cumulus convection 中文意思是什麼
cumulus convection
解釋
積雲對流- cumulus : n. （pl. -li ）1. 堆，堆積物。2. 【氣象學】積雲。
- convection : n. 1. 傳送。2. 【物理學】運流，環流；【氣象學】對流，上升氣流。
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In cumulus convection ascent rates of several metres a second give a cooling rate of a few degrees per minute.
在積雲中，每秒幾米的對流上升速度造成的冷卻速率為每分鐘幾度。 -
The adjoint code technique is employed for projecting the adjoint programs of betts - miller cumulus convection scheme of lasg - rem model and their correctness is verified, indicating that the adjoint program and its nonlinear program are converse in theory
採用伴隨碼方法構造了lasg - rem模式的betts對流參數化方案的伴隨程序，並對其正確性進行了檢驗，結果表明編制的betts方案的伴隨程序與非線性程序在理論上是可逆的。 -
Orsm includes physical processes such as radiative transfer, phase changes of water substance, re - distribution of energy due to cumulus convection, transport of momentum, energy and moisture by turbulence, and exchanges between the atmosphere and the surface layer
： orsm中的物理過程包括輻射交換水分的相變積雲對流所帶動的能量重新分佈湍流所引發的動量能量和水汽輸送大氣與地面層之間的各種交換等等。 -
In day time, especially in mid - summer, the ground heats up under the sun and spurs convection in the air. this lifts moisture up the atmosphere aloft, which gradually develops into isolated, floating cumulus
在日間，特別是在盛夏時候，地面吸收大量太陽的熱量，引起大氣對流運動，將水氣帶上上空，慢慢形成孤立懸浮的積雲。 -
In this paper, the results of simulating two rainfall cases show that lasg - rem adjoint model has good power of predicting rainfall. the adjoint coding technique is employed for projecting the adjoint programs of betts - miller cumulus convection scheme of lasg - rem model and their correctness is verified, indicating that the adjoint program and its nonlinear program are converse in theory
本文利用伴隨碼方法編制了lasg - rem模式的betts對流參數化方案及大尺度降水方案的同化模塊，並對其正確性進行了檢驗，結果表明構造的伴隨模塊與原模式非線性模塊具有理論和實際上的可逆性。 -
Analyze 1000hpa stream field evolvement chart, a southwest - northeast combine strap was forming in liaoning province by southwest air current and northwest air current. level combine induce the combine strap cyclone bend, whorl degree intension increase. boundary layer friction combine bring to ascend and come into being small measure cumulus convection pyrogenation
高低空急流的耦合是此次強對流爆發的重要觸發機制，高低空急流在耦合的過程中， 300hpa高空急流強度超過50m s ， 850hpa低空急流強度超過20m s ，而且低空急流與高空急流剛好在高空急流出口區的位置上相交，對強對流爆發有利。 -
When the atmosphere is moist and unstable, the air rises and causes cumulus clouds to further develop. with strong convection, they can develop into cumulonimbus clouds. cumulonimbus is common in summer, sometimes bringing rain and thunder
當水汽充裕大氣不穩定時，空氣上升，便會加速積雲本身的發展，再加上強勁的對流，積雲會發展成另一雲種積雨雲，尤其在夏天，會經常發生，有時還帶來雷雨。
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