jet stream 中文意思是什麼
jet stream
解釋
1. 急流,噴流。2. 【航空】噴射氣流,噴流。
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The jet stream and gravity wave in the atmosphere
高空急流與重力內波 -
200hpa 24 - hr upper air forecast weather map - jet stream streamline
24小時200百帕斯卡高空預測天氣圖-高空急流及流線 -
200hpa 72 - hr upper air forecast weather map - jet stream streamline
72小時200百帕斯卡高空預測天氣圖-高空急流及流線 -
200hpa 36 - hr upper air forecast weather map - jet stream streamline
36小時200百帕斯卡高空預測天氣圖-高空急流及流線 -
200hpa animation upper air forecast weather map - jet stream streamline
動畫200百帕斯卡高空預測天氣圖-高空急流及流線 -
A jet stream is a narrow band of strong winds several kilometres above ground
高空急流是距離地面數公里高的狹窄強風帶。 -
Jet stream streamline
高空急流及流線 -
Jet stream laser
射流雜料激光器 -
She watched a jet stream grow wider and blur as its thin end rose higher into the blue sky
見到有一股飛機的飛行雲變寬,變模糊,此時它的細端升入了藍天。 -
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。 -
3. synoptic meteorology : the general circulation ; air masses ; fronts ; tropopause ; jet stream ; fog ; local winds ; severe local storms
3 .天氣學:大氣環流氣團鋒對流層頂急流霧地方性風強烈地方性風暴。 -
The jet impacts the companion galaxy at its edge and is then disrupted and deflected, much like how a stream of water from a hose will splay out after hitting a wall at an angle
噴流與伴星系的邊緣處發生碰撞,然後被打亂並反射,非常類似與從水管中噴出的水流從一定角度擊中一面墻壁產生的效果。 -
The flow of air in a jet stream can be likened to a fast - flowing river. where the fast - flowing river meets slow - moving water near the banks, waves and swirls are often generated
空氣在高空急速流動,就好像水在猛急河流中流動一樣,當猛急的河水遇上河岸旁緩緩的水流時,便會產生波浪和漩渦。 -
Jet stream is an elongated belt of high speed air, typically found in upper tropospheric westerly flow round the globe. a jet stream may stretch over tens of thousands of kilometres in length from west to east and a few hundred kilometres in width from north to south
高空急流是圍繞地球的一條強而窄的高速氣流帶,集中在對流層上部或平流層中,在中高緯西風帶內或在低緯度地區都可出現。 -
It shows that the network, affected by stream of water, superposes each other leading to the jet of detonator energy cavity and metal fragments which can break the nonel - tube without transmitting detonation yet, so as to make the detonation transmission in some local network break off and bring about misfire
結果表明,受紊亂水流影響,導爆管網路相互疊加,比較凌亂,致使傳爆雷管產生的聚能射流和碎片容易將尚未傳爆的導爆管切斷或打破,而使局部網路爆轟傳遞中斷,造成拒爆現象的發生。 -
The analysis for the evolution of the upper westerly field, north - south wind field show that the upper jet stream is a good indication to sandstorm - occurring areas, the strong sandstorm appears at the right side of the entry domain of the jet stream and the ascension domain of secondary circulation
對高空東西風場、南北風場的演變進行分析,發現高空急流對沙塵暴發生區有很好的指示作用,強沙塵暴位於200hpa高空急流入口區右側、 500hpa正渦度中心下風方和次級反環流的上升區域內。 -
The low - level jet stream is the result of the spread of the momentum from the upper - level jet stream
低空急流是高空急流的動量向下輸送的結果。低空急流的生成先於水汽及降水的爆發。 -
The red line marks an area with winds exceeding 80 knots around 150 kilometres per hour, revealing where the jet stream was at that level
圖中紅線標志風速超過80海里約每小時150公里的區域,即該高度的高空急流所在。 -
The low - level jet stream has three vibration processes, which corresponded to the three lows " beginning and developing
低空急流有三次脈動過程,與三個低渦的產生和發展對應。 -
And the dv of lower - level systems, e. g., jet stream, is among the intermediate changes happening after the dv is displayed in the meiyu pressure field
低空急流等系統的日變化是梅雨天氣系統內,低層氣壓場形勢出現日變化后發生的眾多中間變化過程之一。
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