middle stratosphere 中文意思是什麼

middle stratosphere 解釋
平流層中層
  • middle : n 1 中央，正中；中間，中部；中途。2 人體的中部，腰部。3 中間物，媒介物；中人，中間人，調解人；中...
  • stratosphere : n. 1. 【氣象學】平流層，同溫層。2. 最上層，最高欄，最高部位。3. 艱深的學科領域。
  1. 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。
  2. The correlation between the transition dates in middle stratosphere and the ozone quantity in stratosphere. the correlation between the zonal wind of 10hpa and 70hpa and the transition dates of these two layers is remarkable

    中平流層環流轉型異常與赤道平流層緯向風準兩年振蕩（ qbo ）及平流層臭氧總量異常存在顯著相關聯系。
  3. When the zonal wind of 10hpa is apheliotes ( zephyrus ) and that of 70hpa is zephyrus ( apheliotes ), the transition delays ( advances ). the correlation between the ozone quantity and the transition dates in middle stratosphere is opposite. when the ozone quantity is excessive ( lack ), the transition advances ( delays )

    分析發現10hpa及70hpa層的熱帶緯向風與相應層環流轉型日期之間的相關顯著， 10hpa熱帶東（西）風位相、 70hpa西（東）風位相時環流轉型滯后（提早） 。
  4. 3. the relation between the transition dates in middle stratosphere and the important systems in troposphere such as polar vortex and the subtropical high in west pacific

    臭氧總量異常與中平流層轉型日期異常之間為反相關關系，臭氧總量偏高（低） ，流型轉型日期偏早（晚） 。
  5. The average values of the transition dates in middle stratosphere and their variations with height. the climatic variability and the interannual and interdecadal variation rule of the transition dates

    中平流層環流轉型日期的多年平均值及其隨高度的變化，各層轉型日期的氣候變率及異常存在年代際、年際變化規律。
  6. 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。
  7. 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。
  8. The transition from negative to positive of the spherical function coefficient a20 reflects it impersonally and quantificationally. with ncep / ncar day - to - day height field analysis data, the coefficient of spherical function a02 is calculated. the transition dates of circulation type in middle stratosphere are determinated based on the dates that a02 have transited from negative to positive steadily

    本文用ncep ncar北半球1958 1997年中平流層五層（ 10 、 20 、 30 、 50和70hpa ）逐日高度場再分析資料，計算出其球函數系數a _ 2 ~ 0 ，並據a _ 2 ~ 0穩定地由負轉正的日期確定了逐年中平流層各層環流轉型的日期，在此基礎上著重分析了春季中平流層環流轉型日期的氣候及異常規律及它們與平流層環流異常及與對流層環流的關系。
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