The simulated latent heat of coarse soil is smaller , and surface temperature and sensible heat is larger than the results of the control run 粗糙土壤，反照率大，造成地面吸收短波辐射减少。粗糙土壤用于蒸发的潜热减少，地温升高，感热大。
The simulations of ground temperature and earth absorbed net solar radiation are lower than the observation . sensible heat and latent heat are also lower than the observation 由于模式模拟的地温偏低，净的短波辐射偏小，则模拟的感热和潜热值偏小。
The fine soil characters have little variation of albedo and absorbed solar radiation . the simulated sensible heat is lower than the result of the control run in clay case 粘土反照率变化不大，因此吸收太阳辐射变化不明显，用于蒸发的潜热变化不明显，地温略降低，感热变小。
The variation of sensible heat flux is dominated by air - sea temperature difference . interannual variability of turbulent heat fluxes is examined using svd , eof and mtm methods 热带太平洋enso事件通过对walker环流的调整减小热带大西洋itcz区的风速值，湍动热通量亦随之减小。
Moreover , evapotranspiration consumes mainly net radiation on a clear day and sensible heat flux is greater than latent heat flux on a cloudy day above spring wheat field 在有植被覆盖或裸地下垫面，晴天、阴天的净辐射、潜热、感热及土壤热通量均表现出了与平均状况一样的日变化特征。
Based on the analysis of pool water evaporation heat transfer and the sensible heat transfer between indoor air and pool water , deduces the calculation formula of latent load by pool water evaporation 摘要通过对游泳馆内池水蒸发换热及池水与室内空气之间的显热换热分析，推导出池水蒸发潜热负荷计算公式。
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。
The diminutive deviate of soil moisture estimated by different hydraulic models affect the land surface net radiation by affecting soil reflectance , and farther affect sensible heat , latent heat and soil heat fluxes 在ssib模式中采用不同的土壤水力模式所引起的土壤湿度模拟结果的差异会对陆面过程模式模拟的感热、潜热和地表热通量等物理量产生影响。
It shows that the surface temperature is extremely sensitive to land surface characteristics . a pdf of land surface temperature is given that is used in calculating sensible heat flux and latent heat flux of yangtze river lower region （ 3 ）利用noaaavhrr卫星资料反演了长江三角洲（长江下游）地表温度，发现地表温度对下垫面特征的空间变化较为敏感。
With highest respective boundary pbl parameter scheme , we devise five test projects : control experiment and sensitive experiments without sensible heat flux , without latent heat flux , without sensible and latent heat flux , without terrain 在高分辨率边界pbl参数化方案下设计5组试验方案，对几个个例风场进行模拟检验：控制试验、无感热试验、无潜热试验、无感热无潜热试验、无地形试验。
