advection heat

[ədˈvekʃən hi:t]
  • advection heat
  • 释义

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纠错 数据更新时间:2026-06-10 14:26:58
1、

There is strong cool advection below highs of 200 m, while the weak warm advection between the heights of 250 m and 400 m. The heat advection have significantly influence on the temperature and stratification of boundary layer;

夜间200m高度以下有较强的冷平流,在250~400m高度有较弱的暖平流,冷暖温度平流对测点上空边界层温度和层结变化有显著影响;

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3、

To determine extent of the effect of groundwater advection on U-type vertical underground heat exchangers, based on a mathematics model considering thermal conduction and groundwater advection, utilizes an overall solution to obtain the whole temperature field including fluid in pipe, pipe wall and surrounding soil.

为确定地下水渗流对U型地下埋管换热器的影响,基于热渗耦合作用下的数学模型,采用整体求解方法求得管内流体、地下埋管换热器及周围土壤的温度场数值解。

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4、

In the KOE region, the vertical advection, heat flux and horizontal advection anomalies are all important in producing the regime shift and the horizontal advection anomalies were found crucial for the time of the regime shift.

在KOE区,垂直平流、热通量和水平平流三者都起了重要作用,其中水平平流异常对这一区域海温年代际跃变出现的时间起了至关重要的作用。

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