Latent Heat Flux

In addition , except for the East China sea , the latent heat flux generally indicates a decreased distribution from north to south , while the annual averaged sensible heat flux shows an increased distribution .

除了东海，潜热通量的年均值基本上表现为自北向南减小的分布，而感热通量年均值则表现为自北向南增大的分布。

Share of latent heat flux in the heat budget tends to increase ;

热收支中，潜热通量所占的份额增多；

Latent heat flux in urban is smaller than suburban .

潜热通量总体上是市区小于郊区。

Generally the latent heat flux increases gradually during the monsoon onset .

一般而言，季风爆发期间潜热输送逐渐增加；

Under the different Surface Cover , the Latent Heat Flux is difference with its unique properties .

通过反演的结果发现：在不同的地表覆被状况下，所表现出的潜热通量不尽相同，并具有独特的性质，潜热通量的空间分布随着地表覆被变化而有明显变化。

During this exchange process , Latent Heat Flux regulates the global water and the energy distribution .

在该交换过程中，潜热通量对全球水分和能量的分布起着一定的调节作用。

Big and Good Matter Oasis has low sensible heat flux and high latent heat flux ;

绿洲地区感热通量小，潜热通量大；

Meteorological factors had no impact on the diurnal centroid for latent heat flux .

潜热通量日变化峰值时间与气象要素关系均不显著。

The peak value of latent heat flux was higher than that of sensible heat flux in summer .

在夏季，农田和森林的潜热通量的峰值大于感热通量。

Model calculation of sensible and latent heat flux in the ocean area between 50 ° s and Antarctic

50°S以南海域的感热潜热通量的模式计算

Under the limited data and resource conditions , the writer studies the Latent Heat Flux in the typical sample region .

本文在有限的数据资源条件下，对研究区进行了潜热通量反演。

The results show that the latent heat flux is much greater than the ra-diate heat flux .

分析结果表明在赤道海域，潜热通量远远大于感热通量。

The net radiation and contribution of latent heat flux tend to decrease due to increasingly grazing intensity .

随放牧强度的增加，净辐射或净有效能减少，而且潜热交换的贡献也相对减少。

The sensible heat flux is very greater than the latent heat flux in the PBL air .

地表感热通量明显大于地表潜热通量；

The structure parameter of refractive index imaginary part for the different latent heat flux was calculated by means of simulation theory .

不同潜热通量时，折射率的结构常数在满足相似理论的条件下可以计算出来。

Relationships of sensible heat flux , latent heat flux and momentum fluxes with meteorological elements are different .

通量变化受不同环境要素的影响：感热通量与海-气温差呈正相关关系，与气温呈明显的负相关关系。

Long-term analysis : The sensible heat flux and the latent heat flux reanalysis data were bigger than their observed data .

长期分析发现：感、潜热通量再分析数据比对应的实测数据偏大。

The results show that the ratio of the latent heat flux to the sensible heat flux is10.14 ;

指出西大平洋暖池海区游热通量与显效通量之比为10.14：1；

Both in clear and foggy conditions , sensible and latent heat flux have negative correlations to the air temperature .

在晴天和雾天时，感热通量均与气温有显著的负相关关系。

The results show that the positive sensible and latent heat flux usually appear in the areas of dust-storms occurring .

结果表明，通常在典型强沙尘暴事件发生区表现为正的感热通量和正的潜热通量；

The reaction of SST and sensible heat flux responding to abnormal latent heat flux curbs this positive feedback process .

在潜热通量与大气相互作用的正反馈机制中，海温和感热通量的响应对这种正反馈过程起到一定的抑制作用。

All the component changes of sensible heat flux and latent heat flux are related to the wet and dry & season changes .

显热通量、潜热通量等分量的变化都与干湿季节变化有关，潜热消耗热量是显热消耗热量的6.9倍。

And ( 3 ) that surface latent heat flux may be one of the main heating factors for the subtropical high intensification and maintenance .

由高低空急流耦合在淮河流域产生持久的上升运动是淮河流域强降水的主要物理机制；（4）地表潜热释放是使副高加强和维持的主要热力因子之一。

The Distribution of Three Kinds of Different Alpine Meadow Vegetation and the Comparison of the Vegetation with Sensible Heat and Latent Heat Flux

三种高寒草甸植被分布及与湍流交换通量关系的比较

But latent heat flux can be up to 570 W · m - 2 , when precipitation occuring .

但8月份的潜热通量大，平均最大约为120W·m-2，当有降水发生时，潜热通量可达570W·m-2，与感热通量相当。

KESSLER-MRF case produces the minimum latent heat flux while LIN-YSU produces the maximum latent flux .

KESSLER方案和MRF方案实验模拟出的平均潜热最小，LIN方案和YSU方案实验潜热最大；

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。

Latent heat flux , sensible heat flux , net radiation flux and photosynthetic active radiation are all significantly positively related with CO2 flux .

潜热通量、显热通量、净辐射、光合有效辐射均与CO2通量呈极显著正相关。

In the SiB model , we calculated the radiation , sensible heat , latent heat flux and the daily variation of temperature at the surface .

利用SiB模式计算了地表辐射。感热、潜热通量，并且预报地表温度。

Analysis of boundary layer fluxes shows that the amount of latent heat flux leaded to differ the Khanun 's horizontal and vertical structure .

边界层方案的差异也导致台风动力和热力结构在水平和垂直分布上都出现显著差异。