circulation branch 中文意思是什麼

circulation branch 解釋
環林支
  • circulation : n. 1. 循環；運行。2. 傳播；環流（量），流通（量）。3. （雜志等的）發行（額），銷數，銷路。4. 通貨，貨幣；流通證券。5. 【航空】環量，環流。
  • branch : n 1 （樹）枝〈泛指大枝或小枝；bough 特指大枝，也指連花、果折下的枝；limb 指大枝；twig 指小枝〉。2...
  1. After the surplus size of the thick liquid trough is retrieved or put, can put the branch water properly, heat, wash the pipeline which sends the thick liquid material with pump circulation again, so as not to stop up

    漿槽的剩餘漿液回收或放掉后，可適當放入清水、用蒸汽加溫，再用泵循環清洗輸送漿料的管路，以免堵塞。
  2. 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。
  3. The seasonal variation of the mean meridional circulation and the double - level structure of the hadley circulation are analyzed by the two methods. the paper also studies the zonal difference of the anomalous meridional circulation and the impacts of el nino / la nina events on the local meridional circulation anomaly. conclusions are drawn as follows : 1, the hadley circulations in both hemisphere and the position of their joint uprising branch move wholly with the heat equation, with most north in july and most south in january

    然後用簡化方法分析了氣候平均經圈環流的季節變化，論文還對hadley環流的雙層結構和異常經圈環流的緯向差異以及elnino 、 lanina事件對局地經圈環流異常的影響作了研究，結果表明： 1 ，北、南半球hadley環流圈及其共同上升支的位置隨熱赤道作整體性移動， 7月最北， 1月最南。
  4. Features : contain greece pure natural olive branch extracts, the which can moisturize deeply, uric acid which can soften the cutin. it can soften the cutin in a short time, lubricate the foot, let it soft and white. natural micro plant particle, massage the foot gently can promote the foot blood circulation, get rid of the dead skin mildly, soften the aged cocoon, wipe out the bad smells from the foot, keep foot fresh, prevent eczema, let foot be tender and smooth, skin is uneasy to take off and grow up cocoon

    特點：蘊含萃取自希臘的純天然橄欖枝精華、深層保濕的木酢液以及使角質柔軟的尿酸，可以在短時間內溶解老化角質，潤滑足部肌膚，使其柔軟、白晰；天然細微植物顆粒，輕輕按摩腳部促進腳部血液循環，溫和的祛除腳部的死皮，軟化頑固的老繭，祛除異味並能保持足部清爽，預防濕疹，使雙腳肌膚細致滑嫩，不易脫皮長繭。
  5. ( 2 ) the idea of system construction is applied to build the new circulation pattern of fruit and vegetable in beijing. this system includes three branches : sales market core system, delivering center, integrated running and morning market system ; the contents of the three system vary with the economic conditions and it is a flexible development pattern ; each branch evolves with corresponding social economic conditions, and each one is indispensable. ( 3 ) through factor assembling, theory analyzing and practical reviewing, it indicates that market organization of fruit and vegetable in beijing is in an environment full of uncertainties

    該體系模式包含三個子系統：批發市場核心系統，一體化經營和早市、直銷市場系統；三個子系統的內容隨著社會經濟環境條件的發展變化而變化，此消彼長，相互轉化，是一個柔性發展模式；三個子系統的現實存在與演變發展是同我國社會經濟發展條件相適應的客觀存在，每一系統都連接著與之相匹配的生產和消費環節，每一系統都承擔著不可或缺、亦無可替代的社會經濟功能。
  6. A transverse secondary circulation is produced by the coupling of high and low jets, while the sinking branch of the secondary circulation providing the dynamic conditions for the dry intrusion air. during the period of the heavy rain process, dry intrusion descends southward along the intense constant potential temperature lines, which promotes the lower cyclone. in addition, the pouring of upper - level dry air not only decreases ground temperature behind the front but also increases surface pressure and velocity

    由於高、低空急流耦合，在高空急流中心左側產生的下沉運動和高空急流中心右側、低空急流左側產生的上升運動在鋒面上形成一次級環流，次級環流的下沉支運動為對流層高層干空氣和高位渦的下傳提供了動力條件；進一步研究發現，干侵入沿相當位溫密集帶向南向下伸展，引起對流層低層氣旋性渦度的發展；此外，高層乾冷空氣向下注入，導致地面溫度降低、氣壓升高、風速加大、低層輻合增強、上升速度加大，從而促進了新的對流運動，引起降水增強。
  7. Climatic mean map, it is further confirmed that it s a good approach to retrieve the equatorial zonal circulation by using the ir indicate ascending branch and wv indicate descending branch channels. the definition of the index of zonal circulation with the olr and fwv are presented and the 17 years mean annual and seasonal equatorial circulation are drawn. the climatic characteristics of the equatorial zonal circulation are analyzed in detail. consequently the fore results of the other observation are corrected

    通過波耳茲曼公式換算得到的6 . 7m水汽輻射通量密度，以便於與olr比較與ncep再分析的500hpa的年氣候平均圖進行比較，分析其異同，進一步證明了用衛星觀測的紅外，水汽雙通道olr表示上升運動， fwv表示下沉運動去反演緯向垂直環流是一個極好的途徑。
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