| 1. | There are negative latent and sensible heat fluxes in south and east of the cyclone central area after it moved to ocean
气旋出海后在气旋中心区南方和东方存在负潜热通量和感热通量区。 |
| 2. | The effect of surface sensible heat flux of the qinghai - xizang plateau on general circulation over the northern hemisphere and climatic anomaly of china
热带准两年振荡影响北半球冬季大气环流的诊断分析 |
| 3. | The distribution and variation of latent and sensible heat fluxes of the cyclones were discussed based on the numerical simulation
在数值模拟基础上重点讨论了出海气旋发展过程潜热通量和感热通量的分布及其演变情况。 |
| 4. | 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。 |
| 5. | 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。 |
| 6. | 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。 |
| 7. | 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。 |
| 8. | The results show that the local average temperature and average surface temperature will rise , and both daily difference will rise , too . average sensible heat flux and its daily difference will also increase while average latent heat flux and its daily difference will reduce after the vegetation degration of some area in the west of liaoning province ; the average temperature will raise 0 - 0 . 5 , average surface temperature will raise 0 - 1 . 0 , average sensible heat flux will increase 5 - 40w / m2 , about 8 - 55 % and average latent heat flux will reduce 5 - 60w / m2 , about 4 - 48 %
模拟结果表明：在辽西部分地区植被退化后，当地6 、 7 、 8三个月的夏季平均气温和平均地面温度升高，两者的日较差增大，平均感热通量及其日较差也增大，平均潜热通量及其日较差减小；平均气温升高0 0 . 5 ，平均地面温度升高0 1 . 0 ，平均感热通量增大5 40w / m ~ 2 ，约8 55 ，平均潜热通量减小5 60w / m ~ 2 ，约4 48 。 |
| 9. | Based on the importance of heat flux variability to the earth ' s climate change and the dependence of the study about heat flux variability on the accuracy of heat flux data , this study will focus on the quality evaluation of heat flux datasets available and seasonal and interannual variability of latent and sensible heat fluxes in the tropical atlantic ocean
基于海表潜热和感热通量的时空变化在全球变化中的重要性和海表潜热和感热通量研究对热通量资料产品精度的依赖性，本文重点就现有热通量资料产品的质量和热带大西洋海表潜热和感热通量的季节和年际变化开展较深入的研究。 |
| 10. | The maximum of instantaneous global radiation is beyond 1000w / m2 and the ten - days average intensity is 338 . 90w / m2 because of high atmospheric transparency over semi - arid rainfed agriculture region of loess plateau between june and august . global radiation , reflected global radiation and surface long wave radiation emerge the characteristic of daily variations on a typical clear day and cloudy day , whereas atmospheric long wave radiation has not this characteristic . meanwhile , net radiation , latent heat flux sensible heat flux and soil heat flux appear the same characteristic as the mean daily variations above spring wheat field and bare soil on a typical clear day and cloudy day
黄土高原半干旱雨养农业区夏秋季大气透明度较高，晴天地面的总辐射值最大瞬时值均超过1000w m ~ 2 ， 6 8月总辐射旬平均强度为338 . 90w m ~ 2 ；典型晴天和阴天总辐射、反射辐射、地表长波辐射均表现出明显的日变化特征，而雨天没有明显的日循环规律；无论是晴天、阴天还是雨天，大气长波辐射基本没有明显的日变化规律。 |
