显热交换 meaning in Chinese
sensible heat transfer
Examples
- ( 3 ) compared with bare soil , income of net radiation declined , apparent heat weakened and latent heat exchange were almost disappeared on the soil surface with film
( 3 )薄膜覆盖于土壤表面后，与未覆盖的土壤相比，地表净辐射r _ n收入下降，显热交换p减弱，潜热交换le趋于零。 - Analyses experimental results with classical heat and mass transfer theory , and indicates that when these parameters change , the latent heat efficiency changes much more than the sensible heat efficiency
利用经典传热、传质理论对实验结果进行了分析，指出当上述因素发生变化时，全热交换器潜热交换效率受到的影响大于显热交换效率。 - Soil heat flux from atmosphere to soil is about 5 % of net radiation on a clear and cloudy day and soil discharge energy to atmosphere on a rainy day above the same field . in brief , average latent heat , sensible heat and soil heat flux is 40 % . 50 % and 10 % of net radiation respectively
在春小麦下垫面，晴天能量主要消耗于农田蒸散，而在阴天显热交换大于农田蒸散耗热；在晴天和阴天大气向土壤的能量传输均维持在净辐射的5左右，雨天时，土壤热通量为负值。 - Similarly , the net radiation on a cloudy day is mainly used up evaporation of soil . the integrated value of soil heat flux is negative on a cloudy day and that shows the soil emits the heat , which is different on a clear day . in short , average latent , sensible and soil heat flux is 67 % , 21 % and 6 % of net radiation respectively
在裸地下垫面时，晴天潜热占到净辐射的60 ，显热交换只占到19 ，在阴天净辐射同样主要消耗于土壤蒸发，与晴天不同的是在阴天土壤热通量积分值小于零，表明土壤在向外释放热量；平均状况下，潜热、显热和土壤热通分别占到净辐射的67 、 21和6 。