| 1. | The variation of wind speed dominates the variation of latent heat flux eventually
感热通量的变化主要由海气温差的变化主导。 |
| 2. | The half - year cycle of latent heat flux exists in the xisha area , with the maximum appearing in winter
西沙海面潜热通量存在半年周期特征，极大值也是出现在冬半年。 |
| 3. | In equatorial regions , the air - sea humidity difference is overestimated in whoi relative to pirata , which leads to the biases in latent heat flux
在赤道区， whoi对海气湿度差的估计相对于pirata偏高，直接导致其对潜热通量的估计偏差。 |
| 4. | 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。 |
| 5. | The results of sensitive experiments indicate that runoff will directly affect the change of soil moisture states , thus affect sensible and latent heat fluxes and other energy terms
并对耦合水文模型的陆面模式做了敏感性试验，结果表明，陆面模式中径流的描述合理与否，将8一对土壤温湿及地表通量产生显著影响。 |
| 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. | ( 2 ) based on gaining the surface parameters , to compare to diversified retrieve model to choose optimal one to retrieve net radiance flux , soil heat flux and latent heat flux , which settle the groundwork to calculate the regional et
在获取地表参数的基础上，反复对比前人各种遥感反演模型，选择最佳模型对长江三角洲的区域净辐射通量、土壤热通量、潜热通量进行了反演，为计算区域蒸散量奠定了基础。 |
| 9. | It is found that the climatological mean of wind speed and air - sea humidity difference are both large , the variation of wind speed are almost in phase with air - sea humidity difference , yielding much larger or smaller latent heat flux . so the ocean release the most latent heat in its own winter of the two hemispheres when both wind speed and air - sea humidity difference are large
发现在南北两信风区，风速和海气湿度差的变化几乎是同位相的，平均背景风速和海气湿度差都较大，他们互相加强彼此对潜热通量变化的贡献，所以海洋潜热损失最大是发生信风南北两区的各自风速和海气湿度差都较大的冬季。 |
| 10. | In the region north of brazil , although both wind speed and air - sea humidity difference have dramatic variations , the variation of latent heat flux is just ordinary in magnitude . the reason is that the variations of wind speed and air - sea humidity difference are out of phase with each other so that they decrease each other greatly
在巴西以北的暖水区，尽管海气湿度差的变化和风速的变化都较大，但二者在区域内总是反相，彼此削弱了对潜热通量变化的贡献，所以该区潜热通量的变化振幅较小，最终由风速的变化主导潜热通量的变化。 |
