blocking high中文什么意思

發(fā)音:

用"blocking high"造句

陰塞高壓
阻塞高壓

block: n. 1.片，塊，大塊；粗料，毛料；木料；石料；金屬塊； ...
high: adj. 1.高的〔指物，形容人的身高用 tall〕；高 ...
blocking: 閉塞; 編塊; 布局; 除泡; 傳導阻滯; 船墩; 船在干塢中撐墊材中斷墊塊; 粗鍛; 粗磨，制造鏡頭過程之一，使; 粗胚鍛件; 大中華印刷網燙金; 單元化; 墊付塊; 定位掩護; 鍛坯; 堆積成塊; 分塊; 封閉，封阻，阻斷; 封閉阻塞中斷; 封護; 封球; 封塞; 封鎖打法; 蓋帽; 擱擋機率; 格檔; 合塊; 劃分采區(qū); 間歇振蕩; 接收機為強信號封閉; 連銷; 龍骨墩; 模塊化; 排塢墩；結塊; 搶籃板球時把對方擋在外面阻擋犯規(guī); 塞板; 燙金；裝底托；結塊; 停滯，一般指進程在非強制狀態(tài)中運行中斷; 舞臺調度; 舞臺設計; 以塊料或類似物件阻塞; 粘連; 粘頁; 遮光的阻塞的; 支撐裝置; 支承物; 指示劑的阻塞; 止碳; 止炭; 紙張吸著; 琢成塊狀; 自行粘著; 字組組合; 阻礙; 阻塞；閉鎖；封鎖；矩形分層; 阻滯
of blocking: 格擋的
blocking order blocking action: 凍結令; 凍結行動

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Plate shaped dc blocking high power ceramic capaci
盤形隔直流電容
( 3 ) obviously differences exist in the location of east - asia block high , the area of subtropical high and its position between extreme flood year and flood year in sxsp
( 3 )三峽庫區(qū)夏季特澇年及偏澇年中高緯度東亞阻塞高壓位置、副熱帶高壓偏西程度及面積大小存在明顯差異。
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(fā)前后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(fā)與烏拉爾地區(qū)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于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(fā)展，使阻塞高壓重新建立。
Firstly , subtropical high center lay to the north than usual , and forms a blocking high in combination with land high in eastern asia . secondly , on account of the strong southwest current which occurred at the west side of the subtropical high and dynamic effect of the typhoon itself , the landing northward tropical cyclone ( 9711 ) landed in liaoning again . thirdly , a trough with some weak air from ural mountain and the northeast cold air entering into the tropical cyclone showed that the systems in different latitudes had some effects each other
模擬結果表明：此次熱帶風暴造成遼寧全省大暴雨的天氣背景是：副熱帶高壓偏北并與大陸高壓疊加，構成了穩(wěn)定的東亞阻塞形勢； 9711臺風減弱的熱帶風暴，在其自身內力和副高西側的強盛偏南氣流引導下，持續(xù)北上并在遼寧營口至盤錦之間登陸；從烏拉爾山冷堆分裂南下出的弱冷空氣不斷南下，與熱帶風暴在遼寧產生了相互作用，增強了上升運動，致使大暴雨出現(xiàn)。
As a result , we find that in winter when the kuroshio is cooler than the normal , at following summer , the continental cyclone deepen and the east asia monsoon strengthen , that the mid - latitude blocking high weaken and zonal circulation develop , the east asia teleconnection of " - + - " is stired up , so that subtropical high weaken and diminish , and tend to east north , tropical monsoon trough strengthen and mei - yu front weaken , and tend to north , meanwhile south asia high weaken and diminish , and tend to eastvnorth , is easy to form eastern region type
結果發(fā)現(xiàn)當黑潮海溫冷異常時，后期夏季大陸熱低壓加深，東亞夏季風偏強。中緯度阻塞高壓減弱，東亞地區(qū)緯向環(huán)流發(fā)展，在東亞-西太平洋地區(qū)激發(fā)“ - + - ”的東亞遙相關型，從而西太平洋副高強度偏弱，面積偏小，位置偏東、偏北，東亞梅雨鋒也偏弱，季風槽則變強，位置偏北。同時南亞高壓偏弱，位置偏北、偏東，易形成東部型。