北西偏西 的英文怎麼說

中文拼音 [běixīpiānxī]
北西偏西 英文
northwest by west
  • 西 : west
  • 偏 : Ⅰ形容詞1 （不正; 歪斜） inclined to one side; slanting; leaning 2 （只側重一面） partial; prejudi...
  1. Tracking generally towards the west - southwest, it intensified into a typhoon over the seas to the north of mariana islands on 14 july

    它大致向西南偏西移動，並於七月十四日在馬里安納群島以北海域增強成為一個臺風。
  2. 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。
  3. Poc in the dongjiang river was influenced mainly by c4 plant such as grass and crops, and poc 6 13c value was heavier than that in the xijiang and beijiang rivers

    在珠江流域中，東江水體poc受c _ 4植物草類以及作物的影響明顯， ~ （ 13 ） c值比西江、北江偏重。
  4. Dean is about 175 miles south of santo domingo in the dominican republic, moving to the west - northwest at about 17 miles an hour

    迪恩位於多米尼亞共和國聖多明各以南175公里，現正以時速17公里/小時向西北偏西方移動。
  5. In drought ( flood ) years over the yangtze river basin, the southerly moisture transport with the summer monsoon can shift to northern ( southern ) than the normal, the southeasterly water vapor from south

    雨季建立之前和雨季結束之後，華北和東北地區西邊界的偏西風水汽輸入占絕對優勢;雨季中南邊界的偏南風水汽輸送對華北最為重要，東北地區雨季期間南邊界的水汽輸入和與來自西邊界的水汽輸入貢獻相當。
  6. Both composite and correlation analyses show that the 150hpa asia - australia cef ( aacef ) in boreal spring has important influences on easm. when aacef is weaker, the summer wpsh tends to be stronger with a southwestward extension, and the south asia high ( sah ) will be stronger too. this circulation pattern will lead to more rainfall in the yangtze and huaihe river valley and less rainfall outside of this region

    相關分析和合成分析的結果還顯示，春季150hpa亞澳越赤道氣流對東亞夏季風有重要影響：當春季該氣流偏弱時，北半球夏季西太平洋副高強度偏強，位置偏南偏西，南亞高壓強度也偏強，這樣的環流背景使江淮流域6 ? 7月降水偏多，華南華北降水偏少；反之，當春季該氣流偏強時，夏季西太副高強度偏弱，位置偏北偏東，南亞高壓強度也偏弱，江淮流域夏季降水偏少，華南華北降水偏多。
  7. The results indicate : ( 1 ) the distribution of magmatic rocks shows the feature that in the middle and western part of the study area basic igneous rocks dominate, and in the middle - eastern part intermediate rocks are predominant, while in the southeastern part acid ones are developed. ( 2 ) in the area west to the shiwandashan basin, intermediate magmatites were controlled by deep ne - striking and nw - striking faults, especially at the conjunction site of these two group faults, magmatic activity was strong ; and its tectonic background can be attributed to extensional continental rift

    其中，在十萬大山盆地以西地區的偏基性巖漿活動受北東和北西向深斷裂控制明顯，尤其以此兩組斷裂交匯處的巖漿活動強烈，盆地構造背景屬大陸伸展裂谷環境；在十萬大山盆地以東地區為偏酸性巖漿活動，主要受東吳運動形成的欽防造山帶的控制，屬大陸邊緣造山帶或島弧造山帶環境。
  8. Spatial distribution and time scales of atmospheric diffusion over beijing area are revealed by means of a random walk simulation model and practical meteorological data with a specified emission source from the city. results show a southward transport pattern for wintertime while a northwest transport of pollutants in summer. the area is the least evidently influenced by the emission source in spring, while the largest in autumn. the time spent for instantly emitted material removing from the model domain varies from winter - spring to summer - autumn. the former was shorter one of less than 20 hours ; the latter was longer one of approximately 30 hours. distribution of occurrence probability for different removal times was not symmetry. reducing slowly at the end of longer removal time, probability exists for pollutants remaining in this area a long time

    結果表明，冬季示蹤物偏南夏季偏西北的輸送明顯春季擴散影響范圍最小秋季最大。示蹤物從200km200km模式區域輸出的平均時間去除時間明顯分為冬春季和夏秋季兩組，前者較小，平均在20h以下，後者較大，平均約30h 。不同去除時間出現的頻率分佈是非對稱的，在長去除時間一側，出現頻率下降緩慢，顯示污染物有在該區域內長時間滯留的可能。
  9. Situated in the north and facing the south with a little to the west, the temple was built with a mixed structure of sheer wall with girder system. a typical hanging over bracket set structure of southern china

    建築座北朝南略偏西，構造形式為承重墻加柱樑系統的混合構造，柱樑系統為南方特有的疊斗式，承重墻則為磚造再予以粉刷。
  10. The best places to observe the " parade of the five planets " will be on high grounds with unobstructed views to the west - northwest

    觀看這次五星匯聚的最佳地點是面向西北偏西方向無障礙物阻擋視線的高地。
  11. The azimuth from the launch point to the target was about 346 deg., or 15 deg. west of due north

    有關消息來源稱，發射點至目標的方位角約346度，或者說北偏西15度。
  12. Abstract : monthly rainfall data from 1951 to 1995 for june, july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months. serious flood mainly happened in july and august, and sevious drought mainly happened in august. there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china. meanwhile, the deeper trough which covered the regions from the ural mts. to the balkhash lake play an important role in serious rainstom in rainy season in the north china. there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ), and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage

    文摘:利用華北平原地區的13個站點， 45年（ 1951 1995 ）的降水資料，對夏季4個時段（ 6月、 7月、 8月、 6 8月）進行了z指數計算，確定了該地區各個時段的嚴重澇年和嚴重旱年.發現華北地區雨季的嚴重洪澇主要集中在7 ， 8月，嚴重乾旱則主要發生在8月，並可明顯看出由50 60年代的多水期向70年代中期以後的少水期的轉變，另外，烏拉爾山到巴爾喀什湖附近的低壓槽加深和西北太平洋副熱帶高壓的北抬，對華北地區雨季持續性暴雨的產生起著決定性的作用.嚴重洪澇年的夏季（ 6 8月） ，西北太平洋副熱帶高壓偏西、偏北，赤道東太平洋海溫多處于下降階段;嚴重乾旱年西北太平洋副高偏東、偏南，赤道東太平洋海溫則處于上升階段
  13. 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。
  14. In the west - northwest, elevation around 15 degrees set of saturn

    在西北偏西方向，仰角約15度
  15. Vicente turned west - northwestwards in the afternoon on the following day

    它于翌日下午轉向西北偏西推進。
  16. 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。
  17. 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。
  18. 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。
  19. 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。
  20. Vicente turned west - northwestwards on 17 september and made landfall over vietnam the following day

    它於九月十七日轉向西北偏西推進，次日在越南登陸。
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