西北強風 的英文怎麼說
中文拼音 [xīběiqiángfēng]
西北強風
英文
nor'wester-
Globigerina bulloides, which was regarded as the mark species for the sw monsoon prevailing in the arab sea, while in this area, it ' s more likely to be a mark species for the strong ne monsoon
在阿拉伯海被認為是西南季風盛行的上升流標志種globigerinabulloides在本區更可能是東北季風增強、西南季風減弱的標志種。Tracking west - northwestwards, songda intensified into a typhoon on 31 august and crossed the mariana islands the next day. it traversed okinawa on 5 september
它向西北偏西移動，在八月三十一日增強成為一個臺風，翌日橫過馬里安納群島。Along the rh ? ne valley, occasional strong, cold, dry, north - to - northwesterly wind known as the mistral
羅訥山谷沿線偶爾會出現從北部吹響西北的乾冷的強風。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。Moving westwards, it intensified into a tropical storm and tracked north - northwestwards the following day
次日它增強為一熱帶風暴后，向西北偏北推進。Moving westwards, tokage intensified into a typhoon on 14 october. it then took on a northwestward course
它於十月十四日增強為一個臺風，並採取西北路徑推進。In the global warming period of 1968 - 2002, the locations of landfalling typhoons in china mostly situated in the middle of the east coastal area of china and the position whereat northwestern pacific typhoons reached their maximum strength had a trend to move northwards during its life
在1968 - 2002年全球明顯增暖時段，我國臺風登陸位置偏向我國中部，西北太平洋臺風在生命史中強度達最強時的位置有向北移動的趨勢。The variation in the early aao beget the rainband latitudinal discrepance of the china summer monsoon by means of impacting on the intensity and position of northwest pacific subtropical high in the late summer
前期aao偏強時，後期6 ? 7月長江流域降水將增加，反之亦然。前期aao的變化通過影響後期夏季西北太平洋副高的強度和位置，引起中國夏季風雨帶位置的南北偏差。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。The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows, so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening, one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea. furthermore, with the effect of terrain, the southern shaanxi province became the center of this extremely heavy rain process
中尺度結構分析表明，本次暴雨具有明顯的中尺度特徵，是由三支氣流共同作用的結果，分析發現（ 1 ）地面東南風和地形在這次大暴雨過程起主要作用； （ 2 ）東路冷空氣主要是通過中低層侵入陜南地區的，並與地面冷式錮囚鋒的形成密不可分； （ 3 ）夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因，一個是由於地形山谷風的作用，另一個是降水的潛熱釋放激發了上升運動: （ 4 ）位勢不穩定層結的形成與低層暖濕平流的發展有很好的對應關系; （ 5 ）本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地區東部，為暴雨的發生提供了必要熱力條件。China is a country with rich wind resources for it locates in the south - east of asia and neighbors west of the pacific ocean. seasonal wind is powerful. especially the north - east, north - west as well as coastal areas have large wind resources
我國位於亞洲大陸東南、瀕臨太平洋西岸，季風強盛，是風資源豐富的國家，尤其是東北、西北和沿海地區風能儲量較大。Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature
其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同，強冬季風使得黑潮與我國近海海洋過多散熱，海溫降低；在西北太平洋暖池北部，強冬季風引起西風異常，從而引發異常氣旋性環流，海水輻合下沉加熱其表層以下海水，同時異常環流使得更多東側異常暖水向西加熱其表層水；在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常，海水輻合下沉升溫。It moved to the west - northwest and intensified into a tropical storm the same day
它向西北偏西移動，並於同日增強為一個熱帶風暴。Moving west - northwestwards, it reached typhoon strength in the early morning of 2 june
它向西北偏西移動，並於六月二日清晨增強為一臺風。Tracking towards the west - northwest, higos intensified into a tropical storm the same day
它向西北偏西移動，于同日增強為一個熱帶風暴。Tracking towards the west - northwest, haishen intensified into a tropical storm the following day
它向西北偏西移動，並於次日增強為一個熱帶風暴。As the cold front passed the airport, winds strengthened from the northwest
冷鋒掠過機場時，西北風增強。At sundown, the strong cold wind has shifted from the southeast to the northwest
日落時分，強勁的冷風由東南風轉為西北風。In the early 1600s, the manchurians took over the sovereignty of china and established the ching dynasty. with many pro - nationalist revolts occurring, the newly set - up government immediately imposed a ban on the study and practice of the martial art ; forbidding them altogether in an attempt to gain effective control and order. fire - wind sun honglei, a military official from the previous dynasty, sees this as an opportunity to make a fortune for himself by helping to implement the new law
七劍的故事敘述於1660年間，滿清雖已入關，但中原武林仍隱藏不少反抗力量，滿清親王哆格多施行禁武令，派前朝降清高手風火連城率領十二門將，剿殺各地違令武林人士而風火連城在西北邊強的最後一個目標，就是武莊。The spokesman said that last sunday evening strong northwesterly cross - winds were generally blowing across the runway at hong kong international airport
發言人表示，上星期日傍晚香港國際機場跑道正颳起強烈西北側風。分享友人