precipitation decadal change in south and north of changjiang river maybe by : positive ssta in tropic west pacific weaken the summer monsoon circulation, lead more precipitation in south of changjiang river and less precipitation in north of it, vice versa ; middle north pacific ssta decadal change infect precipitation decadal change in mid - down valley of changjiang river maybe by : when ssta is negative in middle north pacific, the height field in tropic rises obviously, the subtropical high strengthens and extends westward, the northern limit retreats southward, leads upper trough retreats northward and move eastward, meiyu front moves northward, then leads more precipitation in mid - down valley of changjiang river, vice versa ; middle northwest pacific - low latitude mid - east pacific infects precipitation in north china possibly by change the activity of northeast china cyclone
( 4 )熱帶西太平洋ssta年代際變化影響夏季中國長江南北降水年代際變化的可能機制是熱帶西太平洋海表溫度正(負)異常減弱(加強)東亞夏季風環流,從而使江南降水增加(減少) ,江北降水減少(增加) ;夏季中部北太平洋ssta年代際變化影響中國長江中下游地區夏季降水年代際變化的可能機制是中部北太平洋海表溫度負異常,將導致熱帶地區高度場普遍增高,副高加強西伸,副高北界南退,致使高空槽北縮東移,梅雨鋒西移北進,中國長江游中游、中卜游降水增多,反之亦反;夏季中高緯西北太平洋一低緯中東太平洋反向距平分佈結構影響中國東北降水的可能機制是低緯中東太平洋海表溫為負異常。It is showed that the heat transport crossing the equator has the similar magnitude and the same period of one year, compared with that of 10 n in arabian sea. by contrast, the heat transport across 10 n in bay of bengal has a much smaller value with a prominent semiannual period ; there are tight relationship between integrated zonal wind stress in one latitude of the indian ocean north of 7 n and the total heat transport across that latitude, as well as the total net surface heat flux north of that latitude. the maximum correlation coefficient is less than - 0. 5
結果表明越赤道和越10on阿拉伯海的熱輸送量大小具有可比性,且有相同的年循環特徵,而10on孟加拉灣緯度的經向熱輸送較小,且具有半年變化周期;儼s以北印度洋任一緯度上的緯向風應力異常與此緯度上的經向熱輸送異常以及此緯度以北印度洋總的海面凈熱通量異常有很好的相關關系,相關系數最大可達一0 . 5以上。With the wind, pressure and sea surface temperature ( sst ) data provided by ncep / ncar reanalysis project and excess length of day ( lod ) data provided by international earth rotation service ( iers ), atmospheric angular momentum ( aam ) and its horizontal and vertical transportation are computed and analyzed, which are in accordance with maintenance of the zonal circulation. and the anomalous aam is highly consistent with el nino events
應用ncep / ncar40年再分析計劃提供的風場、氣壓場、海溫等資料以及國際地球自轉服務局( iers )提供的日長變化資料,計算大氣角動量及其水平、垂直輸送,分析其氣候及異常特徵,發現角動量及其輸送與緯向環流的維持相一致,角動量異常與厄爾尼諾事件緊密相關。When confronted the conflict between the constancy of human nature and the drastically changing reality which is brought forth by the transference of china from the feudal civilization to industrial civilization and the gradual erosion of chinese culture by western culture, jinpai writers turn to seek sustenance in common people and look for a cozy cottage for the shelter of humanity
摘要面對農耕文明向工業文明的讓渡遷移、西方文化對中國文化的點滴侵蝕及西風東漸所引發的「人性之常」與「現實之變」的矛盾, 「京派」諸賢「禮失而求諸野」地在鄉土社會中尋找寄?美好人性的小屋,並形成了在所求之野的鄉土社會背景上對民族文化深層結構中的人性之常、人性之美進行尋租模式的輓歌式創作。Said catherine, leaning back, and returning his look with a suddenly clouded brow : her humour was a mere vane for constantly varying caprices. you and edgar have broken my heart, heathcliff
凱瑟琳說,向後仰著,以突然陰沉下來的臉色回答他的凝視:她的性子不過是她那時常變動的精神狀態的風信標而已。Strong gusts manifest themselves as abrupt increases in wind speed or drastic changes in wind direction
強勁的陣風見于風速驟然增強或風向突然改變,通常在大驟雨、雷暴及Strong gusts manifest themselves as abrupt increases in wind speed or drastic changes in wind direction. they often occur in heavy showers ; thunderstorms and strong monsoon situations. they originate mainly from rapid and irregular motion of air currents technically known as turbulence
強勁的陣風見于風速驟然增強或風向突然改變,通常在大驟雨、雷暴及?烈季候風的情況下出現,它主要是由快速不規則的氣流(學名為湍流)所引起的。Strong gusts manifest themselves as abrupt increases in wind speed or drastic changes in wind direction. they often occur in heavy showers ; thunderstorms and strong monsoon situations. they originate mainly from rapid and irregular motion of air currents ( technically known as turbulence )
強勁的陣風見于風速驟然增強或風向突然改變,通常在大驟雨、雷暴及?烈季候風的情況下出現,它主要是由快速不規則的氣流(學名為湍流)所引起的。Indeed, the instabilities produced by volatile capital flows have been the main cause of the financial turmoil in our region during the past two years
事實上,這些變幻無常的資金流向所引起的不穩定情況,正是過去兩年亞洲發生金融風暴的主要原因。分享友人