anticyclone 中文意思是什麼

anticyclone 解釋
n. 名詞 【氣象學】反氣旋；高氣壓。

  1. The anticyclone weather situations are more favorable than the cyclonic ones.

    反氣旋天氣情況比氣旋天氣情況更有利些。
  2. In summer, the south atlantic anticyclone.

    到了夏天，南大西洋的高氣壓反氣旋. .
  3. In summer, the south atlantic anticyclone

    到了夏天，南大西洋的高氣壓反氣旋
  4. Anticyclone area of high pressure

    反氣旋或高氣壓
  5. In the northern southern hemisphere, the air around an anticyclone moves in a clockwise counterclockwise direction

    在北南半球，反氣旋附近的氣流是順時針逆時針方向運行的。
  6. When the air pressure in a region is higher than its surrounding, it is called an anticyclone or an area of high pressure

    當地區的大氣壓力比其外圍高時，便稱之為反氣旋或高氣壓。
  7. In the northern ( southern ) hemisphere, the air around an anticyclone moves in a clockwise ( counterclockwise ) direction

    在北（南）半球，反氣旋附近的氣流是順時針（逆時針）方向運行的。
  8. ( 4 ) summer rainfall anomalies in north china relates to the indian summer monsoon, the south sea monsoon, sub - tropical anticyclone, south asian anticyclone and cold air anomaly

    （ 4 ）華北地區夏季降水異常與印度西南季風、南海東南季風、副熱帶高壓、南亞高壓及冷空氣異常都密切相關。
  9. ( 4 ) there exist close relation between the floods season precipitation in northeast china and the anomalies of subtropical summer monsoon, the anomalies of cold air, sub - tropical anticyclone, polar front jet, north hemisphere general circulation anomalies in winter

    （ 4 ）東北汛期降水與西南夏季風、北方冷空氣、副熱帶高壓、極鋒急流、前期冬季環流異常密切相關。
  10. ( 2 ) another interesting phenomenon is founded that the center of south asia high in the upper level of troposphere is stabile and nearly motionless during the processes of the westward extension of western pacific subtropical high, but its eastern ridge strengthens and extends eastward remarkably because of the anticyclone moves westward over the southeast japan, which may lead to the westward extension of subtropical high in the middle level of troposphere. ( 3 ) in the low level of troposphere, the north australia cold air activity plays an important role on the westward extension of subtropical high

    （ 2 ）本文在研究副高西伸過程中指出，高層200hpa上日本東南部的高壓併入南亞高壓，導致南亞高壓脊的增強發展，對低層500hpa上副高的加強、西伸可能起到引導的作用；同時，對流層低層850hpa上孟加拉灣槽在副高西伸過程中加深，並在西伸脊點到達最西點的前4天強度達到最強，這為預報西太平洋副高的活動提供了參考。
  11. The quasi - geostrophic process was diagnosed for a case of severe cold air breakout under the blocking situation during 16 - 18 march of 1998. the attention was focused on the relationship between the surface anticyclone and 500hpa blocking high. the results indicate that the cold outbreak is associated with the adjustment of blocking situation in the ural area, i. e. the collapsing and rebuilding of the ural mountain blocking high. the temperature advections in the lower troposphere shown that the polar cold air invading from the northwest caused the ural blocking high collapsed, and a new ridge developed rapidly was due to the warm advection on the southwestern side which led to the ural blocking high rebuilt. in addition, the distribution of the vertical motion on 700hpa shown that the surface high splitting was related to the considerable upward motion located on the southeastern part of surface high

    對1998年3月中旬一次高空阻塞形勢下強冷空氣過程進行了診斷分析，著重討論強冷空氣爆發前後地面反氣旋活動與高空阻塞形勢調整的關系。研究結果表明，強冷空氣的爆發與烏拉爾地區阻塞形勢的調整阻塞高壓的崩潰和重建緊密相關。對流層下部的溫度平流分析表明，阻塞形勢的調整是由於阻塞高壓上游西北方有冷空氣侵入導致了阻塞高壓的崩潰，而上游來自西南方向的強暖流則導致高壓脊迅速發展，使阻塞高壓重新建立。
  12. Through analysis of potential vorticity in equity - entropy surface field, a relatively high potential vorticity center in cyclone top in low - troposphere have discovered, and make cyclone develop in a more deep cyclone circulation by this ; and an anticyclone circulation zone with more severe low potential vorticity in high - troposphere

    通過對等熵面的位渦分析，發現了對流層中低層的位渦場，在氣旋上方有一個相對高位渦中心，由此使得氣旋在一個比較深厚的氣旋性環流中發展；而對流層高層則是一個伴有較強位渦低值的反氣旋環流區。
  13. The weather system on july 5th 08bst depicted by the cloud - drift winds could be distinctively seen an anticyclone with divergence in the north and convergence in the south which was much helpful in rationally explaining the real weather process combined with some traditional methods

    由它所表示的2003年7月5日07 ? 08時的高空風場上，可以清楚地看到一個北邊輻散，南邊輻合的反氣旋環流，這些細節有效地幫助了常規方法，使其對天氣過程做出合理的診斷分析。
  14. From time to time, under the influence of upper air disturbances, cold air from this anticyclone plunges southward through china and brings outbursts of cold air to the south china coastal areas

    有時，在高空擾動氣流影響下，冷空氣會南下橫過中國。這些冬季季候風寒潮，最後為華南沿岸帶來一陣陣的冷空氣。
  15. When the spatial pattern is of the north - south asymmetry, in the warm north - cold south years, there is a anticyclone circulation existing over the warm pool at 850hpa, easterly at 15 n and westerly in the tropical region have been greatly strengthened, while the center of anticyclone circulation moves to the east asia at 200hpa, and the hadley circulation has been affected evidently, so the summer rainfall may be above normal in the middle and lower reaches of the yangtze river, vice versa. there are different relations to east asia atmospheric circulation and summer rainfall in china

    當ssta為南北半球反對稱分佈時，與ssta北暖南冷分佈相對應， 850hpa暖池區上空為一反氣旋偏差環流， 15 n附近東風氣流和赤道附近西風氣流增強，長江中下游地區盛行偏南風氣流； 200hpa反氣旋偏差環流中心移到東亞大陸上空；副熱帶高壓強度、西伸脊點都明顯變強、西伸； hadley環流得到發展，長江中下游（華北）地區為上升（下沉）氣流，降水明顯增多（減少） ，北冷南暖年則相反。
  16. In the southern hemisphere an anticyclone circulates counterclockwise around the high - pressure center, as contrasted to the northern hemisphere

    在南半球，反氣旋繞高壓中心反時針方向吹，與北半球情況相反。
  17. Under the combined effect of the anticyclone over china and typhoon sinlaku over the east china sea, light northerly winds prevailed in the vicinity of hong kong this morning and the atmosphere was stable

    受到中國內陸反氣旋及位於東海的臺風森垃克環流共同影響下，今早香港附近地區吹輕微偏北風，大氣穩定。
  18. The remarkable transition of circulation type from winter to summer in middle stratosphere is from cyclonic type to anticyclone type. this is also the notable characteristic which is different from the transition in low stratosphere and troposphere

    因此，在由冬到夏或由夏到冬的某個階段，該層環流流型出現由氣旋向反氣旋或由反氣旋向氣旋型環流轉變的過程。
  19. In this paper, the circulation of 20hpa transits to anticyclone type first ( at april the twenty - fourth averagely ) and then the transition transmit downwards, 54 days later it arrive to 70hpa ( at june the seventeenth averagely ). the interannual variation of transition dates in higher layers of middle stratosphere ( 10hpa 20hpa and 30hpa ) is more remarkable than in lower ones ( 50hpa and 70hpa ). the transition dates of 50hpa and 70hpa have notable interdecadal variation feature : they are sooner before 1978 and later after 1978

    多年平均20hpa環流最先轉為反氣旋型（平均在4月24日） ，然後逐漸下傳，至70hpa （平均在6月17日）歷時54天；而中平流層上部（ 10hpa 、 20hpa和30hpa ）轉型日期的年際差異較下部（ 50hpa 、 70hpa ）大； 50 、 70hpa層環流轉型日期具有明顯的年代際變化特徵， 1978年以前轉型日期偏早， 1978年以後偏晚。
  20. Low - level cyclone circulation with high - level anticyclone circulation, is helpful to form low - level convergence and high - level divergence, and make the rising airflow nearby cyclone keep and strengthen so that have offered necessity condition for convection precipitation

    低層的氣旋性環流和高層的反氣旋性環流相配合，有利於形成低層輻合，高層輻散，使得氣旋附近的上升氣流得以維持和加強，從而為對流性降水提供了必要條件。
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