氣壓的槽 的英文怎麼說
中文拼音 [qìyādecáo]
氣壓的槽
英文
trough- 氣 : Ⅰ名詞1 (氣體) gas 2 (空氣) air 3 (氣息) breath 4 (自然界冷熱陰晴等現象) weather 5 (氣味...
- 壓 : 壓構詞成分。
- 的 : 4次方是 The fourth power of 2 is direction
- 槽 : 名詞1 (盛牲口飼料或飲料等液體的器具) trough; manger (for water animal feed wine vat) 2 (兩邊...
- 氣壓 : [氣象學] pressure; atmospheric pressure; barometric pressure; gas pressure; air pressure
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Application of elastic variable - section pressure - equalizing groove in the structural design of high - stiffness aerostatic thrust bearing
用可變截面均壓槽實現高剛度空氣靜壓軸承的結構設計Some main ones are solar heating, proximity of low pressure troughs and convergence of two different air streams
空氣上升的原因很多,主要有地面受太陽照射加熱在低壓槽附近和兩股不同的氣流匯聚等。The atmospheric circulation of the wet year deviate from enso year to no - enso year. in enso year, the subtropical high is strong with the deepening of trough over south of baikal lake while in no - enso year, the subtropical high is weak with the high incidence of typhoons over northwest of pacific and south china sea
多雨年發生在enso年和no - enso年大氣環流形式的不同主要表現在: enso年副熱帶高壓較強,貝加爾湖地區南部低壓槽容易加深;在no - enso年副熱帶高壓強度減弱,在西北太平洋和南海地區多熱帶系統活動。The result shows that : the sand - dust storm occured in favorable climate background that is drought and rainless, the tilted trough and mongolia cyclone are the important weather systems that caused the severe sand - dust storm, tilted trough and strong frontal zone caused the mongolia cyclone developed and the clod front strengthened at surface, high jet and ferrel circulation are the main reason that momentum spreaded downward from higher level and frontal zone strengthened on lower level
結果表明:沙塵暴是在乾旱少雨的有利的氣候背景下產生的。斜壓槽和蒙古氣旋是觸發這次強沙塵暴天氣過程的重要的天氣系統,高空斜壓槽和強鋒區促使了地面蒙古氣旋的發展和冷鋒的加強,誘發沙塵暴天氣。高空急流及其下方的ferrel環流起到了高層動量下傳和加強低層鋒區的重要作用。We can use the mm5 model in definite time, definite area weather forecasting. we conclude that : : the moving route of this necw in its developing progress was direct - south along latitude, the cold air is rough, and just this made the rough vertical velocity ; the necw southern moving and conflicting with the west pacification sub - tropical high makes rough jet steam. the plenty south - west warm and wet air made by the jet stream gave the rainstorm demanded vapor ;. the rough vertical velocity by jet stream is a main reason in this rainstorm ; the mm5 model uses four - direction analysis data as its input, this avoids some errors occurred in observe and transfer, thus made the result more useful
綜合分析認為: ( 1 ) 、這次冷渦在其發生發展過程中,其移動路徑是沿經圈直線南壓,攜帶的冷空氣勢力較強,形成槽后較強的垂直運動; ( 2 ) 、西太平洋副熱帶高壓偏北位置與東北冷渦南壓形成的急流軸,把源源不斷的西南暖濕氣流輸送到遼西地區,也就是急流軸的左前方位置,為這次暴雨的產生提供了充足的水汽來源; ( 3 ) 、低空急流不但為暴雨輸送水汽,其造成的較強的垂直環流也是產生強降水的一個主要原因; ( 4 ) 、 mm5模式以四維同化資料作為初始場,最大限度地避免了觀測誤差可能造成的積分不穩定,提高了模擬結果的參考價值。By arrangement of the control channels through which the hydraulic fluid flows from the discharge chamber into the oil reservoir, this allows any gas bubbles being released from the hydraulic fluid during the suction stroke to be expelled into the oil reservoir
通過液壓油經控制通道由排出腔流入油槽的這種布置,使得任何在吸入沖程從液壓油中釋放出來的氣泡都被排到油槽中。The summer rainfall anomaly of north china is closely related to indian low, west pacific subtropical high, westerly troughs and ridges in mid - latitude, south asia high, subtropical monsoon circulation and cold air activity on the corresponding period, and similar circulation pattern also appears in the preceding spring
結果表明: ( 1 )華北夏季降水異常與同期印度低壓、西太平洋副高、中緯度西風槽脊、南亞高壓、副熱帶季風環流和冷空氣活動的異常都密切相關。華北夏季降水異常年春季的環流特徵與夏季類似。Linear induction motor is an important kind of machines which have some merits such as simple structure, low cost, durability, convenience for maintenance etc. the subject of this thesis is to study a big circular ring linear induction motor, and the major works in this thesis are summarized as follows : ( 1 ) considering the effects of the finite length of primary core, one - dimension analytical solution for the air gap field is cited in this paper. based on it, the single layer winding magnetic field is studied. considering whole - pitched and short - pitched winding configuration with odd poles and half - fulled slots in both ends, the double - layer winding magnetic field is analyzed, respectively
本文對大圓環直線感應電機進行了深入細致研究,內容包括: ( 1 )本文採用有限長行波面電流作用於有限長鐵芯上的模型,引用了氣隙磁場一維解,研究了單層繞組磁場,奇數極半填槽雙層繞組在採用整距和短距時磁場的分析、比較,簡單介紹了二維解; ( 2 )用有限元軟體ansoft對大圓環直線感應電機空載氣隙磁場進行了靜態分析,並分析了結果; ( 3 )用軟體進行了額定電壓下的瞬態分析,得到了轉矩,位移,轉速隨時間變化曲線圖,利用單極性霍爾元件測定轉速並與軟體計算結果進行了比較,採用等效電路法計算了堵轉時的最大電磁力並做實驗進行了驗證,由實驗測得了三相電流波形,並與計算結果進行了比較,對其不對稱性進行了定性分析。The machine is a specially equipment processing all types of waterspouts and grooves for gas - pressure balance of plastic door and window
本機是加工塑料門窗各種類型排水槽及氣壓平衡槽的專用設備。A trough is an area of low pressure where air from higher pressure converges and is forced to lift upwards to form thunderstorms
槽是氣壓較四周為低的地區,空氣會由高氣壓區流向低氣壓區而匯聚于低壓槽,最後被迫向上升,造成雷雨。The results show that the weather process occurs because of typhoon trough with cold air, deep upper trough ; the southeast low - jet by typhoon transported large water vapour and great energy of instability to heavy rainfaill area ; cold air, lower convergence and upper divergence by deep upper trough lead to development of the east - ocean low pressure and occurd strong wind
分析結果表明:這次天氣過程是由臺風倒槽和冷空氣及深厚的高空槽共同作用引起的;臺風環流引起的東南低空急流為暴雨區輸送了大量的水汽和不穩定能量;冷空氣的侵入加上深厚的高空槽引起的低空輻合、中高層輻散,促使了東海低壓的劇烈發展,產生了猛烈的大風。Modified reynolds equation for squeeze - film air damping of slotted plates in mems devices
微機械槽板結構空氣壓膜阻尼的修正雷諾方程The pressure there is lower than that at neighbouring points on either side of the trough line
槽線上的氣壓會較其兩旁氣壓為低。Conventional approaches to compact hydrogen storage ? compressing the gas to up to 10, 000 pounds per square inch ( psi ) or cooling it down to cryogenic temperatures so that it liquefies ( around - 252 degrees celsius ) ? can attain only about half the energy density needed to fit enough fuel inside something the size of a gas tank
一般壓縮氫氣儲存槽所使用的方式,是將氣體壓縮使壓力達到每平方公尺700萬公斤重,或是冷卻到將近- 252使之液化,但這只能達到所需能量密度的一半,無法將整個氣瓶充滿。Regional difference in lower - level temperature dv and pressure dv are greatly weakened and dv of llj is distinctly faint without the nanling ridge. this result show that nanling ridge acts as a critical role in the establishment of dv of the lower - level temperature and pressure, which give rise to the dv of llj in south china
而當模式中僅僅去掉南嶺和武夷山山脈地形后,低層大氣溫度場日變化的區域性差異明顯變弱,梅雨低壓帶南側原南嶺山脈所在地的溫度日較差明顯減小,使得梅雨低壓槽與華南地區之間的南北向水平溫度梯度和水平氣壓梯度的日較差顯著變小,導致華南低空急流日變化的顯著減弱。Appointing to the characteristic and operating condition of hydrogen compressor, the carrying capacity, the leakage and the film thickness of the dry gas seal are calculated by the theory of narrow groove
針對氫氣壓縮機的特點和具體的操作條件,利用窄槽理論對所設計的干氣密封進行了承載力、泄漏量及膜厚的計算。The extra rainfall was mainly due to an active trough of low pressure over the south china coast in may, the combined effect of an active southwesterly and severe tropical storm bilis in july and a tropical depression in september
本年雨量較多主要是五月時受到華南沿岸的一道活躍低壓槽影響,七月時受到一股活躍西南季候風與強烈熱帶風暴碧利斯的共同影響及九月時受到一個熱帶低氣壓影響所致。When the tcf in nwp is high, the bengal bay cef which located at 90 e is strong and the new guinea cef located at 150 e is weak ; there is a anti - cyclonic circulation near the equator. the equatorial buffer zone is fortified : it is propitious to the equatorial anticyclones activated and push monsoon trough to higher latitude, this circulation pattern can promote the genesis of tc in nwp
多熱帶氣旋年,位於90 e附近的孟加拉灣越赤道氣流顯著增強,而位於150 e附近的新幾內亞越赤道氣流異常偏弱;在赤道附近存在一個異常的反氣旋性環流,赤道緩沖帶較強,有利於赤道高壓的活躍,季風槽被推向較高緯度,從而有利於熱帶氣旋的生成。3 by delineating the various features of the weather maps and putting them into layers i. e., pressure cells, troughs, ridges etc, users can overcome visual information overloads by selecting appropriate layers of interest and animating them over time
將描述天氣地圖的不同特徵如氣壓單元,低壓槽和高壓脊並將其放入不同的層中,用戶可以選擇感興趣的圖層以避免可視信息過量,並使之以動畫形式表示。When the autumn kuroshio ssta is positive, the sea - land sea level pressure differences in the east asian region become large in winter, the east asian trough at 500hpa shifts eastward and is deep in its south and shallow in the northern, along with strong north winds in the above area and weak westerly circulation in the asian region
當秋季黑潮區域海溫異常偏高,東亞地區的海陸氣壓差異進一步加大,東亞大槽北部減弱、南部加深、位置東移,東亞地區的偏北風加強,亞洲地區西風環流減弱,即東亞冬季風加強;反之亦然。分享友人