convective region 中文意思是什麼

convective region 解釋
對流區域
  • convective : adj. 1. 有傳送力[運輸力]的，傳送性的。2. 【物理學】對流的。
  • region : n. 1. 地方，地域，地帶；地區；行政區，管轄區，區；左近，鄰近；（大氣、海水等的）層，界，境。2. 【解剖學；動物學】（身體的）局部，部位。3. （學問等的）范圍，領域。4. 〈罕用語〉天空。
  1. Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin

    通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上，指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地熱流再分配所致；運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場，從而揭示了盆地基底（義縣組）頂界面地溫分佈特徵；闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件，中低溫對流型地熱系統是地熱勘查的主要對象；圈定了平莊盆地北部朝陽溝?駱駝營子地熱勘查遠景區。
  2. Weather information indicates that the region was affected by a broad rain band with vigorous convective activities at that time. it is estimated that the height of the clouds associated with the thunderstorms reached 45000 feet ( 15000 meters )

    天氣資料顯示，當時該區正受到一度廣?雨帶影響，而且對流活動強烈，雲帶頂部高度估計達到45000尺（ 15000米） 。
  3. The results show that there are two centers of occurrence of llsw respectively in dong bei and jiang nan ; the regional torrential rain over the yangtze river basin is closely associated with llsw during the major periods of heavy rainfall ; the diurnal variation of the number of occurrence in the middle and low reaches of the yangtze river is the strongest in china there are some significant differences between llj and nallsw in positive season, spatial variation, diurnal variation and field of pressure. by the way, the important effect of inertial stability on heavy rainfall with both low level south - westerly jet and high level northerly strong flow is analyzed theoretically. the results show that the existence of the maximum of inertial stability in the left font of the low level jet is favor of the accumulation of the moist thermal energy, and conditional symmetric instability or convective instability can be expected in this region

    另外，慣性穩定性的作用以往不受重視，本文通過對西南低空急流左前方和高空偏北大風軸右後方的慣性穩定性和對稱穩定性的理論分析和實例計算，表明慣性穩定性在伴有高低空急流的暴雨中有重要意義，揭示了梅雨暴雨的一種新的高低空急流耦合機制：低空急流左前方慣性穩定度大值區的存在，有利於低層濕熱能量的積累，使低層傾斜對流的不穩定發展更多期望于條件性對稱不穩定或對流不穩定；高空偏北大風軸（西風急流）的存在，是其右後方（右側）出現對稱不穩定的有利條件，高空相對容易出現干對稱不穩定；慣性穩定性的作用，使低層的傾斜對流更偏向於垂直方向，有利於對流發展，使高層的傾斜對流更偏向於水平方向，有利於高層輻散。
  4. By the analysis of the relationship among convective instability, symmetric instability and snowstorm, we found that the convective instability level is under 800hpa. snow belt is located in the negative value region of moist potential vorticity and verified the theory of symmetric instability

    最後分析了這場暴雪中西北和東北地區的對流和對稱穩定度，個例分析表明，暴雪產生在低層對流不穩定的情況下。
  5. The residual effects of the cloud clusters are generally ignored even though the area they cover is perhaps an order of magnitude larger than the convective region itself

    雲團的殘余影響通常是忽略不計的，即使它們覆蓋的地區比對流區本身可能大一個量級也如此。
  6. Multi - mcss mesoscale convective systems over the heavy rainfall region during 23 - 24 may 1998 in south china

    華南前汛期一次暴雨過程中的中尺度對流系統
  7. The most distinct intensification in maximum azimuthally mean tangential velocity occurs when the convective patch is positioned in rmw, the second in the interior region. this intensification exhibit distinct vibration with 6 ~ 7h period and the vibration in inner region diminishes with shorter period

    Rmw附近擾動使最大平均切向風速增大最明顯，其次是內核區，而且這種增強表現出顯著的震蕩特徵，震蕩周期約為6 7h ，內核區的震蕩較弱，震蕩周期略短。
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